Bandelier National Monument, New MexicoWing, Kittridge A.
History
Bandelier National Monument, New Mexico
Wing, Kittridge A.
Bandelier National Monument (N.M.)
The first rains and snows which fell upon this ancestral uplift found
relatively smooth slopes descending outward from the rim of the central
caldera. These rains and melted snows began to drain downhill, finding
whatever slight channels or irregularities there were in the surface. As
the centuries passed, the little water-channels became gullies, then
ravines, trending east and southeast through the Bandelier quadrant,
down the natural fall-line of the Pajarito slopes. In less than a
million years, the plateau has eroded into its present form and the
drainage pattern of canyons radiating from the Jemez ridge and emptying
into the Rio Grande has become well defined. Such canyons as Frijoles,
then, are the products primarily of water erosion, etched into a
one-time smooth slope of volcanic deposits.
During the early years of this erosion process, the caldera itself
became a lake, entrapping the runoff of waters within its circle. This
body of water eventually found an outlet to the south, through the
guarding rim of the basin, and in its outflow began the present system
of canyons of the Jemez River. A modern example of a caldera containing
a lake is to be seen in Crater Lake National Park in Oregon, but the
Valle Grande Lake had nearly six times as great an area.
[Illustration: _Headquarters area in Frijoles Canyon, showing, from
bottom upwards, Tyuonyi Ruin, the Big Kiva, the Museum, and the
Lodge._]
Many of the almost sheer canyon walls of the monument provide good cross
sections of the lava and ash deposits exposed in cliffs several hundred
feet high. In simplest form, these cross sections reveal at their base a
flow of lava or basalt, overlain by perhaps 200 vertical feet of tuff,
and capped by another flow of lava forming the rimrock of the mesa-top.
In most places, the alternating layers of lava and tuff were deposited
several successive times, variously distributed, and complicated by
later faulting and interim periods of erosion, so that the
interpretation of the rock layers is not everywhere as simple as in the
example given above.
[Illustration: _The Lower Falls of the Rito de los Frijoles._]
Public-domain text, read in full here on John Shaqi.
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