sangre de cristo fault map

Subparallel fault scarps in middle Quaternary fan alluvium between Vallejos and San Francisco Creeks indicate the presence of a series of minor grabens and horsts in the hanging wall of the fault and attest to the structural complexities that may be associated with the fault. It was the first official American effort to explore the western Great Plains and the Rocky Mountains in present-day Colorado.After the U.S. took control of the region following the Mexican-American War, the government endeavored to resolve claim disputes. The north-south-striking Rito Seco strand of the Sangre de Cristo Fault enters the quadrangle at the north edge of the map.

In 1851, Colorado’s oldest town, San Luis, was founded, and in 1858, the U.S. Army erected a garrison at Fort Garland in the San Luis Valley to protect settlers from the fierce Comanche tribe. From Salida, Colorado, the Sangre de Cristo’s stretch 225 miles to Santa Fe, New Mexico, but if you follow their crest through all its jogs from Poncha Pass to its terminus at Glorieta Pass, the range’s length exceeds 300 miles.

(1:24,000). Silver Cliff was settled in the late 1870s. Mex., terminates just south of the town in a prominent point known as Hunts Peak (12,446 feet).

(1:24,000). Just a few miles of very soft sand and you come to the paved road and the Sand Dunes Visitor Center.The Rainbow trail on the Northeast side of the Sangre de Cristo’s to Hayden Pass.

Roughly contemporaneous with the Lewis and Clark Expedition, it was led by United States Army Lieutenant Zebulon Pike, Jr. Includes oblique view, booklet, correlation of map units, cross sections, shapefiles with metadata. For reasons that are not clear, the Colorado Plateau experienced a clockwise torsion, helping to pull the rift’s edges apart and allowing the land within to drop thousands of feet.The land within the rift didn’t fall thousands of feet at once, but rather 5-10 feet at a time over millions of years.

The Rainbow trail traverses the East side of the Sangre de Cristo’s from Poncha Pass to Hayden Pass.

The Sangre de Cristo Mountains’ snowpack consolidates earlier than the other ranges in Colorado due to low snow accumulation and warmer temperatures.From Poncha Pass there are only two routes open to motor vehicles. Additionally, fault scarps at the northern end of the range tell us that range continues to rise at an average of an inch every one-hundred years. The town was incorporated in 1879 and by 1880 was Colorado’s third largest city with over 5,000 residents (behind Denver and Leadville). Geologists have determined that rocks found in the Sangre de Cristo Mountains are displaced by nearly The Sangre de Cristo’s beginnings actually predate the Rio Grande Rift, however, so we need to take a quick step back. Hayden pass is very steep on the west side.Medano Pass from the East is steep and twisty. The Pike Expedition (July 15, 1806 – July 1, 1807) was a military party sent out by President Thomas Jefferson to explore the south and west of the recent Louisiana Purchase.

This wilderness area has subsequently lost acreage to the Great Sand Dunes Wilderness, which was created as part of the new Great Sand Dunes National Park and Preserve in 2004Most of New Mexico’s ski areas are located within the Sangre de Cristo Mountains. Kirkham, Robert M., John L. Lufkin, Neil R. Lindsay, and Keith E. Dickens.

The Utes are the oldest continuous residents of Colorado.

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