After a cold and snowy start to winter, April has made an early appearance in the American Midwest. Strong southerly winds, ahead of the next winter storm, have pumped mild, humid air into the Heartland, priming the region for thunderstorms, which rumbled through Missouri overnight and into this morning.
This brief spring interlude, sporting afternoon highs near 60F and morning lows near 50F, is already beginning to fade; blue skies to the northwest, so inviting from a distance, warn of cold air behind the front. As the storm moves off to the east, northerly winds will push this air into Central Missouri and winter will reclaim the State.
These weather oscillations usually settle down in January as the jet stream assumes a steady, more southern track, keeping us on the cold side of that atmospheric boundary. But the word "usually" is a relative term and North American weather patterns are notoriously fickle. We have reason to hope that April makes several more visits before it finally moves in next spring.
Jumat, 31 Desember 2010
Rabu, 29 Desember 2010
Winter & the Elderly
In nature, winter is the culling season. Wild creatures that are old, sick, injured or malnourished often succumb to the harsh conditions; hypothermia, starvation and predation all take a toll. Early man also faced these threats as he emigrated from his tropical home to northern latitudes.
Most older humans will admit that their tolerance to cold weather has decreased with their advancing age and there are physiologic reasons for this perception. As we age our metabolic rate falls, our activity decreases, our calorie intake is reduced and our body fat begins to diminish; all of these factors make it more difficult to retain and generate heat. Furthermore, older persons often have chronic conditions that lead to impaired mobility and balance, making them more prone to falls and injury; the presence of snow and ice only exacerbates this risk. Finally, all of us are more likely to be infected with viruses during the colder months as our indoor lifestyle increases contact with other humans; many of these infections, including influenza, are more severe in the elderly and are more likely to be complicated by pneumonia, sepsis and other potentially fatal conditions.
Sensing all of these factors, older persons with financial resources tend to migrate to warmer climes for the winter months. While longevity is more related to genetics and healthy lifestyle choices, they know that they will be more comfortable in the warm environment. At some deeper level, we may also be experiencing the urge to return to our native ecosystem; we are, after all, a tropical species.
Most older humans will admit that their tolerance to cold weather has decreased with their advancing age and there are physiologic reasons for this perception. As we age our metabolic rate falls, our activity decreases, our calorie intake is reduced and our body fat begins to diminish; all of these factors make it more difficult to retain and generate heat. Furthermore, older persons often have chronic conditions that lead to impaired mobility and balance, making them more prone to falls and injury; the presence of snow and ice only exacerbates this risk. Finally, all of us are more likely to be infected with viruses during the colder months as our indoor lifestyle increases contact with other humans; many of these infections, including influenza, are more severe in the elderly and are more likely to be complicated by pneumonia, sepsis and other potentially fatal conditions.
Sensing all of these factors, older persons with financial resources tend to migrate to warmer climes for the winter months. While longevity is more related to genetics and healthy lifestyle choices, they know that they will be more comfortable in the warm environment. At some deeper level, we may also be experiencing the urge to return to our native ecosystem; we are, after all, a tropical species.
Selasa, 28 Desember 2010
Unnoticed Visitors
Novice birders, focusing on common, local, avian residents, often overlook migrants and seasonal visitors that resemble those birds. One such visitor is the purple finch, a fairly common winter resident in California and across the eastern half of the U.S. Since they are similar in appearance to the abundant house finches, their presence may not be appreciated.
A bit larger, stockier and possessing a heavier bill, purple finches are also recognized by distinct plumage characteristics and a notched tail. The males have a rasberry wash over their head, breast and rump, which mixes with brown on their back and is diffused with white on their chest and abdomen; in contrast, the male house finch has an uneven, orange-red coloration, primarily on the head and upper chest. Female purple finches, like female house finches, are streaked with white and brown but have a prominant white facial stripe, just above each eye.
The summer breeding range of purple finches extends across the coniferous forest belt of Canada, down through the northern Midwest, New England, the Pacific Northwest, and southward along the Appalachian and Sierra Nevada mountains. In winter, they abandon the northernmost section of that breeding range and appear in sizable flocks throughout California and the eastern half of the U.S. Maintaining a fondness for coniferous woodlands, they also forage for seeds, buds and berries in mixed woods and weedy fields during the colder months, often turning up at backyard feeders. Like some other winter visitors, such as evening grosbeaks, red-breasted nuthatches and Bohemian waxings, purple finches are erratic wanderers and their numbers vary widely from year to year.
A bit larger, stockier and possessing a heavier bill, purple finches are also recognized by distinct plumage characteristics and a notched tail. The males have a rasberry wash over their head, breast and rump, which mixes with brown on their back and is diffused with white on their chest and abdomen; in contrast, the male house finch has an uneven, orange-red coloration, primarily on the head and upper chest. Female purple finches, like female house finches, are streaked with white and brown but have a prominant white facial stripe, just above each eye.
The summer breeding range of purple finches extends across the coniferous forest belt of Canada, down through the northern Midwest, New England, the Pacific Northwest, and southward along the Appalachian and Sierra Nevada mountains. In winter, they abandon the northernmost section of that breeding range and appear in sizable flocks throughout California and the eastern half of the U.S. Maintaining a fondness for coniferous woodlands, they also forage for seeds, buds and berries in mixed woods and weedy fields during the colder months, often turning up at backyard feeders. Like some other winter visitors, such as evening grosbeaks, red-breasted nuthatches and Bohemian waxings, purple finches are erratic wanderers and their numbers vary widely from year to year.
Senin, 27 Desember 2010
Unaweep Canyon Mystery
While the field of plate tectonics has solved many geologic mysteries, others remain. One of these is Unaweep Canyon in the northern portion of the Uncompahgre Plateau, in western Colorado; unlike other canyons, it has two mouths and a divide along its course, which is now traversed by Colorado Route 141.
Geologists have long debated the natural history of Unaweep Canyon. Some have suggested that, since the canyon is U-shaped, it was carved by mountain glaciers during the Pleistocene; however, closer examination of its floor has revealed that it is a V-shaped, stream-cut canyon, since filled with erosional debris to produce the flattened bed. Others, realizing that the small streams that now flow east and west from the divide could have not produced this magnificent canyon, with its massive walls of hard, Precambrian rock, theorized that the Colorado River originally sculpted Unaweep before changing course to skirt the northern edge of the Plateau.
The most recent evidence suggests that the Gunnison River, which also carved the Black Canyon, once cut through the Uncompahgre Plateau, joining the Dolores River on its west side before flowing northwestward into the Colorado. Based on examination of gravels and other sediments, it appears that the Gunnison gradually sliced through the Uncompahgre ridge as it rose with the rest of the Colorado Plateau during the Miocene-Pliocene Uplift, 25-10 million years ago. A landslide is thought to have disrupted the Gunnison's flow within the Canyon (presumably about 6 million years ago), causing it to back up and eventually flow northward to join the Colorado in the Grand Valley. The abandoned Canyon is now drained by East and West Creeks, too weak to remove the erosional debris of the powerful Gunnison. Time and more field work will tell if this is the true solution to the Unaweep Canyon mystery.
Geologists have long debated the natural history of Unaweep Canyon. Some have suggested that, since the canyon is U-shaped, it was carved by mountain glaciers during the Pleistocene; however, closer examination of its floor has revealed that it is a V-shaped, stream-cut canyon, since filled with erosional debris to produce the flattened bed. Others, realizing that the small streams that now flow east and west from the divide could have not produced this magnificent canyon, with its massive walls of hard, Precambrian rock, theorized that the Colorado River originally sculpted Unaweep before changing course to skirt the northern edge of the Plateau.
The most recent evidence suggests that the Gunnison River, which also carved the Black Canyon, once cut through the Uncompahgre Plateau, joining the Dolores River on its west side before flowing northwestward into the Colorado. Based on examination of gravels and other sediments, it appears that the Gunnison gradually sliced through the Uncompahgre ridge as it rose with the rest of the Colorado Plateau during the Miocene-Pliocene Uplift, 25-10 million years ago. A landslide is thought to have disrupted the Gunnison's flow within the Canyon (presumably about 6 million years ago), causing it to back up and eventually flow northward to join the Colorado in the Grand Valley. The abandoned Canyon is now drained by East and West Creeks, too weak to remove the erosional debris of the powerful Gunnison. Time and more field work will tell if this is the true solution to the Unaweep Canyon mystery.
Minggu, 26 Desember 2010
The Davis Mountains
Looking at a satellite map of the U.S., one notices a dark smudge in West Texas, north of the Big Bend area and just south of I-10. This dark terrain reflects the vegetation and rock formations of the Davis Mountains, which stand out against the pale, drier landscape of the Chihuahuan Desert.
Volcanic in origin, the Davis Mountains are remnants of two large calderas and their associated rhyolite lava flows, ash tuffs, cinder cones and laccolith formations. Persisting for 10 million years, the volcanic activity began in the Oligocene, some 35 million years ago, when grasslands were evolving across the Great Plains and mammalian megafauna dominated the scene. The Davis Mountains cover much of Jeff Davis County and represent the most extensive mountainous region in Texas; summits range from 3500 to almost 8400 feet. Like the Chisos Mountains of Big Bend National Park, the Davis Mountains are part of the Trans-Pecos Volcanic Field, which extends across West Texas and into Northern Mexico.
Catching upslope moisture from all directions, these mountains receive about 18 inches of precipitation each year, more than double that of the surrounding desert. For this reason, they support mixed woodlands of oak, juniper and pine, attracting a large variety of birds, mammals and other wildlife.
Volcanic in origin, the Davis Mountains are remnants of two large calderas and their associated rhyolite lava flows, ash tuffs, cinder cones and laccolith formations. Persisting for 10 million years, the volcanic activity began in the Oligocene, some 35 million years ago, when grasslands were evolving across the Great Plains and mammalian megafauna dominated the scene. The Davis Mountains cover much of Jeff Davis County and represent the most extensive mountainous region in Texas; summits range from 3500 to almost 8400 feet. Like the Chisos Mountains of Big Bend National Park, the Davis Mountains are part of the Trans-Pecos Volcanic Field, which extends across West Texas and into Northern Mexico.
Catching upslope moisture from all directions, these mountains receive about 18 inches of precipitation each year, more than double that of the surrounding desert. For this reason, they support mixed woodlands of oak, juniper and pine, attracting a large variety of birds, mammals and other wildlife.
Sabtu, 25 Desember 2010
Red-Shouldered Hawks
Though less conspicuous and somewhat smaller than their red-tailed cousins, red-shouldered hawks are fairly common throughout the eastern half of the U.S. and along the coast of California. Identification of this buteo is generally made by the fine, rust-colored barring on its chest, its relatively long, banded tail and its loud, high-pitched, descending call; the red shoulder patches, for which it is named, are not always apparent.
