Geological Terms Beginning With "F"
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a) The characteristics of a rock or sediment unit that reflect its environment of deposition and allow it to be distinguished from rock or sediment deposited in an adjacent environment.
b) A mass of rock that can be recognized by its composition, structures or fossil content and mapped on the basis of those characteristics.
"Fancy sapphire" is a name used for a gem corundum that has a body color other than blue (sapphire) or red (ruby).
A contractual agreement in which a mineral rights owner or lessee assigns a working interest to another party who will become responsible for specific exploration, development or production activities.
A fracture or fracture zone in rock along which movement has occurred. When movement occurs the vibrations that are produced are known as an earthquake.
A linear mountain that is bounded on both sides by normal faults. The photo is a view of Mount Moran near Jackson Lake Junction, Wyoming, part of the Teton Range.
A very slow movement that occurs on faults in response to continuous
tectonic deformation. The deformation might not be accompanied by
earthquake activity. Faults that creep usually have fewer earthquakes than
faults that move suddenly. The photo shows deformed pavement in a fault
zone that crosses under Foothill Boulevard south of Hayward, California.
Crushed and smeared rock debris that is found between the two walls of a
fault produced by crushing action of fault movement. The photo shows
serpentinite gouge in the Bartlet Springs Fault.
The intersection of a fault with Earth's surface, often as seen in the
field, on an aerial photo or on a satellite image. A line on a geologic
map that represents the intersection of a fault with the Earth's surface.
The image is an oblique aerial photo of the Banning Fault in the northern
portion of the Coachella Valley of California.
An area of rock that has numerous fractures of similar trend and dip. Rocks usually do not fail with a clean break, instead they fail through the formation of numerous fractures along a zone of failure. As a result, many named "faults" are actually zones of fractured rock.
The term also has a regulatory use. These "fault zones" are geographic areas where buildings and land use are subject to regulation because they are thought to be exposed to the hazard of a nearby fault. These fault zones are usually drawn on maps and published by a government agency for public viewing.
A principle of relative dating that is based upon the observed sequence of organisms in the rock record. The relative age of two rock units can frequently be determined by matching the fossils found in those rocks to their positions in the rock record.
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A term used to describe an igneous rock that has a large percentage of light-colored minerals such as quartz, feldspar, and muscovite. Also used in reference to the magmas from which these rocks crystallize. Felsic rocks are generally rich in silicon and aluminum and contain only small amounts of magnesium and iron. Granite and rhyolite are examples of felsic rocks. (See mafic to contrast.)
Colored flashes of light emitted from a gemstone that result from incident light being separated into its component colors as it passes through the stone. Each gem material has a characteristic dispersion. Some have exceptional dispersion and produce a very intese fire. Although many people believe that diamond has the strongest dispersion of all gems, a few gems such as sphalerite, demantoid garnet (shown in the photo), sphene, and zircon have an even greater dispersion.
A translucent-to-transparent opal with a warm background color of yellow, orange or red. It may or may not exhibit a "play-of-color." The warm, uniform background color is what defines the stone.
An open fracture or crack in Earth's surface that can result from a wide variety of causes that include: earthquake, volcanic activity, dessication, subsidence, mass wasting, groundwater withdrawal, oil production, faulting, and other movements. Fissures associated with volcanic activity can produce large outpourings of magma. Others can be the initial step of forming an igneous dike. Some fissures are filled with valuable minerals.
A deep, narrow, steep-walled, U-shaped valley that was carved by a glacier and is now occupied by the sea.
An overflow of water onto lands that are normally above local water levels. Can be caused by stream discharge exceeding the capacity of the stream channel, storm winds and reduced pressure drawing water from a lake or ocean onto the coastline, dam failure, lake level increase, local drainage problems or other reasons.
A sequence of parallel to subparallel basalt flows that were formed during a geologically brief interval of time and which covered an extensive geographic area. Thought to have formed from simultaneous or successive fissure eruptions. In the photo are layered flood basalts from the Columbia River. Public domain image by William Borg.
A tidal current that moves towards land as high tide approaches, covering
the inter-tidal zone. Flood currents can temporarily reverse the flow of
rivers that enter the ocean. They can be very strong at the openings of
bays and between barrier islands, where large amounts of water must flow
through a narrow opening in a limited amount of time. The arrows in the
image show the directions that water would flow as flood currents enter a
river and fill lagoons behind barrier islands.
