Big Bend National Park, TexasUnited States. National Park Service. Division of Publications
History
Big Bend National Park, Texas
United States. National Park Service. Division of Publications
Big Bend National Park (Tex.)
The Chisos Basin has been hollowed out of volcanic rock by stream
erosion. The peaks that ring the Basin all came into being when molten
rock squeezed up under enormous pressure from deep within the Earth.
Some of the red hot stuff poured out over the land surface in lava flows
which cooled so quickly that they cracked in long vertical fissures.
Then as the ages passed, joints toppled and square-faced peaks,
buttresses, and free-standing spires emerged. So the Basin wall took
shape from Casa Grande southward through Emory Peak. Later on, more
molten rock pushed up from below, bulging the surface rocks upward
without breaking through. Again the eons passed and the softer surface
rocks wore away, exposing the dome-shaped peaks which now rim the Basin
to the north and west. Today, loose rocks and clays still inch downhill
toward the Window. All Basin runoff heads for this chute, and when it
storms in the heights, the dry waterfall turns into a torrent, with
boulders bouncing along like so many corks. Growling and grumbling, the
big rocks plunge over the pouroff in a 67-meter (220-foot) free fall,
coming to Earth in a great rubble pile below.
Pinyon pines grow abundantly across both Mexico and the American
Southwest. In the Chisos you’ll find them almost anywhere above 1,500
meters (4,800 feet) of elevation, and at lower elevations they will be
the only pines. Short of trunk, with spreading lower branches, egg-sized
cones, and short, slender, bluish-green needles, pinyons range from
dwarf size to a tree 15 meters (50 feet) tall. Many birds and mammals
eat its delicious nuts.
As elevation increases you may find fewer junipers, while more pinyons
appear on the open slopes and more oaks along drainages. The deciduous
Graves oak requires more moisture than other oaks, so you find it
putting forth its shiny, dark green leaves in high moist canyons. The
Emory oak also prefers high drainages but it grows at slightly lower
elevations. It has small lance-shaped leaves. The Chisos oak, a small,
graceful tree with narrow, leathery leaves, requires a high water table.
In all the world it grows only in the Chisos Mountains’ Blue Creek
Canyon.
[Illustration: Mule deer frequent the park’s lower, drier
elevations.]
[Illustration: The Sierra del Carmen whitetail haunts the Chisos
Mountains. It has much smaller ears than the mule deer and bears the
characteristic flag tail. Isolation allowed this sub-species of
whitetail to develop. These deer live only in the Chisos and across
the river in the Sierra del Carmen.]
Public-domain text, read in full here on John Shaqi.
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