Preferring wooded swamps and riparian forest, red-shouldered hawks usually hunt from a low perch and feed on a wide range of prey, from mice and voles to lizards, frogs, snakes and songbirds. Often considered to be the diurnal counterpart of barred owls, both raptors share the same habitat and both have been threatened by the gradual destruction of forest and wetlands. Ironically, red-shouldered hawks, though often heckled by jays and crows themselves, are known to join these birds when they mob great-horned owls, red-tails and other large raptors.
Like many birds of prey, red-shouldered hawks nest in late winter or early spring; 2-4 eggs are generally laid in a bulky nest, high in a tree, and are incubated by both parents. The young hatch within a month and are usually self-sufficient by summer. While most red-shouldered hawks are nonmigratory, those that nest in northern portions of their range often winter in the southern U.S. or in Mexico.
Preferring wooded swamps and riparian forest, red-shouldered hawks usually hunt from a low perch and feed on a wide range of prey, from mice and voles to lizards, frogs, snakes and songbirds. Often considered to be the diurnal counterpart of barred owls, both raptors share the same habitat and both have been threatened by the gradual destruction of forest and wetlands. Ironically, red-shouldered hawks, though often heckled by jays and crows themselves, are known to join these birds when they mob great-horned owls, red-tails and other large raptors.
Like many birds of prey, red-shouldered hawks nest in late winter or early spring; 2-4 eggs are generally laid in a bulky nest, high in a tree, and are incubated by both parents. The young hatch within a month and are usually self-sufficient by summer. While most red-shouldered hawks are nonmigratory, those that nest in northern portions of their range often winter in the southern U.S. or in Mexico.
Jumat, 24 Desember 2010
White Christmas
Caught between high pressure over the Northern Plains and low pressure over the Texas Panhandle, we are getting our Christmas snow here in Missouri. The low is sweeping Gulf moisture in from the south while flow around the high is bringing colder air down from the north; the latter will hang around for several days, assuring us of a White Christmas.
The snow began overnight and has already dropped a few inches of wet snow on the frozen ground; by tomorrow morning, we may have half a foot or more and it will look very much like the Christmas Day that most Americans hope to experience. Snug in our heated homes, we can look out on the winter scene with no sense of alarm and, of course, children will enjoy romping through or sledding over nature's blanket.
Though challenged by the snow cover, wildlife are well equipped to survive its presence; the feeder sites will be especially busy but our winter birds would manage just fine without the handouts. Some mammals will den up until conditions improve while predators may actually benefit from the snowfall, their prey more conspicuous against a background of white. Whether challenged by the storm or not, it is safe to say that wild creatures do not share our sentimental view of a White Christmas; they will carry on with their life-long struggle, surviving one day at a time.
The snow began overnight and has already dropped a few inches of wet snow on the frozen ground; by tomorrow morning, we may have half a foot or more and it will look very much like the Christmas Day that most Americans hope to experience. Snug in our heated homes, we can look out on the winter scene with no sense of alarm and, of course, children will enjoy romping through or sledding over nature's blanket.
Though challenged by the snow cover, wildlife are well equipped to survive its presence; the feeder sites will be especially busy but our winter birds would manage just fine without the handouts. Some mammals will den up until conditions improve while predators may actually benefit from the snowfall, their prey more conspicuous against a background of white. Whether challenged by the storm or not, it is safe to say that wild creatures do not share our sentimental view of a White Christmas; they will carry on with their life-long struggle, surviving one day at a time.
Kamis, 23 Desember 2010
The Pineapple Express
Produced by an atmospheric trough over the eastern Pacific, the Pineapple Express is a plume of deep, tropical moisture that is swept into the western edge of North America. Developing ahead the the trough's leading cold front and reinforced by circulation around high pressure to the southeast, this flow of warm, humid air, which originates near Hawaii, is forced to rise as it invades the Continent, producing heavy valley rains and dropping copious snow across higher terrain.
In most cases, the plume first strikes the Pacific Northwest; as the trough advances eastward and the angle of its cold front changes, the stream of moisture moves southward, through California and into Mexico. Should the front become stationary, as it did earlier this week, the onshore flow of tropical moisture may continue for several days, producing floods, mud slides, avalanches and great skiing conditions from the Coastal Ranges to the Rockies.
Once the trough moves across the western edge of North America, the Pineapple Express is shut off and cooler, drier air invades from the northwest. While other cold fronts may follow in its wake, they cannot tap the tropical moisture until the original trough moves further eastward and a ridge of high pressure reprimes the atmosphere.
In most cases, the plume first strikes the Pacific Northwest; as the trough advances eastward and the angle of its cold front changes, the stream of moisture moves southward, through California and into Mexico. Should the front become stationary, as it did earlier this week, the onshore flow of tropical moisture may continue for several days, producing floods, mud slides, avalanches and great skiing conditions from the Coastal Ranges to the Rockies.
Once the trough moves across the western edge of North America, the Pineapple Express is shut off and cooler, drier air invades from the northwest. While other cold fronts may follow in its wake, they cannot tap the tropical moisture until the original trough moves further eastward and a ridge of high pressure reprimes the atmosphere.
Senin, 20 Desember 2010
Merry Consumption!
It's the most wonderful time of the year....especially for retailers. Pressured by tradition and expectations, Christians of all kind, from timid secular participants to evangelical zealots, invade the malls, spending lavishly to shower one another with the latest outfits and gadgets. Though bought with loved ones in mind, the gifts also soothe the mind of the purchaser, who must fight the guilt that pervades this season.
While born of a simple story about a charismatic figure who, by all accounts, led a spartan life, Christmas has become a three-month event, focused on extravagant consumption. Some might argue that this annual frenzy, instigated by Big Business and promoted by its army of advertisers, is crucial to the global economy but, in the end, those of us in "developed" countries receive far more than we truly need.
Excess consumption, combined with unbridled population growth, is perhaps the greatest threat to natural ecosystems across our planet. The acquisition of raw materials, the industrial production of consumer goods, the transportation of those products, the trashing of unwanted or used items and secondary pollution at all stages of this cycle degrade the health of our environment. Learning to live with less is the ultimate key to conservation.
While born of a simple story about a charismatic figure who, by all accounts, led a spartan life, Christmas has become a three-month event, focused on extravagant consumption. Some might argue that this annual frenzy, instigated by Big Business and promoted by its army of advertisers, is crucial to the global economy but, in the end, those of us in "developed" countries receive far more than we truly need.
Excess consumption, combined with unbridled population growth, is perhaps the greatest threat to natural ecosystems across our planet. The acquisition of raw materials, the industrial production of consumer goods, the transportation of those products, the trashing of unwanted or used items and secondary pollution at all stages of this cycle degrade the health of our environment. Learning to live with less is the ultimate key to conservation.
Sabtu, 18 Desember 2010
A Morning of Raptors
Venus gleamed brightly in the eastern sky as I drove to our meeting site for the annual Christmas Bird Count. Our group, as usual, was assigned an area south of Columbia that extends from wooded uplands down to the banks of the Missouri; most of this territory is covered by rolling terrain with forested hills, rocky creek channels and valley farms.
The theme for this year's count was set when we heard and spotted two barred owls just before dawn. Clear skies and a minimal wind provided a perfect, if chilly, morning for birding and a large number of species were logged; but this was a morning for raptors. Not long after finding the barred owls, we encountered six bald eagles (5 adults and 1 immature) along the Missouri River, which was nearly covered with floating chunks of ice. As usual, red-tailed hawks were common above and along the farms fields and, today, were matched in number by red-shouldered hawks, which perched in wooded meadows. A sharp-shinned hawk streaked across the road, in pursuit of songbirds, a Cooper's hawk scattered a large flock of cedar waxwings and an American kestrel hunted from a rural powerline. Finally, a seventh bald eagle (another adult) soared above a wetland area, far from the wide Missouri.
Accepting this raptor bonanza to be a hopeful sign, I agreed to trudge up to an abandoned barn to see if it just might harbor a barn owl, an increasingly uncommon species in the American heartland. Alas, the old structure was empty but this morning of raptors will long hold a place in my memory.
The theme for this year's count was set when we heard and spotted two barred owls just before dawn. Clear skies and a minimal wind provided a perfect, if chilly, morning for birding and a large number of species were logged; but this was a morning for raptors. Not long after finding the barred owls, we encountered six bald eagles (5 adults and 1 immature) along the Missouri River, which was nearly covered with floating chunks of ice. As usual, red-tailed hawks were common above and along the farms fields and, today, were matched in number by red-shouldered hawks, which perched in wooded meadows. A sharp-shinned hawk streaked across the road, in pursuit of songbirds, a Cooper's hawk scattered a large flock of cedar waxwings and an American kestrel hunted from a rural powerline. Finally, a seventh bald eagle (another adult) soared above a wetland area, far from the wide Missouri.
Accepting this raptor bonanza to be a hopeful sign, I agreed to trudge up to an abandoned barn to see if it just might harbor a barn owl, an increasingly uncommon species in the American heartland. Alas, the old structure was empty but this morning of raptors will long hold a place in my memory.
Jumat, 17 Desember 2010
The Scent of Skunk
In winter, cold, dry air and frozen ground suppress most of nature's fragrance. One potent exception is the scent of skunk musk, which wafts through the air and is detectable by our relatively poor olfactory system for up to a mile from its source.
Skunks, members of the Mephitidae Family, are represented by at least ten species across the globe, most of which are native to the Americas. Omniverous and crepuscular, skunks roam about to feast on a wide variety of plants, small animals, eggs, garbage and carrion; guided by an excellent sense of smell but hampered by poor eyesight, they represent a large portion of our roadkill. Of course, it is their volatile and irritating musk that wards off many natural predators (great horned owls excluded); produced in perianal glands and found to contain a mix of sulfur-containing thiols, this noxious musk can be accurately ejected for up to 15 feet. Mustelids (weasels, otters, martens, badgers and wolverines) have similar musk glands but, in comparison with skunks, their glands are less developed and their musk is less potent.
Hikers and homeowners have little to fear from these docile creatures; their poor eyesight does not permit planned attacks and they use their musk only in defense. Most often encountered during their mating season in late winter or early spring, skunks spend much of the winter in communal dens, venturing out during periods of relatively mild weather. After mating, females dig their own burrows and give birth to 4-6 kits by May; they will stay with her through the summer, learning to find food and striking fear in potential predators that associate their distinctive coats with foul, irritating showers of musk.
Skunks, members of the Mephitidae Family, are represented by at least ten species across the globe, most of which are native to the Americas. Omniverous and crepuscular, skunks roam about to feast on a wide variety of plants, small animals, eggs, garbage and carrion; guided by an excellent sense of smell but hampered by poor eyesight, they represent a large portion of our roadkill. Of course, it is their volatile and irritating musk that wards off many natural predators (great horned owls excluded); produced in perianal glands and found to contain a mix of sulfur-containing thiols, this noxious musk can be accurately ejected for up to 15 feet. Mustelids (weasels, otters, martens, badgers and wolverines) have similar musk glands but, in comparison with skunks, their glands are less developed and their musk is less potent.
