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Sedimentary Rocks Around Las Vegas
Rocks and Geology Around Las Vegas Sedimentary Rocks Around Las Vegas

Sedimentary Rocks, the most common rocks around Las Vegas, are formed by two different processes. First, sedimentary rocks are formed by cementing together particles that eroded from pre-existing rocks. Particles are washed or blown away to accumulate somewhere else, and if left in place long enough, can become cemented to form rocks such as conglomerate, sandstone, and mudstone, depending on the size of the particles and the degree of sorting of the eroded materials.

Second, sedimentary rocks form on the bottom of the ocean when particles "rain" down from the surface. These particles can become compressed and cemented to form limestone. Fossilized sea creatures are often found in these rocks.

Most of the mountains around Las Vegas are composed of sedimentary rocks. Red Rock Canyon (photo) provides a spectacular example of both types: the gray mountains are limestone, and the red-and-white hills are sandstone.

Carbonate Rock
Carbonate rock layers in the Las Vegas Range

Carbonate Rocks (Limestone and Dolomite). Around Las Vegas, carbonate rocks were formed in horizontal layers on the bottom of ancient seas some 600-250 million years ago [mya]. As particulate matter in the water column rained down, it built up layers and eventually solidified. The particulate matter was mostly plankton, precipitates, and suspended sediments that washed down rivers into the ocean, but also dead fish, seaweeds, shells, and similar detritus. The different layers in the carbonate rocks represent different environmental conditions as climate and water depth changed over time. Most of the mountains in southern Nevada are composed of carbonate rocks.

Around Las Vegas, fossils are generally uncommon in these rocks, but they can be found in some areas. Most of the fossiliferous material was formed from organic muck, and as such, appears as layers of amorphous dark material in the lighter limestone. In some places, large numbers of algae and sponge fossils can be found, but these too can appear a bit amorphous. Fossil corals, crinoids, brachiopods (clam-like creatures), and trilobites can be abundant in some areas.

Sand dunes trapped by time at Red Rock Canyon NCA

Sandstone. Around Las Vegas, the sandstone cliffs are formed from grains of sand that once were vast sand dunes covering much of the southwestern United States about 180-60 mya. Over time, the wind-blown sand grains were cemented together and became rock. Layers in the sandstone (cross bedding) often reveal the original sand dune structure, and the original sand grains can be scraped out of the rock.

The red-and-white cliffs at Red Rock Canyon are sandstone, as are the red cliffs at Valley of Fire State Park and parts of Lake Mead . The red color in the cliffs is from rust (iron oxide), but the exact process by which the rust formed, and where it formed (red rock) and did not form (white rock) still confuses geologists.


Mudstone. Around Las Vegas, mudstones were formed from muds that settled in the bottom of ancient lake or were formed in the delta of rivers flowing into the ocean. Depending on the size of the particles, mudstones can be coarse or fine grained, and depending on the cementing, mudstones can be soft or very hard.

In many places around Las Vegas, the source of the "dirt" particles that formed the mud was volcanic ash. Mudstones near Lake Mead NRA often originated as volcanic ash, but mudstones around Red Rock Canyon (below the sandstone) originated as river deposits.

conglomerate Conglomerate. Conglomerate rock is formed of well or poorly sorted river deposits, and the originally deposited materials are unaltered and remain clearly visible.
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