Mosaic of New Mexico's Scenery, Rocks, and History
History
Mosaic of New Mexico's Scenery, Rocks, and History
Geology -- New Mexico; New Mexico -- Description and travel; New Mexico -- History
But as Interstate 40 approaches Grants, the dominant feature is black
frozen lava. The mesas surrounding Mount Taylor are capped by black
basalt, built up in many layers, each individual flows, and loose blocks
tumble down on the hillsides. Young basalt, twisted and wrinkled as if
it were still hot, winds along the valley; just east of Grants, a huge
“field” of this recent basalt stretches southward beyond the horizon.
And above all looms Mount Taylor, remnant of an ancient volcano,
snow-capped in winter, towering 11,389 feet above sea level.
At Casa Blanca, southeast of Mount Taylor, State Road 23 leads south to
Acoma Pueblo. Eleven miles to the southwest, Enchanted Mesa, _Katsim_ as
it is called by the Acomas, towers 450 feet above the surrounding valley
floor. This sheer-cliffed rock is built by layers of (from the base to
the top) pink and white Entrada Sandstone, gray Todilto limestone, pink
and green Summerville beds, a massive cliff of light-tan Zuni Sandstone,
and a cap of yellow-brown Dakota Sandstone.
The top of Enchanted Mesa is inaccessible by normal means. Legend has it
that once the Acomas lived there, and there are Indian ruins up on the
isolated rim. A terrific rain and lightning storm, one summer day, sent
huge waterfalls down the sides of the mesa, tearing away large blocks of
sandstone, and destroyed the trail to the top, a series of narrow zigzag
ledges and toeholds in crevasses. Thus the Acoma Indians moved a few
miles to the southwest to Acoma, onto the top of another sheer cliff, a
rock fortress carved in Zuni Sandstone and capped by Dakota Sandstone.
[Illustration: Talk about wide open spaces ... around the Enchanted
Mesa]
Southwest of Grants, the forested Zuni Mountains rise, bordered on the
north by a valley cut in Triassic redbeds and on the east by the recent
black basalt flows. The hurrying traveler will follow Interstate 40 to
Gallup around the north edge of the Zuni dome, flanked on the north by
the spectacular pink, red, brown, and gray cliffs of Jurassic and
Cretaceous sandstones. If one has time, take the low road, State
Highways 53 and 36, around the southern edge of the Zunis. For almost
twenty miles, passing through San Rafael, the paved highway parallels
the west edge of the Grants black basalt flow; then up over low ridges
and past black cinder cones toward El Morro. In the lava tunnels,
perpetual ice stays hidden from the sun; these can be visited at Ice
Caves.
El Morro, Inscription Rock, with its towering cliffs of Zuni Sandstone,
overlooks peaceful green valleys; farther west, the red and brown
sandstones are carved into many mesas and buttes near Zuni Pueblo. Then
northward to Gallup, swinging around the west edge of the Zuni
Mountains, the roller-coaster highway, State 36, cuts through ponderosa
pine country, bordered by Cretaceous brown sandstones, black shales, and
coal beds.
Public-domain text, read in full here on John Shaqi.
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