Hikers and homeowners have little to fear from these docile creatures; their poor eyesight does not permit planned attacks and they use their musk only in defense. Most often encountered during their mating season in late winter or early spring, skunks spend much of the winter in communal dens, venturing out during periods of relatively mild weather. After mating, females dig their own burrows and give birth to 4-6 kits by May; they will stay with her through the summer, learning to find food and striking fear in potential predators that associate their distinctive coats with foul, irritating showers of musk.
Kamis, 16 Desember 2010
Great Gray Owls
One of the least conspicuous birds in North America, the great gray owl inhabits the boreal forests of Alaska and Canada and the mountain forests of the Cascades, Northern Sierra Nevada and Northern Rockies; during the winter months, they may also be encountered in Minnesota and northern New England. Preferring dense, coniferous woodlands, they hunt primarily at night but become increasingly crepuscular or diurnal during the colder months of the year; it is then that they are most often observed, perched on a limb that overlooks a forest clearing. While this owl is seldom seen, its deep, resonant hoots often echo through remote northern forests.
Though great grays are our largest owls by length and wingspan (the latter may be up to 5 feet), they are not as heavy as great horned owls; their large head and prominant, ringed facial disc accentuate their size and make their yellow eyes appear to be small and closely spaced. Despite their size, great grays are not overly aggressive and feed primarily on small rodents (mice, voles, hares), grouse and songbirds.
Adult great gray owls have little to fear from natural predators (lynx are among their few adversaries) but their young (born in mid-late spring) may fall victim to goshawks, fishers, wolverines, lynx or bears. Indeed, the adults are more endangered by the activity of man, who drains the bogs and logs the forests that provide refuge to this ghost of the Great Northwoods.
Though great grays are our largest owls by length and wingspan (the latter may be up to 5 feet), they are not as heavy as great horned owls; their large head and prominant, ringed facial disc accentuate their size and make their yellow eyes appear to be small and closely spaced. Despite their size, great grays are not overly aggressive and feed primarily on small rodents (mice, voles, hares), grouse and songbirds.
Adult great gray owls have little to fear from natural predators (lynx are among their few adversaries) but their young (born in mid-late spring) may fall victim to goshawks, fishers, wolverines, lynx or bears. Indeed, the adults are more endangered by the activity of man, who drains the bogs and logs the forests that provide refuge to this ghost of the Great Northwoods.
Rabu, 15 Desember 2010
Winter Farmlands
Yesterday afternoon, the farmlands east of Columbia presented a bleak winter landscape; snow covered the ground, dead corn stubble and dry, yellow grass quivered in a cold, east wind, dark, barren woodlands shrouded the stream channels and a flat, gray sky diffused and scattered the weak winter sunlight. Were it not for the occasional grove of eastern cedars, one could have painted the scene in black and white.
Amidst this harsh and forbidding environment, one might not expect to see much wildlife but they would be wrong. As expected, raptors dominated the scene; red-tailed hawks surveyed the grasslands from the barren trees, northern harriers skimmed above the cropfields and American kestrels hunted from the powerlines. Skeins of Canada geese moved across the sky, eastern meadowlarks streamed across the roadways and large flocks of blackbirds settled in the fields. Dark-eyed juncos and white-crowned sparrows combed the roadside thickets, eastern bluebirds and mourning doves perched on the fences and northern mockingbirds flashed across the barnyards. Stopping near the woodlots, I observed the usual mix of winter residents (chickadees, woodpeckers, cardinals, blue jays) and, if I had stayed until dusk, there is little doubt that deer, fox and coyotes would have appeared on the snow-covered meadows.
By late afternoon, a band of pink and gold stretched across the western horizon, a sign that tomorrow might be a brighter day. The wildlife, of course, focused on survival, pay no heed to such signs of hope; driven by instinct, they live in the present and have no inclination or ability to anticipate the future. Indeed, in the fickle world of nature, tomorrow is never assured.
Amidst this harsh and forbidding environment, one might not expect to see much wildlife but they would be wrong. As expected, raptors dominated the scene; red-tailed hawks surveyed the grasslands from the barren trees, northern harriers skimmed above the cropfields and American kestrels hunted from the powerlines. Skeins of Canada geese moved across the sky, eastern meadowlarks streamed across the roadways and large flocks of blackbirds settled in the fields. Dark-eyed juncos and white-crowned sparrows combed the roadside thickets, eastern bluebirds and mourning doves perched on the fences and northern mockingbirds flashed across the barnyards. Stopping near the woodlots, I observed the usual mix of winter residents (chickadees, woodpeckers, cardinals, blue jays) and, if I had stayed until dusk, there is little doubt that deer, fox and coyotes would have appeared on the snow-covered meadows.
By late afternoon, a band of pink and gold stretched across the western horizon, a sign that tomorrow might be a brighter day. The wildlife, of course, focused on survival, pay no heed to such signs of hope; driven by instinct, they live in the present and have no inclination or ability to anticipate the future. Indeed, in the fickle world of nature, tomorrow is never assured.
Selasa, 14 Desember 2010
Mourning Dove Sit-In
Faced with snow-covered ground and an invasion of Arctic air, mourning doves have gathered in our large magnolia over the past two days; since this tree is on the south side of our house, it is protected from the cold north wind and receives plenty of sun, even in the winter.
Like many bird species, mourning doves form large, sociable flocks during the colder months but, unlike the others, these mellow birds assemble with little fanfare. Were it not for their distinctive forms, huddled in groups on the bare branches, one could easily overlook them. Content to watch their high strung neighbors as they squabble over the nearby feeder, the doves sit patiently, basking in the sun and waiting to partake of seed that falls to the ground. If not spooked by a sharp-shinned hawk, they may sit there all afternoon, heads on chests, oblivious to the winter chill.
Their peaceful sit-ins are a welcome sight during this trying season; the tranquility is infectious and their calm, polite demeanor is especially reassuring in the midst of our holiday frenzy. The doves remind us to stop and enjoy the moment; life is too short to be rushing through its fickle course.
Like many bird species, mourning doves form large, sociable flocks during the colder months but, unlike the others, these mellow birds assemble with little fanfare. Were it not for their distinctive forms, huddled in groups on the bare branches, one could easily overlook them. Content to watch their high strung neighbors as they squabble over the nearby feeder, the doves sit patiently, basking in the sun and waiting to partake of seed that falls to the ground. If not spooked by a sharp-shinned hawk, they may sit there all afternoon, heads on chests, oblivious to the winter chill.
Their peaceful sit-ins are a welcome sight during this trying season; the tranquility is infectious and their calm, polite demeanor is especially reassuring in the midst of our holiday frenzy. The doves remind us to stop and enjoy the moment; life is too short to be rushing through its fickle course.
Senin, 13 Desember 2010
Night of the Geminids
While not as famous as the Perseids of August or the Leonids of November, the Geminid meteors of December offer the most reliable display of the year. Produced by debris from the 3200 Phaethon asteroid, discovered in 1983, the Geminid meteors were first observed by a British astronomer in 1862, making them the youngest of the annual meteor showers; indeed, most of the other major displays, produced by debris from comets, have been documented for thousands of years (and have likely occurred much longer than that).
The Geminid debris field is the largest that Earth encounters in its annual journey around the sun. Up to 160 meteors may be seen in the course of an hour, seeming to radiate from the Gemini constellation; since they are relatively slow moving (compared to meteors in other displays) and since they tend to leave a vapor trail, the Geminids are also the easiest to observe.
Occurring from December 6 to December 19, the Geminid meteor show peaks on the nights of the 13th and 14th; as with all meteor displays, they are best observed on clear, moonless nights, away from the glow of city lights. Fortunately, astronomers project that the Geminid display will intensify over the coming years as Earth's orbit more directly intersects the path of the parent asteroid.
The Geminid debris field is the largest that Earth encounters in its annual journey around the sun. Up to 160 meteors may be seen in the course of an hour, seeming to radiate from the Gemini constellation; since they are relatively slow moving (compared to meteors in other displays) and since they tend to leave a vapor trail, the Geminids are also the easiest to observe.
Occurring from December 6 to December 19, the Geminid meteor show peaks on the nights of the 13th and 14th; as with all meteor displays, they are best observed on clear, moonless nights, away from the glow of city lights. Fortunately, astronomers project that the Geminid display will intensify over the coming years as Earth's orbit more directly intersects the path of the parent asteroid.
Minggu, 12 Desember 2010
Backside Blizzard
In the Northern Hemisphere, as storm systems track from west to east, the winds around their center of low pressure move counterclockwise. Ahead of the storm, southerly winds pump warm, humid air into the system, triggering showers and thunderstorms as the cold front approaches. North of the storm's center, this moisture is pulled into cold air behind the front, producing cool rain or snow, depending on the temperature of that air. If the storm is especially strong, determined by the depth of its central pressure, the circulating winds can be fierce and, when combined with snowfall, may produce blizzard conditions on the north and west sides of the system.
The current winter storm, centered over Lake Michigan this morning, is very potent. Its vanguard of showers and mild air flowed across Missouri on Friday, extending into Saturday morning; by Saturday afternoon, cold air was filtering in from the north and, by last evening, snow showers mixed with a gusty northwest wind. The strong winds and snowfall increased through the night, producing blizzards of horizontal snow and pulsations of wind that roared through the barren trees. By morning, we had 4 inches of fresh powder, blown clear in some areas and piled into deeper drifts in others.
It is now almost noon; the storm has moved to the east, the winds have died down and a snowy landscape reflects a bright southern sun; the temperature sits at 18 degrees F. Travel will be slow and shoveling will be necessary but we have survived another round of nature's fury.
The current winter storm, centered over Lake Michigan this morning, is very potent. Its vanguard of showers and mild air flowed across Missouri on Friday, extending into Saturday morning; by Saturday afternoon, cold air was filtering in from the north and, by last evening, snow showers mixed with a gusty northwest wind. The strong winds and snowfall increased through the night, producing blizzards of horizontal snow and pulsations of wind that roared through the barren trees. By morning, we had 4 inches of fresh powder, blown clear in some areas and piled into deeper drifts in others.
It is now almost noon; the storm has moved to the east, the winds have died down and a snowy landscape reflects a bright southern sun; the temperature sits at 18 degrees F. Travel will be slow and shoveling will be necessary but we have survived another round of nature's fury.
Jumat, 10 Desember 2010
Cheshire Moon
Stepping onto the deck last evening, I caught sight of the crescent moon, turned on its back in the western sky. Catching the orange glow of the setting sun and looming just above a branch of our neighbor's tree, it evoked the grin of the Cheshire Cat, Alice's friend and nemesis.
Both enamored with and frightened by the winter night, humans, like Alice in Wonderland, have long confronted its mysteries and threats. Natives of the Tropics, we are poorly equipped to survive the harsh conditions of winter and, devoid of night vision, we remain at the mercy of creatures that patrol its darkness. And the night sky, with its fabulous cast of glowing objects, has long inspired and threatened man, prompting us to imagine figures and omens in its pattern of moving lights.
