Colorado_Plateau_Bioregion_www by changcheng2


									Colorado Plateau Bioregion
"A Bioregion can be described as an area without hard boundaries but which can be
distinguished by its may natural features including the flora, fauna, soil, climate,
geology, and drainage area. A critical component of a bioregion is the human culture
which has developed within and is integral to that area. This essential human
element is what distinguishes the concept of bioregion from similar ecological
entities which traditionally treat humans and their cultures as interlopers rather
than as integral components of a natural community. All together, these bioregions
form a vast patchwork extending over the planet. Political boundaries have little
meaning from either a bioregional perspective or in classical ecological thinking. In
short, bioregionalism is having, or developing, 'a sense of place'."

The Colorado Plateau, the physiographic study area for this Program, is in reality a massive basin
surrounded by highlands and filled with a myriad of plateaus. Covering an area of 130,000 square miles, it
spreads over portions of southeastern Utah, northern Arizona, northwestern New Mexico and western
Colorado. Of America's 50 states, only Alaska, Texas, California, and Montana are larger . The underlying
geology is ancient, at least 500 million years old. Drifting along as a portion of continental crust some 400
million years ago, the Colorado Plateau was covered by rising ocean waters. As the waters receded, deep
layers of sediment in different thickness were revealed. Further sedimentary material worked its way down
from surrounding high country, and the wind deposited dust and volcanic ash from active volcanoes from
the west and southwest.

Under the weight of the accumulated material, the crust sank. Time, pressure and heat eventually solidified
the deposits forming sedimentary and metamorphosed rock 2-3 miles thick. When the surrounding geologic
material began to move, and uplifting formed the various mountain ranges on the continent, the sediment of
the Colorado Plateau remained stable and in place. Because of the dense, thick nature of the consolidated
sedimentary rock on the Plateau, volcanic activity in the region was unable to penetrate the surface. Instead,
isolated ranges, such as the Henry, La Sal, Sleeping Ute, and Abajo mountains were the result of hot
magma pushing up and penetrating these thick layers. When the volcanic activity tapered off and the
magmas cooled and hardened, these mountains, termed "laccoliths," remained as a testament to the solid,
ancient nature of the Colorado Plateau. Tectonic forces, while sculpting the Sierra Nevada and the Rocky
Mountains, could only impress this area with shallow basins, low dome uplifts and long, continuous folds
called "reefs." As the continent under and around us continues to move, the Colorado Plateau remains
essentially motionless, slowly eroding and changing its face with the passage of time.

The Plateau presents some interesting contradictions and puzzles. Although largely a desert environment of
130,000 square miles situated a mile above sea level, it also contains the Colorado River, one of the
continent's largest rivers. Hard and soft rock battle for position in every canyon and on every mesa top.
Side canyons of the larger rivers serpentine their way down and through the landscape as water and wind
perpetually carve away at them. The sandstones of varied form, including Chinle, Navajo, Wingate,
Entrada, Mesa Verde and countless others, are unique shapes and faces of rock. Alcoves, potholes,
striations, bowls, basins, and deep canyons are all cut from these faces by the erosive actions of wind and
Within the sandstone layers are deposits of gypsum, potash and salt. Large seam deposits of coal, and fluid
layers of oil and natural gas can be found in localized clusters throughout the region. Pockets of uranium
and radium rich ores are folded into the layers. Red Halgaito shale, gray Mancos shale, gray limestone, and
red and white Cedar Mesa sandstone confound the onlooker further. Throughout the area, you will likely be
overwhelmed by the "hugeness" of it all.

To top