The Sandia Mountains are an east-tilted fault block along the margin of the Rio Grande Rift. It is believed that the name Sandia (Spanish: “Watermelon”) was given to the mountains for the pinkish colour of their … The Sandia Mountains are an east-tilted fault block along the margin of the Rio Grande Rift.The images in the banner of our website highlight interesting geological features in New Mexico.
Discusses caves and artifacts, historical geologic surveys and early mining operations; also includes such environmental problems as landslides and earthquakes. The exposed portion of the pluton is approximately 3-5 km wide and 30 km long. The section is 16,000 ft thick exclusive of the late Tertiary and Quaternary trough-filling Santa Fe Formation.The long east- to northeast-tilted homocline from the Sandia uplift into the Hagan Basin contains most of the formations of central New Mexico, and is the most complete sequence in the state. This mountain range continues to the south and is known as the Manzano Mountains in that region. The Sandia Mountains area covers 400 mi 2 within six 7.5-min quadrangle east and northeast of Albuquerque. Thick sequences of early and late Tertiary sediments lie in order above the Cretaceous in the Hagan Basin northeast of the uplift. The Sandia Mountains run in a North-South line for 17 miles on the eastern edge of Albuquerque, NM. Contacts between the Over 11 million passengers have taken the Sandia … The first riders up Sandia Peak ascended on May 7, 1966. Variations in thickness indicate deposition on an eroded Precambrian surface. The Sandia Mountains are a fault block range, on the eastern edge of the Rio Grande Rift Valley. The Sandias were uplifted in the last ten million years as part of the formation of the Rio Grande Rift.
Tijeras rift belt is principally a Laramide feature as are a few other faults along the eastern flank of the late Tertiary Sandia uplift.We are a research and service division of:The area contains most of the significant Paleozoic to Cenozoic stratigraphic units and a varied representation of the Precambrian rocks of central New Mexico; important stratitectonic relationships are observable there that bear on the understanding of the origin of the Rio Grande depression and of the Sandia Mountains.
The view to the north/northwest shows the basic geological structure of the SMNHC. The area is particularly important to Albuquerque, the major city of New Mexico, with respect to environment, recreation, urban development, and esthetics.This 1000-piece beauty may be just the thing for a relaxing evening in isolation...Comprehensive coverage of rocks and formations, structure, paleontology, stratigraphy, geologic history, and mineral resources.
For some of our pages, the random assortment of images is related thematically to the section or page being visited.
If you click on any of our banner images, you will see a larger version of that image with descriptive information like the one above.Off highway 550 north of Bernalillo.We are a research and service division of: The most unusual structure of the area is the Tijeras rift belt bounding the uplift on the southeast. The core of the range consists of Sandia granite, with a U-Pb age of 1453±12 million years. Sandia Mountains, mountain range in central New Mexico, U.S., northeast of Albuquerque and east of the Rio Grande.
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