As the Cheshire Moon dropped toward the horizon, I turned my attention to bright Jupiter, high in the southern sky, and to the other constellations that adorn our winter nights. Despite our advanced scientific knowledge, we have only begun to understand the worlds beyond our own. One day, if we do not destroy our own civilization first, we will step through the looking glass to explore the rest of our Universe.
Both enamored with and frightened by the winter night, humans, like Alice in Wonderland, have long confronted its mysteries and threats. Natives of the Tropics, we are poorly equipped to survive the harsh conditions of winter and, devoid of night vision, we remain at the mercy of creatures that patrol its darkness. And the night sky, with its fabulous cast of glowing objects, has long inspired and threatened man, prompting us to imagine figures and omens in its pattern of moving lights.
As the Cheshire Moon dropped toward the horizon, I turned my attention to bright Jupiter, high in the southern sky, and to the other constellations that adorn our winter nights. Despite our advanced scientific knowledge, we have only begun to understand the worlds beyond our own. One day, if we do not destroy our own civilization first, we will step through the looking glass to explore the rest of our Universe.
Selasa, 07 Desember 2010
Life, Dinosaurs & Time
Life first appeared in Earth's primordial seas some 3.6 billion years ago and evolved into a wide diversity of marine and terrestrial creatures before dinosaurs arose. Unicellular organisms, echinoderms, mollusks, insects, arachnids, crustaceans, fish, sharks, mosses, ferns, conifers, amphibians and many reptiles appeared before the dinosaurs and continue to evolve today.
Dinosaurs ruled our planet throughout the Mesozoic, which stretched from 225 to 65 million years ago (MYA), but other life forms also arose during that Era. Turtles, crocodilians and the earliest mammals appeared in the Triassic Period (225-190 MYA), ancestral birds and flowering plants graced the Jurassic Period (190-135 MYA) and the Cretaceous Period (135-65 MYA) witnessed the rise of ants, social bees, snakes, marsupials and the first deciduous trees.
Since the end of the Mesozoic (65 MYA), when dinosaurs became extinct, these "terrible lizards" live on as birds and Earth's mammals have exploded in number and variety. Primates, bats, cetaceans, manatees, rodents, canids, felines, ruminants, horses and essentially all of our modern mammals arose after the Age of Dinosaurs. Hominids have walked the Earth for no more than 6 million years and the human species is less than 150,000 years old.
Dinosaurs ruled our planet throughout the Mesozoic, which stretched from 225 to 65 million years ago (MYA), but other life forms also arose during that Era. Turtles, crocodilians and the earliest mammals appeared in the Triassic Period (225-190 MYA), ancestral birds and flowering plants graced the Jurassic Period (190-135 MYA) and the Cretaceous Period (135-65 MYA) witnessed the rise of ants, social bees, snakes, marsupials and the first deciduous trees.
Since the end of the Mesozoic (65 MYA), when dinosaurs became extinct, these "terrible lizards" live on as birds and Earth's mammals have exploded in number and variety. Primates, bats, cetaceans, manatees, rodents, canids, felines, ruminants, horses and essentially all of our modern mammals arose after the Age of Dinosaurs. Hominids have walked the Earth for no more than 6 million years and the human species is less than 150,000 years old.
Senin, 06 Desember 2010
Eastern White Pines
It is during the winter, when the deciduous trees are bare, that we pay most attention to the conifers. But, since I park by pickup beneath a large white pine at our Columbia home, I find it hard to ignore this tree in any season. In spring, its small staminate flowers release a copious amount of yellow pollen which coats the truck; soon thereafter the spongy flowers begin to fall, collecting in the bed or along the base of the windshield. Drops of pine sap leave sticky residue on the hood throughout the year and heaps of yellowing pine needles surround the pickup in mid autumn.
Eastern white pines, the largest conifers in eastern North America, are native to southern Canada, New England, Pennsylvania, and the Great Lake States, extending southward along the Appalachian chain. Widely planted as ornamentals, these stately trees were once used for sail masts and are now harvested for lumber or used as Christmas trees. Often growing up to 100 feet tall and possessing a girth that may exceed 10-15 feet, some white pines in virgin stands exceed 200 feet in height. Those that escape browsing, disease or human harvesting may live for 250 years and a few specimens are known to be nearly 500 years old.
Due to their relatively long needles (bundled in groups of 5) and the open spacing of their limbs, eastern white pines have an airy appearance. Their 6-inch cones peak in number every 3-5 years and bear seeds that are favored by tree squirrels, pine siskins, nuthatches, crossbills and a variety of finches. Moderately resistant to fire, white pines often form extensive stands in undisturbed areas, overgrowing and shading out their smaller deciduous neighbors. My pickup truck and I can certainly vouch for their rapid growth and prolific nature!
Eastern white pines, the largest conifers in eastern North America, are native to southern Canada, New England, Pennsylvania, and the Great Lake States, extending southward along the Appalachian chain. Widely planted as ornamentals, these stately trees were once used for sail masts and are now harvested for lumber or used as Christmas trees. Often growing up to 100 feet tall and possessing a girth that may exceed 10-15 feet, some white pines in virgin stands exceed 200 feet in height. Those that escape browsing, disease or human harvesting may live for 250 years and a few specimens are known to be nearly 500 years old.
Due to their relatively long needles (bundled in groups of 5) and the open spacing of their limbs, eastern white pines have an airy appearance. Their 6-inch cones peak in number every 3-5 years and bear seeds that are favored by tree squirrels, pine siskins, nuthatches, crossbills and a variety of finches. Moderately resistant to fire, white pines often form extensive stands in undisturbed areas, overgrowing and shading out their smaller deciduous neighbors. My pickup truck and I can certainly vouch for their rapid growth and prolific nature!
Minggu, 05 Desember 2010
Evolution of the Sonoran Desert
The Sonoran Desert of the Southwest U.S. and Northwest Mexico is a product of its latitude, the global climate and the regional topography. Lying along one of the desert bands (which run just north and just south of the Tropics), this arid ecosystem receives copious sunshine and is subjected to prolonged periods of high pressure, below which the air is sinking. This atmospheric condition retards cloud formation and both warms and dries the air as it plummets toward the Earth's surface.
Covering a broad basin and surrounded by highlands, the Sonoran Desert is shielded from moisture in all directions; to the northwest are the Sierra Nevada Mountains and the high Mojave Desert, to the north and east is the Mogollon Rim of the Colorado Plateau, to the southeast is the wall of the Sierra Madre Range and, to the southwest, are the mountains of Southern California and the Baja Peninsula. Any air that enters the Sonoran is thus downsloping from higher terrain, causing it to heat up and dry out even further. Since the mountains and plateaus that surround it were uplifted within the past 4 to 20 million years (during the Miocene and Pliocene), the Sonoran Desert is one of the youngest ecosystems on our planet.
Throughout the Pleistocene and into the Holocene, Earth's climate has undergone dramatic shifts. When the climate cooled and glaciers advanced, the area of the Sonoran Desert decreased; in contrast, when the climate warmed (as it has done over the past 10,000 years), the Desert advanced, climbing onto the walls of the adjacent highlands. Throughout these gyrations, the regional flora and fauna have evolved, developing traits that enhanced survival in an arid environment with intense sunshine, cool nights and seasonal rains.
Covering a broad basin and surrounded by highlands, the Sonoran Desert is shielded from moisture in all directions; to the northwest are the Sierra Nevada Mountains and the high Mojave Desert, to the north and east is the Mogollon Rim of the Colorado Plateau, to the southeast is the wall of the Sierra Madre Range and, to the southwest, are the mountains of Southern California and the Baja Peninsula. Any air that enters the Sonoran is thus downsloping from higher terrain, causing it to heat up and dry out even further. Since the mountains and plateaus that surround it were uplifted within the past 4 to 20 million years (during the Miocene and Pliocene), the Sonoran Desert is one of the youngest ecosystems on our planet.
Throughout the Pleistocene and into the Holocene, Earth's climate has undergone dramatic shifts. When the climate cooled and glaciers advanced, the area of the Sonoran Desert decreased; in contrast, when the climate warmed (as it has done over the past 10,000 years), the Desert advanced, climbing onto the walls of the adjacent highlands. Throughout these gyrations, the regional flora and fauna have evolved, developing traits that enhanced survival in an arid environment with intense sunshine, cool nights and seasonal rains.
Sabtu, 04 Desember 2010
Madagascar and its Primates
As Pangea continued to break apart, Madagascar split from Africa, some 160 million years ago. Drifting to the south, it merged with the remnants of Gondwanaland, the combined mass of Antarctica, India and Australia. There, its African flora and fauna mingled with the plants and animals of that tropical land mass. About 95 million years ago, the India-Madagascar segment broke from Antarctica-Australia, moving to the northeast; within another 15 million years, Madagascar began to rift from India, presumably triggered by an underlying hotspot that also produced the massive Deccan Traps basalt flow at the end of the Mesozoic. By 70 million years ago, Madagascar was moving into prolonged isolation and now rests 350 miles off the southeast coast of Africa.
While the earliest mammals arose during the Triassic, more than 200 million years ago, primates first appeared late in the Cretaceous, after Madagascar had become an isolated land mass. About 60 million years ago, these ancestral primates split into the prosimian line (which led to lemurs, lorises, galagos and pottos) and the anthrapoid line (leading to monkeys, apes and hominids). Spreading across the globe these two groups shared similar habitats and, over time, the anthrapoids were more successful, pushing the prosimians toward extinction.
According to current scientific theory, ancestral lemurs reached Madagascar on rafts of vegetation, torn from the African coast by seasonal storms. There, free from anthrapoid competition, they have flourished and, today, are represented by more than 100 species and subspecies. A second primate, humans, reached Madagascar by boat, colonizing the Earth's fourth largest island about 2000 years ago. Unfortunately, the Malagasy and their descendents have since destroyed much of the natural habitat; lemurs and other Madagascar animals, 80% of which are endemic to the island, are increasingly threatened by deforestation and other human activity.
While the earliest mammals arose during the Triassic, more than 200 million years ago, primates first appeared late in the Cretaceous, after Madagascar had become an isolated land mass. About 60 million years ago, these ancestral primates split into the prosimian line (which led to lemurs, lorises, galagos and pottos) and the anthrapoid line (leading to monkeys, apes and hominids). Spreading across the globe these two groups shared similar habitats and, over time, the anthrapoids were more successful, pushing the prosimians toward extinction.
According to current scientific theory, ancestral lemurs reached Madagascar on rafts of vegetation, torn from the African coast by seasonal storms. There, free from anthrapoid competition, they have flourished and, today, are represented by more than 100 species and subspecies. A second primate, humans, reached Madagascar by boat, colonizing the Earth's fourth largest island about 2000 years ago. Unfortunately, the Malagasy and their descendents have since destroyed much of the natural habitat; lemurs and other Madagascar animals, 80% of which are endemic to the island, are increasingly threatened by deforestation and other human activity.
