Geological Glossary |

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A descriptive term used for rocks and other earth materials that have an abundance of calcium carbonate (CaCO3). For example, a calcareous sandstone has up to 50% calcium carbonate.
A soil layer at least 15 cm thick that has been enriched with calcium carbonate (CaCO3). Mineral made of calcium
carbonate (CaCO3). Generally white, easily scratched with knife. Most
seashells are made of calcite or related minerals. This is the lime
of limestone.
Large, generally circular, fault-bounded depression caused by the withdrawal of magma from below a volcano or volcanoes. Commonly, the magma erupts explosively as from a giant volcano and, falling back to Earth as volcanic ash, fills the caldera so formed.
A sedimentary rock made mainly of calcium carbonate (CaCO3). Limestone and dolomite are common carbonate sedimentary rocks.
A mild acid formed when water and carbon dioxide chemically combine in the atmosphere and soil.This acid is a very important component in the development of cave decorations (speleothems). A natural opening in the
ground extending beyond the zone of light and large enough to permit
the entry of an average human.
A cave or caves having
a complex network of interconnected chambers and passages that constitute
an underground drainage system.
A combination of chemical and mechanical weathering processes act on rock surfaces to produce hollows and caverns. This is also called honeycomb weathering.
One of the processes that work together to turn sediment into sedimentary rock (lithification). Mineral-laden water percolates through sediment with open pore spaces. The spaces are gradually filled by minerals precipitating from the water, binding the grains together. Cenozoic Era The time span between 66.4
million years ago to the present.
Sedimentary rock composed of minerals that were precipitated from water. This process begins when water traveling through rock dissolves some of the minerals, carrying them away from their source. Eventually these minerals are redeposited, or precipitated, when the water evaporates away or when the water becomes over-saturated. The process that changes
the chemical makeup of a rock or mineral at or near the Earth’s
surface. Chemical weathering alters the internal structure of minerals
by the removing and/or adding elements. Compare with mechanical weathering.
A very fine-grained sedimentary rock made of quartz. Usually made of millions of globular siliceous skeletons of tiny marine plankton called radiolarians. Black chert is called flint.
Family of platy silicate minerals containing various amounts of magnesium, iron, aluminum, water, and small amounts of other elements. Some mineralogists include chorites in the mica family because the crystals form small flakes. Commonly green.
A bubbly (vesicular) volcanic
rock fragment that forms when molten, gas-filled lava is thrown into
the air, then solidifies as it falls. A volcanic cone built almost
entirely of loose volcanic fragments, ash, and pumice (pyroclastics
or tephra) clast A fragment of a pre-existing
rock or fossil embedded within another rock.
A sedimentary rock composed of fragments (clasts) of pre-existing rock or fossils. (=Detrital sedimentary rocks) clay A family of platy silicate
minerals that commonly form as a product of rock weathering. Also,
any particle smaller than 1/256 of a millimeter in diameter. cleavage The tendency of a mineral to break along weak planes.
Loose particles of rock
or mineral (sediment) that range in size from 64 - 256 millimeters
in diameter. Cobbles are a size of gravel larger than pebbles, but
smaller than boulders. compaction Occurs when the weight of overlying material compresses more deeply buried sediment. Along with cementation, this process converts sediments to solid rock. composite volcano See stratovolcano. conformable Rock layers that were deposited in sequence without episodes of erosion between deposition of layers. . A sedimentary rock rock
made of rounded rock fragments, such as pebbles, cobbles, and boulders,
in a finer-grained matrix. To call the rock a conglomerate, some of
the consituent pebbles must be at least 2 mm (about 1/13th of an inch)
across.
Metamorphism caused by heat from an igneous intrusion. continental collision Convergence of two continental
plates. Such a convergence between the Indian and Eurasian plates
is responsible for producing the Himalayas.
The rigid, outer layer of relatively low density rock that makes up the continents. continental drift A hypothesis proposed by
Alfred Wegener suggesting that the continents are not stationary,
but have 'drifted' through time. Plate tectonics is the name for the
theory that provided the evidence necessary to support Wegener’s
hypothesis.
A boundary in which two
plates collide. The collision can be between two continents (continental
collision), an relatively dense oceanic plate and a more buoyant continental
plate (subduction zone) or two oceanic plates (subduction zone).
The innermost layer of
the Earth, made up of mostly of iron and nickel. The core is divided
into a liquid outer core and a solid inner core. The core is the most
dense of the Earth’s layers.
The depression produced by a meteorite impact or at the summit of a volcano. The relatively stable nucleus
of a continent. Cratons are made up of a shield-like core of Precambrian
Rock and a buried extension of the shield.
The rocky, relatively low
density, outermost layer of the Earth.
Growth of minerals (crystalline solids) from a liquid or gas.
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