An area of alluvium-covered, relatively level land along the banks of a stream that is covered with water when the stream leaves its channel during a time of high flow.
A water height that is reached when the discharge of a stream exceeds the capacity of the channel.
A tidal current that generally moves landward and occurs during the part of the tide cycle when sea level is rising. (See neap tide for contrast.)
A well that taps an aquifer that is under enough pressure to force water to the surface. Caused when the aquifer has a recharge area at a higher elevation.
A small amount of fluid (liquid and/or gas) trapped within a rock and which is thought to represent the fluid from which the rock crystallized.
The ability of a material to temporarily absorb a small amount of light and an instant later release a small amount of light of a different wavelength. This change in wavelength causes a temporary color change of the mineral in the eye of a human observer. The color change of fluorescent materials is most obvious when the materials are illuminated in darkness by ultraviolet light (which is not visible to humans) and the materials release visible light. A more detailed explaination of fluorescence can be found in our article on fluorescent minerals. The photo shows specimens of opal from Virgin Valley, Nevada in normal light and under shortwave ultraviolet light. Image courtesy of RockTumbler.com, a GeoShops website.
Fluorescent minerals are minerals that have the ability to be stimulated by ultraviolet light and release a fluorescent glow. About 15% of minerals will fluoresce in wavelengths that are visible by people. Some require illumination by longwave ultraviolet light, some require illumination by shortwave ultraviolet light. Geology.com store has small collections of fluorescent minerals, inexpensive ultraviolet lamps, and UV-blocking safety glasses.
Fluorite is an important industrial mineral composed of calcium and fluorine (CaF2). It is used in a wide variety of chemical, metallurgical and ceramic processes. Specimens with exceptional diaphaneity and color are cut into gems or used to make ornamental objects.
A point beneath Earth's surface where the vibrations of an earthquake are thought to have originated. Also known as a hypocenter.
A bend or flexure in a rock unit or series of rock units that has been caused by crustal movements. Folds frequently form near convergent plate boundaries where the rock units are under compression and the folds accomodate crustal shortening. Sketch of folds in outcrop by Sir Charles Lyell.
The planar or layered characteristics of metamorphic rocks that are evidence of the pressures and/or temperatures to which the rock was exposed. These can be structural such as cleavage, textural such as mineral grain flattening or elongation, or compositional such as mineral segregation banding. The photo shows a phyllite from Frederick County, Maryland.
A group of tiny organisms, protozoans that belong to the subclass Sarcodina, order Foraminifera. They produce a very thin calcium carbonate test (shell) with one to many chambers. They are usually marine, less then one millimeter in size, and their tests can make up a significant portion of the carbonate sediment in some areas. The image shows foraminifera collected from a sediment-trap moored in the northern Gulf of Mexico by USGS workers.
A calcareous sea-floor sediment composed primarily of foraminifer tests. The image shows a lab dish containing calcareous ooze dredged from the floor of the Arctic Ocean.
The tectonic region between a subduction zone and its associated volcanic
arc. This is the area underlain by the subducting plate. Image by USGS.
Activities located outside of the United States, its offshore territorial waters, commonwealth territories, and protectorates.
Small earthquakes that precede the largest earthquake of an earthquake
sequence. Some researchers believe that they may be of value for
predicting a major earthquake, but not all large earthquakes are
accompanied by foreshocks.
The distinctly dipping sediment layers deposited on the front of a prograding delta or on the lee side of a sand dune.
A laterally continuous rock unit with a distinctive set of characteristics that make it possible to recognize and map from one outcrop or well to another. The basic rock unit of stratigraphy.
Remains, imprints or traces of an ancient organism that have been preserved in the rock record. Bones, shells, casts, tracks and excrement can all become fossils.
A carbon-rich rock material or fluid, of organic origin that can be produced and burned as a fuel. Coal, oil and natural gas are examples of fossil fuels.
A vent that emits hot gases to the atmosphere, usually associated with past or current magmatic activity below. Some are active for a short amount of time before stopping permanently, some are intermittent and some are active for centuries. Common gases include: carbon dioxide, sulfur dioxide, hydrogen chloride, hydrogen sulfide, all of which can be deadly. The photo shows a fumarole on the flank of Kilauea Volcano in Hawaii with yellow crystals of sulfur that have been deposited by sublimation from the escaping gas.
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