Jumat, 03 Desember 2010
The Voice of Winter
Winter is the quiet season. Compared with the rest of the year, there are relatively few natural sounds that greet us on our excursions through the fields and woodlands. Of course, exceptions do exist: the crunch of snow beneath our boots, the rattling of limbs in the winter wind, the rustling of dead oak leaves and the dreaded sound of sleet, coating our cars and walkways. The wild creatures chime in now and then: the howl of coyotes, the eerie bark of fox, the cheerful tune of chickadees, the drumming of woodpeckers and the raucous cries of jays and crows come to mind. But, for me, the voice of winter is the gruff call of the great horned owl.
Oblivious to the ice, snow and frigid air and well equipped to stalk the long, dark nights, this large and powerful predator symbolizes the harsh winter season and epitomizes the survival skills that it demands. Hidden from view for much of the day, great horned owls appear along wood borders in the gathering dusk, ready for a night of hunting. They have a distinct advantage during the barren months of winter, ensuring good health for their breeding season, which will commence by January.
Ominous to many, their deep, echoing hoots inspire those of us who appreciate the hardiness and stamina of our wild winter residents. It is understandable that mice, cottontails and other small mammals may not share that appreciation.
Oblivious to the ice, snow and frigid air and well equipped to stalk the long, dark nights, this large and powerful predator symbolizes the harsh winter season and epitomizes the survival skills that it demands. Hidden from view for much of the day, great horned owls appear along wood borders in the gathering dusk, ready for a night of hunting. They have a distinct advantage during the barren months of winter, ensuring good health for their breeding season, which will commence by January.
Ominous to many, their deep, echoing hoots inspire those of us who appreciate the hardiness and stamina of our wild winter residents. It is understandable that mice, cottontails and other small mammals may not share that appreciation.
Kamis, 02 Desember 2010
The Benefits of Aging
Aging has its disadvantages. Our physical strength and stamina tend to deteriorate, we are more prone to a variety of illnesses and, for some, our mental faculties begin to fail. When we reach middle age, we begin to notice the early signs of aging and, combined with the other stressors of that period, this observation can induce a sense of resignation and cause some to give up on the joys of life.
But those who remain active, both physically and mentally, come to realize that there are also benefits of growing older. For most of us, the responsibilities of our career and our family life begin to disipate and we have more time to engage in exercise, hobbies and other personal interests. Those endowed with creativity are especially rewarded by this age-induced freedom; indeed, history is replete with famous writers, painters, photographers and other artisans who took up their passion later in life and, possessing the experience and wisdom of advanced age, were especially productive and successful.
Whether or not you possess such talents, the decision to engage in new activities will likely benefit your physical and mental health. The process of learning a new skill exercises the brain and the body, enhancing mental function, improving coordination and inducing a sense of personal satisfaction, all of which make us less prone to illness and injury. Death is surely inevitable but growing old can have its rewards.
But those who remain active, both physically and mentally, come to realize that there are also benefits of growing older. For most of us, the responsibilities of our career and our family life begin to disipate and we have more time to engage in exercise, hobbies and other personal interests. Those endowed with creativity are especially rewarded by this age-induced freedom; indeed, history is replete with famous writers, painters, photographers and other artisans who took up their passion later in life and, possessing the experience and wisdom of advanced age, were especially productive and successful.
Whether or not you possess such talents, the decision to engage in new activities will likely benefit your physical and mental health. The process of learning a new skill exercises the brain and the body, enhancing mental function, improving coordination and inducing a sense of personal satisfaction, all of which make us less prone to illness and injury. Death is surely inevitable but growing old can have its rewards.
Rabu, 01 Desember 2010
December
A northwest wind developed yesterday afternoon, behind the latest cold front, and, overnight, ushered in the coldest air and lowest wind chill since last winter. December made its appearance beneath a frigid, clear sky, lit by a crescent moon, bright Venus and a bowl of twinkling stars. On my walk to work this morning, it was 22 degrees F.
Festooned with holiday lights and leading up to the beloved season of Christmas, December does not incite the animosity that January and February stir in the soul of tropical man. Nevertheless, in the Northern Hemisphere, December is the darkest month of the year and often brings severe winter weather. Even when relatively mild, the month heralds the long, steady descent toward the nadir of nature's year.
December 1 marks the calendar and meteorologic onset of winter which, from an astronomical point of view, begins with the winter solstice, on or about December 21. One can debate when the season officially begins but, to paraphrase a Supreme Court Justice, "we know it when we feel it" and, today, it felt like winter.
Festooned with holiday lights and leading up to the beloved season of Christmas, December does not incite the animosity that January and February stir in the soul of tropical man. Nevertheless, in the Northern Hemisphere, December is the darkest month of the year and often brings severe winter weather. Even when relatively mild, the month heralds the long, steady descent toward the nadir of nature's year.
December 1 marks the calendar and meteorologic onset of winter which, from an astronomical point of view, begins with the winter solstice, on or about December 21. One can debate when the season officially begins but, to paraphrase a Supreme Court Justice, "we know it when we feel it" and, today, it felt like winter.
Minggu, 28 November 2010
South of Town
North of Columbia, the landscape soon gives way to the relatively flat terrain of the Glacial Plain that covers much of the Midwest, from central Ohio to the eastern Dakotas. But south of town, one encounters the rolling hills, bluffs and floodplain of the Missouri River Valley; it is a landscape of wooded slopes, hilltop meadows and valley farms, all sloping toward a broad, flat swath of cropfields, wetlands, bottomland woods and the River itself.
On this bright, cloudless morning, I journeyed through this landscape, winding along graveled roads and stopping now and then to observe the changing scenery. Mourning doves and eastern bluebirds huddled on the powerlines, blue jays, mockingbirds and cardinals flashed across the roadways and mixed flocks of juncos and winter sparrows scattered from the roadside thickets. Red-tailed hawks circled above the frosted fields and an occasional red-shouldered hawk patrolled from a barren tree. Though common in this habitat, wild turkeys had not yet left their forest retreats, leaving the meadows and corn stubble to herds of livestock and flocks of Canada geese.
Down on the floodplain, noisy killdeer raced along the mudflats, crows foraged in the crop fields and a lone bald eagle surveyed the scene from a riverside grove. A steady south wind negated my opportunity to observe migrant snow geese but distant, high clouds, off to the northwest, foretold of an approaching storm. That front, due tomorrow, will reinforce the winter season and another wave of snow geese will ride its northerly wind across the Heartland.
On this bright, cloudless morning, I journeyed through this landscape, winding along graveled roads and stopping now and then to observe the changing scenery. Mourning doves and eastern bluebirds huddled on the powerlines, blue jays, mockingbirds and cardinals flashed across the roadways and mixed flocks of juncos and winter sparrows scattered from the roadside thickets. Red-tailed hawks circled above the frosted fields and an occasional red-shouldered hawk patrolled from a barren tree. Though common in this habitat, wild turkeys had not yet left their forest retreats, leaving the meadows and corn stubble to herds of livestock and flocks of Canada geese.
Down on the floodplain, noisy killdeer raced along the mudflats, crows foraged in the crop fields and a lone bald eagle surveyed the scene from a riverside grove. A steady south wind negated my opportunity to observe migrant snow geese but distant, high clouds, off to the northwest, foretold of an approaching storm. That front, due tomorrow, will reinforce the winter season and another wave of snow geese will ride its northerly wind across the Heartland.
Jumat, 26 November 2010
Swans over the South Platte
Not inclined to join the mob scene at area malls and presented with another mild, sunny morning along the Front Range, my wife and I decided to take a hike along the South Platte River. A series of cold nights have coated many of the smaller ponds with a sheet of ice and wintering waterfowl are now congregating along the river and its adjacent lakes.
Joining the permanent residents (mallards, gadwalls, Canada geese, wood ducks, northern shovelers, American wigeon and common mergansers) were an excellent variety of winter residents and visitors; these included buffleheads, common goldeneyes, American coot, hooded mergansers, lesser scaup, green-winged teal and ring-necked ducks. On our walk through the South Platte Valley we also encountered belted kingfishers, northern flickers, red-tailed hawks, a lone rough-legged hawk, black-billed magpies, great blue herons, ring-billed gulls, song sparrows, red-winged blackbirds and an industrious muskrat.
But the highlight of this November morning was a flock of tundra swans, winging their way toward Chatfield Reservoir. All eight were in full adult plumage and were unusually silent on their graceful flight above the South Platte. After breeding on the Arctic tundra of Alaska and northern Canada, most tundra swans winter on estuaries along the mid Atlantic and Pacific Coasts; smaller numbers migrate through the interior, heading for the marshlands of New Mexico and Texas.
Joining the permanent residents (mallards, gadwalls, Canada geese, wood ducks, northern shovelers, American wigeon and common mergansers) were an excellent variety of winter residents and visitors; these included buffleheads, common goldeneyes, American coot, hooded mergansers, lesser scaup, green-winged teal and ring-necked ducks. On our walk through the South Platte Valley we also encountered belted kingfishers, northern flickers, red-tailed hawks, a lone rough-legged hawk, black-billed magpies, great blue herons, ring-billed gulls, song sparrows, red-winged blackbirds and an industrious muskrat.
But the highlight of this November morning was a flock of tundra swans, winging their way toward Chatfield Reservoir. All eight were in full adult plumage and were unusually silent on their graceful flight above the South Platte. After breeding on the Arctic tundra of Alaska and northern Canada, most tundra swans winter on estuaries along the mid Atlantic and Pacific Coasts; smaller numbers migrate through the interior, heading for the marshlands of New Mexico and Texas.
Kamis, 25 November 2010
A Global Thanksgiving
On this American holiday of Thanksgiving, most of us will give thanks for our human possessions and relationships. But our lives, our health and our society are dependent upon the background support of Earth's natural ecosystems.
Those who do focus on the benefits of nature are likely to mention spectacular sunsets, beautiful scenery, wondrous night skies and the inspiration of our magnificent diversity of wildlife. In referring to the latter, there will be reference to eagles, whales, wild horses and other creatures that humans hold in high esteem. Few will give thanks for fungi or beetles or earthworms, yet, their presence and activity is as vital to our welfare as any other life forms that share this planet.
Indeed, all life on Earth is interdependent. Diverse human cultures, while prone to disagreement and conflict, must learn to cooperate if our species is to survive. And we humans, inclined toward self importance, could not survive without the support of our planet's "lowest" plants and animals. It is thus appropriate that we give thanks for life itself, in whatever form it may exist, and dedicate ourselves to its protection and conservation.
Those who do focus on the benefits of nature are likely to mention spectacular sunsets, beautiful scenery, wondrous night skies and the inspiration of our magnificent diversity of wildlife. In referring to the latter, there will be reference to eagles, whales, wild horses and other creatures that humans hold in high esteem. Few will give thanks for fungi or beetles or earthworms, yet, their presence and activity is as vital to our welfare as any other life forms that share this planet.
