Geological Terms Beginning With "O"
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A fault that has both horizontal and vertical elements of displacement.
A glassy igneous rock with a composition similar to granite. The glassy texture is a result of cooling so fast that mineral lattices were not developed. Picture of Obsidian.
The geographic area that is seaward of a coastline.
The geographic area above an underground accumulation of oil and natural gas.
A dark-colored shale containing an unusual amount of solid organic material known as kerogen. This shale can be crushed and heated to liberate gaseous and liquid hydrocarbons. At present the expenditure required to process oil shale into a fuel makes this effort marginally profitable or unprofitable.
A stage in the development of a landscape when streams have a low gradient and meander back and forth across broad floodplains. The landscape is marked by meander scars and oxbow lakes.
A small sphere of calcium carbonate no more than a few millimeters in diameter and with a concentric internal structure . These spheres are thought to have formed by inorganic precipitation of calcium carbonate in very thin layers around a grain of sand or a particle of shell or coral. A rock composed primarily of oolites.
A limestone texture that is characterized by spherical grains of calcium carbonate with a concentric internal structure. These grains are thought to form by inorganic precipitation of calcium carbonate around a sand grain or shell particle nucleus.
An adjective used in reference to a substance that does not allow light of visible wavelength to enter or pass through. Minerals with a metallic or submetallic luster are normally opaque.
The typical sequence of rocks in the oceanic crust: from bottom to top: ultrabasic rocks, gabbro, sheeted dikes, pillow basalts, and sea-floor sediments. Igneous rocks and deep-sea sediments associated with divergence zones and the sea-floor environment.
An elliptical or hyperbolic path traveled by a satellite object around a more massive body. For example, the Earth orbits the Sun.
A natural accumulation of a metal, gemstone or other valuable mineral substance, which is rich enough in concentration that it can be mined and processed at a profit.
A mineral that contains a high enough concentration of a useful element or compound that the element or compound can be extracted at a profit.
One of the principles of relative dating. Based upon the good assumption that sedimentary rocks are deposited in horizontal or nearly horizontal layers; then if sedimentary layers are found in an inclined orientation the force that moved them to that orientation must have been applied at some time after their deposition.
A linear or arcuate region of folded and uplifted rocks.
A compressive tectonic process that results in intense folding, reverse faulting, crustal thickening, uplift and deep plutonic activity. A mountain-building episode.
Oscillation Ripple Marks:
Symmetrical ridges in sand or other sediment that are caused by a back-and-forth wave action.
An exposure of bedrock. Outcrops can be formed naturally or by human action. Stream erosion and highway construction can produce outcrops.
A location where water is discharged. Normally used in reference
to where a water treatment facility releases treated water into
The release of juvenile gases and water to the surface from a magma source.
Sorted and stratified sediment deposited in front of a glacier by meltwater streams.
A fold that has both limbs dipping in the same direction, resulting from one of those limbs being rotated through an angle of at least 90 degrees. Overturned folds are found in areas of intense deformation. The name overturned is given because the strata on one limb of the fold are "overturned" or upside down.
A crescent-shaped lake that forms when a meandering stream changes course. Such changes in course frequently occur during flood events when overbank waters erode a new channel.
A chemical reaction in which substances combine with oxygen. For example, the combination of iron with oxygen to form an iron oxide.
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