The Sandia Mountains area covers 400 mi 2 within six 7.5-min quadrangle east and northeast of Albuquerque. It is believed that the name Sandia (Spanish: “Watermelon”) was given to the mountains for the pinkish colour of their … The Sandia Mountains are a great block of granite and limestone which was uplifted during the formation of the Rio Grande Rift. Over 11 million passengers have taken the Sandia … 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. The view to the north/northwest shows the basic geological structure of the SMNHC. The Sandia Mountains are an east-tilted fault block along the margin of the Rio Grande Rift. 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 two ranges are connected by Manzanito Mountains, a smaller subrange of the Manzanos, and divided by interstate 40. The Sandia Range is the dominant feature, but part of the Manzanita Mountains south of US-66, Tijeras Basin, Monte Largo (east of the Sandias), Hagan Basin (northeast of the Sandias), and an edge of the Rio Grande depression are all included in the geologic map and text. Geologic Setting The Sandia pluton is exposed along the western escarpment of the Sandia Mountains and in a few inliers on the eastern side of the range (Condie and Budding, 1979). Discusses caves and artifacts, historical geologic surveys and early mining operations; also includes such environmental problems as landslides and earthquakes. The Spanish word \"Sandia\" means Watermelon and refers to the pinkish color the mountai… Contains a topographic map, structure map, structure sections, and color geologic map. Thick sequences of early and late Tertiary sediments lie in order above the Cretaceous in the Hagan Basin northeast of the uplift. Sedimentary rocks range in age from Mississippian to Cretaceous within and immediately flanking the mountains. 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 belt, 2–3 mi wide, 16 mi long, trending northeastwards, consists mainly of two longitudinal parts: a southwestern folded graben and a northeastern horst. Contacts between the They form the eastern boundary of the Albuquerque Basin. For some of our pages, the random assortment of images is related thematically to the section or page being visited. 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. This is topped by a relatively thin layer (approximately 300 feet/100 meters) of sedimentary rock (mostly The Sandia Mountains run in a North-South line for 17 miles on the eastern edge of Albuquerque, NM. Stratigraphic units consist of 1) marine Mississippian and Pennsylvanian shelf beds, 2) continental Permian, Triassic, and Jurassic red beds formed under flood-plain, evaporitic, lacustrine, and eolian environments, and 3) intertonguing marine and flood-plain Cretaceous beds of the Rocky Mountain geosyncline.The Sandia Mountains area is dominated by an eastward-tilted fault block that stands imposingly above the deep Rio Grande trough on the west.
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