Indeed, all life on Earth is interdependent. Diverse human cultures, while prone to disagreement and conflict, must learn to cooperate if our species is to survive. And we humans, inclined toward self importance, could not survive without the support of our planet's "lowest" plants and animals. It is thus appropriate that we give thanks for life itself, in whatever form it may exist, and dedicate ourselves to its protection and conservation.
Rabu, 24 November 2010
The Colorado Piedmont
When the Rocky Mountains first crumpled skyward, 70 million years ago, the adjacent plains rose with them, producing a gradual rise from the High Plains to the eastern flank of the central uplift. Streams meandered eastward from the modest summits which were gradually eroded to the level of the sloping plain. A second uplift of what is now the Colorado Plateau and Rocky Mountain corridor began about 25 million years ago, significantly augmenting the elevation of the mountains and increasing the erosive power of the streams that flowed from the high country.
These streams and subsequent Pleistocene glaciers sculpted the mountains and foothills, removing overlying sediments and cutting numerous canyons through the ancient, Precambrian core. Rumbling onto the plains, the streams merged to form two primary channels, the South Platte and the Arkansas Rivers, their watersheds split by the Palmer Divide; this high, broad ridge, which rises between Denver and Colorado Springs, still connects the High Plains with the east edge of the Front Range. The Rivers and their numerous tributaries have molded a scenic terrain of valleys, low ridges, mesas and hidden canyons along the base of the Rockies, extending eastward along the channels of the primary streams; lower than the adjacent mountains and High Plains, this landscape is known as the Colorado Piedmont.
The great majority of Coloradans live on the Piedmont and its valleys of Cretaceous Pierre Shale support a large portion of the State's agricultural production. The numerous lakes and reservoirs of the Piedmont attract bald eagles and migrant waterfowl while the wooded streams and canyons host the greatest concentrations of eastern Colorado wildlife. Basking in the rain shadow of the Rockies, the human and wild residents of Colorado's Piedmont enjoy a spectacular climate while dodging most of the severe thunderstorms and blizzards that plague the High Plains.
These streams and subsequent Pleistocene glaciers sculpted the mountains and foothills, removing overlying sediments and cutting numerous canyons through the ancient, Precambrian core. Rumbling onto the plains, the streams merged to form two primary channels, the South Platte and the Arkansas Rivers, their watersheds split by the Palmer Divide; this high, broad ridge, which rises between Denver and Colorado Springs, still connects the High Plains with the east edge of the Front Range. The Rivers and their numerous tributaries have molded a scenic terrain of valleys, low ridges, mesas and hidden canyons along the base of the Rockies, extending eastward along the channels of the primary streams; lower than the adjacent mountains and High Plains, this landscape is known as the Colorado Piedmont.
The great majority of Coloradans live on the Piedmont and its valleys of Cretaceous Pierre Shale support a large portion of the State's agricultural production. The numerous lakes and reservoirs of the Piedmont attract bald eagles and migrant waterfowl while the wooded streams and canyons host the greatest concentrations of eastern Colorado wildlife. Basking in the rain shadow of the Rockies, the human and wild residents of Colorado's Piedmont enjoy a spectacular climate while dodging most of the severe thunderstorms and blizzards that plague the High Plains.
Selasa, 23 November 2010
Canadian Sunsets
As the sun sets behind the Colorado Front Range, lines and Vs of Canada geese take to the skies. Common across the urban corridor throughout the year, these large waterfowl are especially abundant from November to March, when the permanent residents are joined by their migrant cousins.
After feasting on natural grasslands, golf courses and the manicured lawns of parks and cemeteries throughout the day, the geese return to our lakes and reservoirs to spend the night. There, surrounded by water or ice, they are protected from the coyotes, fox and feral dogs that prowl the Piedmont; unless taken by surprise, Canada geese are large and aggressive enough to protect themselves from these predators.
Having lost favor due to their abundance and their habit of fouling our pristine lawns, Canada geese do not inspire the average citizen (or even the average birder); but one must admire their tenacity, their cooperative instincts and their powerful flight. Backed by the Rockies and the spectacular Front Range sunsets, their wildness and beauty are easy to appreciate.
After feasting on natural grasslands, golf courses and the manicured lawns of parks and cemeteries throughout the day, the geese return to our lakes and reservoirs to spend the night. There, surrounded by water or ice, they are protected from the coyotes, fox and feral dogs that prowl the Piedmont; unless taken by surprise, Canada geese are large and aggressive enough to protect themselves from these predators.
Having lost favor due to their abundance and their habit of fouling our pristine lawns, Canada geese do not inspire the average citizen (or even the average birder); but one must admire their tenacity, their cooperative instincts and their powerful flight. Backed by the Rockies and the spectacular Front Range sunsets, their wildness and beauty are easy to appreciate.
Senin, 22 November 2010
Snows in the Clouds
Heading to Colorado for the Thanksgiving Holiday, we left Columbia shrouded in moist, balmy air, courtesy of a stiff southerly wind; the latter was produced by an advancing cold front, still in Kansas at the time of our departure. Once we reached Kansas City, the location of the front was obvious as low, gray clouds formed a dense wall across the western horizon.
Passing through the front, the temperature dropped from the sixties to the forties and the wind shifted from the south to the northwest. Layered cloud decks replaced the blue sky and sunshine of our Missouri leg and it looked like our trip across the Great Plains would be far from appealing. Then, in Central Kansas, flocks of snow geese appeared amidst the clouds and my concern about the weather was soon forgotten.
Catching a ride on the strong, northwest winds, these vocal migrants were surely on their way to the Gulf marshes of the Texas Coast. They will probably make another stop in the Arkansas or Red River Valley before pushing on to their wintering grounds and we were fortunate to observe a small segment of their journey from the Arctic. The encounter may have been relatively brief, but the memory will invoke wanderlust in my soul for years to come.
Passing through the front, the temperature dropped from the sixties to the forties and the wind shifted from the south to the northwest. Layered cloud decks replaced the blue sky and sunshine of our Missouri leg and it looked like our trip across the Great Plains would be far from appealing. Then, in Central Kansas, flocks of snow geese appeared amidst the clouds and my concern about the weather was soon forgotten.
Catching a ride on the strong, northwest winds, these vocal migrants were surely on their way to the Gulf marshes of the Texas Coast. They will probably make another stop in the Arkansas or Red River Valley before pushing on to their wintering grounds and we were fortunate to observe a small segment of their journey from the Arctic. The encounter may have been relatively brief, but the memory will invoke wanderlust in my soul for years to come.
Minggu, 21 November 2010
Marriage: an Unnatural Union
Marriage is not a natural human relationship. Rather, our society has collectively decided (and most of us would agree) that children are best reared in the setting of a monogamous commitment. Unfortunately, our natural traits tend to undermine and disrupt these good intentions.
The romantic, "can't get enough of each other" phase of marriage is often fleeting and, in some cases, is over before the vows are exchanged. It is followed by the "what have I done?" phase, when we begin to pay more attention to annoying traits of our partner and come to resent our loss of independence. The arrival of children usually rescues the marriage, as parental pride and the shared responsibilities of nurturing our kids rekindle the romance. Once they are teens or young adults, however, other threats emerge, including discipline issues, Oedipal jealousies and nostalgic yearnings for the freedom that our progeny enjoy.
Perhaps the greatest threat to the stability of marriage occurs when the children are finally independent, often coinciding with the boredom of our middle age lives. Men, naturally attracted to fertile females, have a tendency to stray while many women, having sacrificed careers for their children and now facing entrenched societal discrimination, come to resent the advantage that their spouse has enjoyed; if not rescued by communication, compromise and the trust to extend individual freedoms, the relationship often disintegrates. Those couples who make it through this stage have generally learned to respect the human need for personal space and, if luck holds, they finish out their lives together.
The romantic, "can't get enough of each other" phase of marriage is often fleeting and, in some cases, is over before the vows are exchanged. It is followed by the "what have I done?" phase, when we begin to pay more attention to annoying traits of our partner and come to resent our loss of independence. The arrival of children usually rescues the marriage, as parental pride and the shared responsibilities of nurturing our kids rekindle the romance. Once they are teens or young adults, however, other threats emerge, including discipline issues, Oedipal jealousies and nostalgic yearnings for the freedom that our progeny enjoy.
Perhaps the greatest threat to the stability of marriage occurs when the children are finally independent, often coinciding with the boredom of our middle age lives. Men, naturally attracted to fertile females, have a tendency to stray while many women, having sacrificed careers for their children and now facing entrenched societal discrimination, come to resent the advantage that their spouse has enjoyed; if not rescued by communication, compromise and the trust to extend individual freedoms, the relationship often disintegrates. Those couples who make it through this stage have generally learned to respect the human need for personal space and, if luck holds, they finish out their lives together.
Sabtu, 20 November 2010
Winter's Assault
As of this morning, a potent winter storm was spinning over the Great Basin and its associated cold front stretched from San Francisco to Maine. Pulling in moisture from the Pacific Ocean, the storm is expected to drop heavy snow from the Sierra Nevada to the Rocky Mountains.
North of the front, frigid air is pouring into Montana and the Dakotas, the vanguard of winter's sweep through the country. Here in Missouri, the temperature will push into the sixties over the next few days, as southerly winds develop ahead of the front; by Tuesday, winter should arrive.
Summer's feeble jabs are weakening and, like a light-weight contender facing the heavy-weight champion, it is at risk of a knock-out blow. Winter is gaining strength with each shortening day and its grip will tighten as summer retreats to the south. For all practical purposes, the battle has been won.
North of the front, frigid air is pouring into Montana and the Dakotas, the vanguard of winter's sweep through the country. Here in Missouri, the temperature will push into the sixties over the next few days, as southerly winds develop ahead of the front; by Tuesday, winter should arrive.
Summer's feeble jabs are weakening and, like a light-weight contender facing the heavy-weight champion, it is at risk of a knock-out blow. Winter is gaining strength with each shortening day and its grip will tighten as summer retreats to the south. For all practical purposes, the battle has been won.
Kamis, 18 November 2010
Ringing in the Season
On this first cold evening of the season, I was surrounded by the tinkling song of juncos as I walked home in the fading twilight of dusk. Down from the great Northwoods, these small, attractive songbirds are a fixture of the Midwest winter, thrilled to spend the cold, dark months in our relatively balmy climate.
Feasting on weed seeds, they scavenge our brushy fields and woodlots, scattering into shrubs and thickets if danger is sensed; as they do, their white outer tail feathers unveil their identity. Dark-eyed juncos are hardy survivors, christened "snow birds" for their seeming indifference to the challenges of winter weather.
