Tag Archive for: TOP SN

Slope-shade model that combines hillshade and slope models. Airborne data for mapping the Wasatch fault zone at the mouth of Little Cottonwood Canyon, Utah.

We recently mapped part of the upper Bear River watershed using the National Wetland Inventory (NWI) Program’s mapping standards and the Cowardin classification system.

A small pink flower and green succulent emerge from sand scattered with round brown rocks.

Moqui marbles are small, brownish-black balls composed of iron oxide and sandstone that formed underground when iron minerals precipitated from flowing groundwater.

Survey Notes 46-3

The Uinta Mountains are one of Utah’s premier mountain ranges. Rising above the Uinta Basin in Utah on the south and the Green River Basin in Wyoming on the north, they stretch from near Kamas eastward into northwestern Colorado. However, the Uintas are a tale of two geographies, so much so that many people refer to the “western (or high) Uintas” and the “eastern Uintas.”

Gray and black cliffs in horizontal stripes.

Geologists generally know the age of a rock by determining the age of the group of rocks, or formation, that it is found in. The age of formations is marked on a geologic calendar known as the geologic time scale. Development of the geologic time scale and dating of formations and rocks relies upon two fundamentally different ways of telling time: relative and absolute.

Eastward view of research trench across a small (about 3 feet high) fault scarp on the West Valley fault zone in Salt Lake Valley. Photo by Michael Hylland.

The Wasatch fault zone has long been known to be a serious earthquake threat to the Wasatch Front region. However, another possible source of large (approximately magnitude [M] 6.5) earthquakes lies just a few miles west of Salt Lake City—the West Valley fault zone, comprising a system of faults on the floor of northern Salt Lake Valley.

Young man holding a dinosaur bone in front of a body of water

Whether you can keep a fossil or not depends on 1) the type of fossil, and 2) who owns or manages the land where the fossil was found.

The dull, light khaki gray color of Fantasy Canyon sandstone transforms to a glowing pale orange at sunset. This sculpture is named “Prowling Coyote.”

Fantasy Canyon is crowded with intricate and peculiar stone figures that are a unique expression of rock weathering and erosion. Covering only a few acres, this miniature canyon can be viewed up-close on a short 0.6-mile loop trail.

Fragment of the Gunlock Meteorite. The polished slice through meteorite reveals it’s distinctive chondritic texture and fractures possibly due to impact with the surface of the Earth.

You found a strange rock. It is heavy, dark-colored, and magnetic; so you are thinking it must be from outer space. You visualize it falling through the air in a blaze and landing right where you are. Let’s do a reality check. The odds of finding a meteorite are slim even if you see it fall. Most disintegrate before reaching the ground.

Most people have never seen a fulgurite, and many that have probably did not realize what it was at the time. Fulgurites are natural tubes or crusts of glass formed by the fusion of silica (quartz) sand or rock from a lightning strike. Their shape mimics the path of the lightning bolt as it disperses into the ground.

Fluorite Mineral, Bell Hill mine

The importance of minerals in everyday life is hardly recognized by the vast majority of people. To help illustrate how important minerals are to us, perhaps a trip through a normal working day of a geologist will better explain our reliance on minerals.