Over 11 million passengers have taken the Sandia … 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. Variations in thickness indicate deposition on an eroded Precambrian surface. 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. The Sandia Mountains are an east-tilted fault block along the margin of the Rio Grande Rift. This is topped by a relatively thin layer (approximately 300 feet/100 meters) of sedimentary rock (mostly
Structural relief from uplift to trough is as much as 6 mi; into the basins to the east and northeast relief is 2.5–5 mi. The Sandias were uplifted in the last ten million years as part of the formation of the Rio Grande Rift. Contains a topographic map, structure map, structure sections, and color geologic map. 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. Contacts between the Precambrian rocks, prominent in the bold western fault scarp, consist of granite, gneiss, schist, quartzite, and greenstone. The two ranges are connected by Manzanito Mountains, a smaller subrange of the Manzanos, and divided by interstate 40. They form the eastern boundary of the Albuquerque Basin. Sandia Mountains, mountain range in central New Mexico, U.S., northeast of Albuquerque and east of the Rio Grande. The most unusual structure of the area is the Tijeras rift belt bounding the uplift on the southeast. 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. The Spanish word \"Sandia\" means Watermelon and refers to the pinkish color the mountai… The exposed portion of the pluton is approximately 3-5 km wide and 30 km long. 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). The Sandia Mountains are a great block of granite and limestone which was uplifted during 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.
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