Those who place feeders in the yard can observe these birds at close range; both slate-colored and Oregon races visit the Heartland. Unlike many of our residential songbirds, they shun the feeder perches, preferring to search for seed that has fallen to the ground. We'll enjoy their company until early April, when the weather gets too warm for their taste; it is then they'll escape to their homeland, the vast coniferous forests of Canada.
Feasting on weed seeds, they scavenge our brushy fields and woodlots, scattering into shrubs and thickets if danger is sensed; as they do, their white outer tail feathers unveil their identity. Dark-eyed juncos are hardy survivors, christened "snow birds" for their seeming indifference to the challenges of winter weather.
Those who place feeders in the yard can observe these birds at close range; both slate-colored and Oregon races visit the Heartland. Unlike many of our residential songbirds, they shun the feeder perches, preferring to search for seed that has fallen to the ground. We'll enjoy their company until early April, when the weather gets too warm for their taste; it is then they'll escape to their homeland, the vast coniferous forests of Canada.
Rabu, 17 November 2010
Autumn Rain
Unlike recent cold fronts, our current trough has tapped a fetch of Gulf moisture and cold rain is falling across central Missouri. Though the rain will be short-lived and modest in quantity, it has temporarily doused our image of a crisp and sunny Midwest autumn.
Such bands of rainfall, caused by the same atmospheric clash that brings early spring showers, are more common in autumn than we care to admit. An unruly jet stream characterizes both seasons, mixing chilly air from the north with a warm, moist flow from the south. The result, raw days with cold rain and shifting winds, is perhaps the least favored weather of nature's year.
While spring showers are often welcomed, ushering in the season of growth and renewal, autumn rains are recognized as the vanguard of a deeper chill. The wet leaves and muddy fields that they leave behind offer little promise of brighter and warmer days ahead. Rather, these autumn rains lead toward the dark, cold realm of winter where, in time, they will convert to a seasonal mix of sleet and snow.
Such bands of rainfall, caused by the same atmospheric clash that brings early spring showers, are more common in autumn than we care to admit. An unruly jet stream characterizes both seasons, mixing chilly air from the north with a warm, moist flow from the south. The result, raw days with cold rain and shifting winds, is perhaps the least favored weather of nature's year.
While spring showers are often welcomed, ushering in the season of growth and renewal, autumn rains are recognized as the vanguard of a deeper chill. The wet leaves and muddy fields that they leave behind offer little promise of brighter and warmer days ahead. Rather, these autumn rains lead toward the dark, cold realm of winter where, in time, they will convert to a seasonal mix of sleet and snow.
Senin, 15 November 2010
Exorcism 2010
Born of fear and scientific ignorance, religions have retained significant influence thoughout the course of human history. Early man, facing the many threats of prehistoric life, developed beliefs and rituals which, over time, have morphed into the religions that we know today. Ingrained in childhood, reinforced by clergy, imposed by governments and maintained by social pressures, they continue to govern our lives.
Modern man tends to ridicule the "pagan" rituals of prehistoric "savages" while defending the mysticism that still pervades our culture. This week, Catholic bishops are convening in Baltimore to review and update the Church dogma related to exorcism, the ritualistic treatment of persons who are "possessed by demons." Despite the advances and revelations of modern neuroscience, the bishops cannot relinquish their conviction that mental illness may be induced by evil spirits!
While some are amused by this exorcism conference, many of us see it as another sign that the talons of religious indoctrination still grip human society. We are embarrassed for our species and view Exorcism 2010 as an insult to human intelligence.
Modern man tends to ridicule the "pagan" rituals of prehistoric "savages" while defending the mysticism that still pervades our culture. This week, Catholic bishops are convening in Baltimore to review and update the Church dogma related to exorcism, the ritualistic treatment of persons who are "possessed by demons." Despite the advances and revelations of modern neuroscience, the bishops cannot relinquish their conviction that mental illness may be induced by evil spirits!
While some are amused by this exorcism conference, many of us see it as another sign that the talons of religious indoctrination still grip human society. We are embarrassed for our species and view Exorcism 2010 as an insult to human intelligence.
Minggu, 14 November 2010
Red-tail Highway
Red-tailed hawks are common on the farmlands of the Midwest and are especially conspicuous during the colder months of the year. It is then that they congregate along our country roads and Interstate highways, hunting for small rodents that inhabit the grassy medians and berms.
On my travels to and from Ohio this weekend, the red-tails were abundant, perched on fenceposts, tree limbs or power poles if not soaring high overhead or rising from the grass with a victim in their talons. Their bulky frame is easy to spot in the barren woodlands and their pale, red tail feathers aid identification as they flap and glide above the fields. Though outnumbered by starlings and (perhaps) turkey vultures, these buteos are readily observed by anyone who traverses the open country of America's Heartland.
Indeed, when scouting birds for the annual Audubon counts, one often hears the retort that "it's just another red-tail." But their common occurrence does not detract from the power and grace of these magnificent raptors and should not minimize their role in controlling the rodents and cottontails that might otherwise decimate our vital croplands.
On my travels to and from Ohio this weekend, the red-tails were abundant, perched on fenceposts, tree limbs or power poles if not soaring high overhead or rising from the grass with a victim in their talons. Their bulky frame is easy to spot in the barren woodlands and their pale, red tail feathers aid identification as they flap and glide above the fields. Though outnumbered by starlings and (perhaps) turkey vultures, these buteos are readily observed by anyone who traverses the open country of America's Heartland.
Indeed, when scouting birds for the annual Audubon counts, one often hears the retort that "it's just another red-tail." But their common occurrence does not detract from the power and grace of these magnificent raptors and should not minimize their role in controlling the rodents and cottontails that might otherwise decimate our vital croplands.
Rabu, 10 November 2010
A Polarized Nation
As if our political polarization was not bad enough, the jet stream has now divided our country. This afternoon, a broad dip in the jet has brought winter conditions to the western U.S. while the eastern half, protected by a dome of high pressure, basks in summertime warmth. The dividing line between the trough and ridge runs north to south across the Central Plains; on either side of this cold front the temperature varies by 20 degrees F.
Such potent contrasts set the stage for severe weather and, once the trough moves into areas primed with Gulf moisture, thunderstorms will ignite. Meanwhile, within the trough, an upper level low is spinning from the northwest to the southeast, producing mountain snows and bringing the first significant upslope snow to Front Range cities.
Over the next few days, the protective dome will shift eastward, summer will retreat and a taste of winter will invade the Heartland. Here in Missouri, we'll escape the western snow but chilly rain and blustery weather will deliver a reality check; it is, after all, November.
Such potent contrasts set the stage for severe weather and, once the trough moves into areas primed with Gulf moisture, thunderstorms will ignite. Meanwhile, within the trough, an upper level low is spinning from the northwest to the southeast, producing mountain snows and bringing the first significant upslope snow to Front Range cities.
Over the next few days, the protective dome will shift eastward, summer will retreat and a taste of winter will invade the Heartland. Here in Missouri, we'll escape the western snow but chilly rain and blustery weather will deliver a reality check; it is, after all, November.
Selasa, 09 November 2010
Jurassic Parks
The Colorado Plateau of the Western U.S. harbors one of the most extensive exposures of Jurassic strata on our planet. Stretching from 200 to 135 million years ago, the Jurassic Period covered the heart of the Mesozoic Era, the Age of Dinosaurs.
A number of our National Parks and Monuments are famous for their Jurassic deposits and, by extension, their cargo of dinosaur fossils. Dinosaur National Monument, in northwest Colorado and northeast Utah, is a showcase for the Morrison Formation; deposited in a long, shallow basin, from Canada to New Mexico, this layer cake of mudstones, siltstones, coal and sandstone is famous for its late Jurassic fossils. A bit older, the Entrada Sandstone, deposited in the mid Jurassic, is highlighted at Arches National Park, in eastern Utah, where it has been sculpted into a spectacular array of fins, natural bridges and arch formations.
Perhaps most famous of the Jurassic sedimentary rocks is the Navajo Sandstone, deposited about 190 million years ago when a vast desert covered the region. Relatively soft and heavily jointed, this sandstone forms the upper cliffs of Canyonlands National Park, the scenic domes of Capitol Reef National Park and the towering walls of Glen Canyon, now drowned by Lake Powell. Separated from the Navajo Sandstone by the Kayenta Formation, the Wingate Sandstone yields the middle cliffs of Canyonlands and the majestic, sheer walls of Colorado National Monument; though officially dated from the onset of the Jurassic, some geologists argue that, based on its fossil contents, the Wingate was deposited near the end of the Triassic.
A number of our National Parks and Monuments are famous for their Jurassic deposits and, by extension, their cargo of dinosaur fossils. Dinosaur National Monument, in northwest Colorado and northeast Utah, is a showcase for the Morrison Formation; deposited in a long, shallow basin, from Canada to New Mexico, this layer cake of mudstones, siltstones, coal and sandstone is famous for its late Jurassic fossils. A bit older, the Entrada Sandstone, deposited in the mid Jurassic, is highlighted at Arches National Park, in eastern Utah, where it has been sculpted into a spectacular array of fins, natural bridges and arch formations.
Perhaps most famous of the Jurassic sedimentary rocks is the Navajo Sandstone, deposited about 190 million years ago when a vast desert covered the region. Relatively soft and heavily jointed, this sandstone forms the upper cliffs of Canyonlands National Park, the scenic domes of Capitol Reef National Park and the towering walls of Glen Canyon, now drowned by Lake Powell. Separated from the Navajo Sandstone by the Kayenta Formation, the Wingate Sandstone yields the middle cliffs of Canyonlands and the majestic, sheer walls of Colorado National Monument; though officially dated from the onset of the Jurassic, some geologists argue that, based on its fossil contents, the Wingate was deposited near the end of the Triassic.
Senin, 08 November 2010
Summer takes a Round
After a week of frosty mornings and the sense that winter was taking control, summer got off the mat and reclaimed mid Missouri today. Its victory may be brief but we'll enjoy a few days in the seventies before the next cold front pushes through the Heartland.
Any thought of raw, gray, November weather has vanished, as coeds stroll across campus in shorts and t-shirts. A steady, southerly wind has the flags rippling atop the ROTC building and has coaxed a trio of vultures into the air. If not for the long shadows and the fading colors of autumn, one might think it was early September.
Such gyrations in our Midwest weather are typical of autumn as a restless jet stream undulates across the country. While songbirds, attuned to the light cycle, are not fooled, the waterfowl will slow their migration until heavy snows and frozen ponds drive them south. As much as I look forward to those wavering flocks of snow geese, this mild interlude is a welcome setback. After all, in due course, winter will win the battle.
Any thought of raw, gray, November weather has vanished, as coeds stroll across campus in shorts and t-shirts. A steady, southerly wind has the flags rippling atop the ROTC building and has coaxed a trio of vultures into the air. If not for the long shadows and the fading colors of autumn, one might think it was early September.
