3 minute read

Rocks

Current Research



Scientists who study rocks attempt to answer a wide variety of questions: What do rocks and the ratios of stable to unstable isotopes within rocks tell us about the age of the Earth, the times at which the Earth's tectonic plates collided to produce mountains, and global warming? At what times were glaciers present on different continents? Where might we expect to have earthquakes and volcanic eruptions? What types of fossils occur in rocks and how do the fossils differ among rocks from all over the world? In which rocks might we find safe supplies of water, hydrocarbons, and mineral resources such as copper, diamonds, graphite, and aluminum? Although these problems are not often easy to solve, rocks supply important information about them.



Scientists examine rocks in various settings. Some scientists go out to places where rocks are exposed at the surface of the Earth in order to map occurrences and to collect samples of rocks for further study in the laboratory. Others work exclusively in the laboratory examining thin slices of rock under microscopes, determining the structure and chemical composition of individual crystals within a rock, determining the ratios of different isotopes of atoms within a crystal or rock, or examining the fossils in rocks. Scientists who work in different areas of Earth try to compare the rocks and fossils they find in order to determine how the Earth has changed through time. For example, the eastern coast of South America and the western coast of Africa share many common rocks and fossils, suggesting that these areas might have been closer in the past.

Scientists also pay close attention to several significant ongoing phenomena: large, destructive earthquakes in California and Japan; a surge in the Bering Glacier of Alaska, the largest glacier in North America; and volcanic activity in Mexico, West Indies, Indonesia, Papua New Guinea, and Italy. Scientists are actively involved in the search for safe locations to dispose of some of our dangerous wastes. Our understanding of Earth's processes are also helping unravel questions about other planets and astronomical bodies in our solar system. In addition, studies of how and where rocks form continue.

See also Geology; Metal; Ore.


Resources

Books

Chesterman, Charles W. National Audubon Society Field Guide to North American Rocks and Minerals. New York: Alfred A. Knopf, 2001.

Monroe, James S. Physical Geology: Exploring the Earth. Pacific Grove, CA: Brooks/Cole-Thomson Learning, 2001.

Oxlade, Chris. Rock. Chicago: Heinemann Library, 2002.


Other

The Standard Deviants. The Rockin' World of Geology, Parts 1 and 2 (Videorecording) Falls Church, VA: Cerebellum Corporation, 1997.


Gretchen M. Gillis

KEY TERMS


. . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . .

Cementation

—Process through which minerals are glued together, usually as a result of precipitation of solids from solutions in sediments. Calcite, quartz, and clay minerals such as chlorite are common cement-forming minerals in sedimentary rocks.

Compaction

—Reduction of volume of material. Sediments typically compact following burial beneath newer sediments.

Igneous rock

—Rock formed by solidification of molten minerals.

Lava

—Molten rock that occurs at the surface of the Earth, usually through volcanic eruptions. Lava solidifies into igneous rock when it cools.

Magma

—Molten rock found below the surface of the Earth. It can crystallize, or solidify, to form igneous rock.

Metamorphic rock

—Rock formed by alteration of preexisting rock through changes in temperature, pressure, or activity of fluids.

Mineral

—A naturally occurring, inorganic substance with a definite chemical composition and structure.

Rock

—A naturally occurring solid mixture of minerals.

Rock cycle

—The processes through which rocks change from one type to another, typically through melting, metamorphism, uplift, weathering, burial, or other processes.

Sedimentary rock

—Rock formed by deposition, compaction, and cementation of weathered rock or organic material, or by chemical precipitation. Salt and gypsum form from evaporation and precipitation processes.

Uplift

—An episode in the history of a region when tectonic forces lift the region's crust to a higher elevation.

Weathering

—Biological, chemical, and mechanical attack on rock which breaks it up and alters it at or near the surface of the Earth.

Additional topics

Science EncyclopediaScience & Philosophy: Revaluation of values: to Sarin Gas - History And Global Production Of SarinRocks - The Rock Cycle, Current Research - Types of rocks