Skip to main content
U.S. flag

An official website of the United States government

Publications

Results from our Program’s research and minerals information activities are published in USGS publications series as well as in outside journals.  To follow Minerals Information Periodicals, subscribe to the Mineral Periodicals RSS feed.

Filter Total Items: 2294

D is for diamond

Real diamonds are a girl's best friend, but synthetic ones opened up a whole new world for granite.
Authors
W. H. Langer

C is for cactolith

Geologic jargon - though handy for triple-word scores - should be used in moderation.
Authors
W. H. Langer

B is for blinding

An enterprising operator finds a solution to a geologic problem that had been in the making for 1.4 million years.
Authors
W. H. Langer

A is for aggregate

No abstract available.
Authors
W. H. Langer

H is for highway

From cow paths to freeways, we seldom appreciate what went into America's highway system.
Authors
W. H. Langer

K is for potassium

K - the chemical symbol for the element/metal potassium.
Authors
W. H. Langer

L is for lava

From Mt. Vesuvius to Hawaii, molten rock continues to leave its mark.
Authors
W. H. Langer

J is for jack

The early days of drilling created a test of strength and endurance for miners.
Authors
W. H. Langer

I is for isinglass

Once commonly used in coal and wood-burning stoves, U.S. production of mica has all but ceased.
Authors
W. H. Langer

Geometry and kinematics of the eastern Lake Mead fault system in the Virgin Mountains, Nevada and Arizona

The Lake Mead fault system is a northeast-striking, 130-km-long zone of left-slip in the southeast Great Basin, active from before 16 Ma to Quaternary time. The northeast end of the Lake Mead fault system in the Virgin Mountains of southeast Nevada and northwest Arizona forms a partitioned strain field comprising kinematically linked northeast-striking left-lateral faults, north-striking normal fa
Authors
Sue Beard, David J. Campagna, R. Ernest Anderson

Kinetics of selenium release in mine waste from the Meade Peak Phosphatic Shale, Phosphoria Formation, Wooley Valley, Idaho, USA

Phosphorite from the Meade Peak Phosphatic Shale member of the Permian Phosphoria Formation has been mined in southeastern Idaho since 1906. Dumps of waste rock from mining operations contain high concentrations of Se which readily leach into nearby streams and wetlands. While the most common mineralogical residence of Se in the phosphatic shale is elemental Se, Se(0), Se is also an integral compo
Authors
Lisa L. Stillings, Michael C. Amacher