Such gyrations in our Midwest weather are typical of autumn as a restless jet stream undulates across the country. While songbirds, attuned to the light cycle, are not fooled, the waterfowl will slow their migration until heavy snows and frozen ponds drive them south. As much as I look forward to those wavering flocks of snow geese, this mild interlude is a welcome setback. After all, in due course, winter will win the battle.
Minggu, 07 November 2010
The Great Oceanic Plates
When Earth's Continents merged into Pangea, some 250 million years ago, the vast intervening ocean stretched across two oceanic plates, the Pacific and the Farallon; spreading out from a mid-oceanic ridge, the Pacific Plate lied beneath the western half of the sea while the Farallon occupied the eastern half, abutting the future Americas.
Pangea began to break up during the Triassic, as the Tethys Sea opened from east to west. Later, in the Jurassic, the Atlantic began to open, shoving the American Plates to the west. As this occurred (and continues to occur), the Farallon Plate was forced to subduct beneath the American Plates and, in doing so, added a cargo of sub-continents to western North America, crumpled up the Rockies and created a broken chain of subduction volcanoes from the Andes to southeast Alaska. Today, only remnants of the Farallon persist, including the Nazca Plate along the west coast of South America, the Cocos Plate west of Central America and the Juan de Fuca Plate (and a few smaller remnant plates) off the west coast of the Pacific Northwest.
The Pacific Plate, devoid of major continental masses continues to form along its ridge with the remnants of the Farallon and along its younger ridge with the Antarctic Plate. Inching to the northwest, the Pacific Plate scrapes through Southern California along the San Andreas Fault and eventually subducts beneath or overruns the North American, Eurasian, Philippine and Australian Plates in a broad arc, from the Aleutians to New Zealand. For now, only hotspot volcanic islands disrupt its vast expanse of open sea; eventually, this great oceanic plate will also disappear as new oceans open, our current continents rift apart and the Pacific subducts into history. Just like the Farallon and its many other predecessors, the Pacific Plate is a transient feature of Planet Earth.
Pangea began to break up during the Triassic, as the Tethys Sea opened from east to west. Later, in the Jurassic, the Atlantic began to open, shoving the American Plates to the west. As this occurred (and continues to occur), the Farallon Plate was forced to subduct beneath the American Plates and, in doing so, added a cargo of sub-continents to western North America, crumpled up the Rockies and created a broken chain of subduction volcanoes from the Andes to southeast Alaska. Today, only remnants of the Farallon persist, including the Nazca Plate along the west coast of South America, the Cocos Plate west of Central America and the Juan de Fuca Plate (and a few smaller remnant plates) off the west coast of the Pacific Northwest.
The Pacific Plate, devoid of major continental masses continues to form along its ridge with the remnants of the Farallon and along its younger ridge with the Antarctic Plate. Inching to the northwest, the Pacific Plate scrapes through Southern California along the San Andreas Fault and eventually subducts beneath or overruns the North American, Eurasian, Philippine and Australian Plates in a broad arc, from the Aleutians to New Zealand. For now, only hotspot volcanic islands disrupt its vast expanse of open sea; eventually, this great oceanic plate will also disappear as new oceans open, our current continents rift apart and the Pacific subducts into history. Just like the Farallon and its many other predecessors, the Pacific Plate is a transient feature of Planet Earth.
Sabtu, 06 November 2010
Morning Chill at Eagle Bluffs
Arriving at Eagle Bluffs Conservation Area this morning, it was clear that winter had taken charge of the refuge. Flocks of horned larks and meadowlarks moved across the frosted fields while smaller groups of crows foraged amidst the brown corn stubble. Kestrels surveyed the scene from roadside powerlines and red-tailed hawks soared overhead, scouting for mice or cottontails on the cold, yellowing grasslands.
As expected, most of the preserve is closed for duck hunting but there were a fair variety of waterfowl on accessible lakes and waterways. Mallards and wood ducks cruised through the flooded timber while shovelers, gadwall and coot gathered in the shallows; pied-billed grebes were especially common, diving amidst the reeds and aquatic vegetation that rimmed the ponds.
This placid scene was disturbed only by the shotgun blasts that rang through the valley. Watching the ducks in the safe zone, one wanted to warn them of danger just to the south; they, of course, were oblivious to the threat and showed no response to the distant explosions. It was, in some ways, a disturbing experience, watching these potential victims that, later in the morning, might venture across the killing fields.
As expected, most of the preserve is closed for duck hunting but there were a fair variety of waterfowl on accessible lakes and waterways. Mallards and wood ducks cruised through the flooded timber while shovelers, gadwall and coot gathered in the shallows; pied-billed grebes were especially common, diving amidst the reeds and aquatic vegetation that rimmed the ponds.
This placid scene was disturbed only by the shotgun blasts that rang through the valley. Watching the ducks in the safe zone, one wanted to warn them of danger just to the south; they, of course, were oblivious to the threat and showed no response to the distant explosions. It was, in some ways, a disturbing experience, watching these potential victims that, later in the morning, might venture across the killing fields.
Jumat, 05 November 2010
Claron Lake
When the Rocky Mountain chain began to rise, some 70 million years ago, the crust to its west was stretched, producing a mosaic of ridges and broad basins. Drainage into the basins created large inland lakes, including the Green River Lakes of the Utah-Colorado-Wyoming Tristate and Claron Lake of southwest Utah. All of these lakes gradually filled with sediments of the Paleocene and Eocene Periods (60-50 million years ago); the deposits in the Green River Lakes would eventually yield the famous oil-shales of the Roan Plateau while deposits in Claron Lake would become prized more for their natural beauty.
Compacting into layers of limestone, dolomite, siltstone and conglomerates and capped by volcanic tuff from the Oligocene Period (30 million years ago), the Claron Formation was lifted with the rest of the Colorado Plateau during the Miocene-Pliocene Uplift, some 25-10 million years ago. Erosion and faulting would eventually expose the Claron beds along the edge of regional plateaus; Cedar Breaks National Monument, a spectacular natural amphitheater on the west edge of the Markagunt Plateau and Bryce Canyon National Park, on the east edge of the Paunsaugunt Plateau, protect the most scenic exposures.
Rich in iron oxides and manganese oxides, the colorful limestones and dolomites have eroded into striking rock formations, known as hoodoos. These pinnacles, capped by more resistant rock layers have been split apart by stream erosion and freeze-thaw fracturing. Once lying beneath an ancient lake, they now gleam in the bright Utah sun and adorn calendars across the globe.
Compacting into layers of limestone, dolomite, siltstone and conglomerates and capped by volcanic tuff from the Oligocene Period (30 million years ago), the Claron Formation was lifted with the rest of the Colorado Plateau during the Miocene-Pliocene Uplift, some 25-10 million years ago. Erosion and faulting would eventually expose the Claron beds along the edge of regional plateaus; Cedar Breaks National Monument, a spectacular natural amphitheater on the west edge of the Markagunt Plateau and Bryce Canyon National Park, on the east edge of the Paunsaugunt Plateau, protect the most scenic exposures.
Rich in iron oxides and manganese oxides, the colorful limestones and dolomites have eroded into striking rock formations, known as hoodoos. These pinnacles, capped by more resistant rock layers have been split apart by stream erosion and freeze-thaw fracturing. Once lying beneath an ancient lake, they now gleam in the bright Utah sun and adorn calendars across the globe.
Kamis, 04 November 2010
Tardy Canadians
Perhaps our balmy October weather kept them at bay. Or perhaps they arrived under the radar and I've been too busy to notice their presence. For whatever reason, I saw the first white-throated sparrows under our feeder this afternoon, a sign that they have escaped the harsh winter of Canada to spend the dark season in the mild confines of central Missouri.
Two weeks behind schedule, their appearance is always a welcome sight and their plaintive song will brighten the long, dreary months of winter. That tune will build in urgency during the waxing days of early spring and, by mid April, they'll depart for their homeland, never to endure the sticky weather of a Midwest summer.
Watching them beneath the feeder, one wonders if they would stay put if they knew about the mild conditions along the Gulf Coast. If informed, would they pull up stakes and head for the sandy pinelands of that southern clime? I tend to doubt it; after all, these hardy birds have adapted to the cool climate of the Great Northwoods and our Missouri winters, however taxing, pose little threat to their survival. On the other hand, a few months in the heat and humidity of the Gulf Coast, while inviting to many humans, might sap their energy and hasten their demise. I, for one, would never encourage them to leave; their stoic presence, especially on those frigid winter mornings, is an inspiration to all of us who cannot escape.
Two weeks behind schedule, their appearance is always a welcome sight and their plaintive song will brighten the long, dreary months of winter. That tune will build in urgency during the waxing days of early spring and, by mid April, they'll depart for their homeland, never to endure the sticky weather of a Midwest summer.
Watching them beneath the feeder, one wonders if they would stay put if they knew about the mild conditions along the Gulf Coast. If informed, would they pull up stakes and head for the sandy pinelands of that southern clime? I tend to doubt it; after all, these hardy birds have adapted to the cool climate of the Great Northwoods and our Missouri winters, however taxing, pose little threat to their survival. On the other hand, a few months in the heat and humidity of the Gulf Coast, while inviting to many humans, might sap their energy and hasten their demise. I, for one, would never encourage them to leave; their stoic presence, especially on those frigid winter mornings, is an inspiration to all of us who cannot escape.
Rabu, 03 November 2010
The Nature of Politics
The elections are over. The Republicans control the House, the Democrats will likely retain the Senate and, in the end, nothing will change. At least the obnoxious commercials and recorded phone messages will stop for a while.
American politics is all about power, celebrity and perks. During campaigns, the candidates parade their families before the camera, visit local merchants, extol the values of middle America and promise to restore our faith in Government. Once elected, it's politics as usual: pompous rhetoric, cable TV appearances, travel junkets, celebrity galas, golf tournaments, extra-marital affairs and deal-making legislation to ensure that constituents get what they want. After all, their primary goal is to be re-elected. Meanwhile, wars drag on, the economy stagnates, the wealth gap widens, individual rights are threatened and a commitment to environmental protection is but an empty promise.
The concept of term limits surfaces now and then and, in my opinion, deserves serious consideration. Professional politicians argue that they understand the logistics of government and that a regular turnover of Congress would diminish their effectiveness. The evidence, however, suggests otherwise.
American politics is all about power, celebrity and perks. During campaigns, the candidates parade their families before the camera, visit local merchants, extol the values of middle America and promise to restore our faith in Government. Once elected, it's politics as usual: pompous rhetoric, cable TV appearances, travel junkets, celebrity galas, golf tournaments, extra-marital affairs and deal-making legislation to ensure that constituents get what they want. After all, their primary goal is to be re-elected. Meanwhile, wars drag on, the economy stagnates, the wealth gap widens, individual rights are threatened and a commitment to environmental protection is but an empty promise.
The concept of term limits surfaces now and then and, in my opinion, deserves serious consideration. Professional politicians argue that they understand the logistics of government and that a regular turnover of Congress would diminish their effectiveness. The evidence, however, suggests otherwise.
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