Loose particles of rock or mineral (sediment) that range in size from 0.0625 - 2.0 millimeters in diameter.
Sedimentary rock made mostly of sand-sized grains.
A type of potassium feldspar that forms only at high temperature. Common in potassium-rich volcanic rocks.
A cliff formed by faulting, erosion, or landslides. (Also called escarpment).
Metamorphic rock usually derived from fine-grained sedimentary rock such as shale. Individual minerals in schist have grown during metamorphism so that they are easily visible to the naked eye. Schists are named for their mineral constituents. For example, mica schist is conspicuously rich in mica such as biotite or muscovite.
Sea stacks are blocks of erosion-resistant rock isolated from the land by sea.
Loose, uncemented pieces of rock or minerals.
Refers to earthquakes.
Sedimentary rocks are formed from pre-existing rocks or pieces of once-living organisms. They form from deposits that accumulate on the Earth's surface. Sedimentary rocks often have distinctive layering or bedding.
A family of silicate minerals rich in magnesium and water, derived from low-temperature alteration or metamorphism of the minerals in ultramafic rocks. Rocks made up of serpentine minerals are called serpentinite. Serpentine minerals are light to dark green, commonly varied in hue, and greasy looking; the mineral feels slippery.
Sedimentary rock derived from mud. Commonly finely laminated (bedded). Particles in shale are commonly clay minerals mixed with tiny grains of quartz eroded from pre-existing rocks. Shaley means like a shale or having some shale component, as in shaley sandstone.
Overland flow of water in thin sheets
Refers to the property of many clays to swell when wetted and shrink when dried.
Silicon dioxide (SiO2). One of the most common compounds in the Earth's crust. Common window glass is made of silica. The building block of the mineral quartz and other silicate minerals.
Refers to the chemical unit silicon tetroxide, SiO4, the fundamental building block of silicate minerals. Silicate minerals make up most rocks we see at the Earth's surface.
Generally refers to a rock rich in quartz.
Loose particles of rock or mineral (sediment) that range in size from 0.002 - 0.0625 millimeters in diameter. Silt is finer than sand, but coarser than clay.
A sedimentary rock made mostly of silt-sized grains.
A depression in the surface commonly found in in karst landscapes. Sinkholes often form where limestone or some other soluble rock is partially dissolved by groundwater, then collapses to form a depression. Sinkholes are often "bowl-shaped" and can be a few to many hundreds of meters in diameter. Also known as dolines.
A type of landslide in which a mass of rock breaks away along a curved surface and rotates more or less intact downslope. The sliding mass of rock is called a slump block.
All loose, unconsolidated earth and organic materials above bedrock that support plant growth.
The exploration and study of caves.
A deposit formed in caves when calcium carbonate (CaCO3) or some other mineral precipitates from drips or thin films of water. Stalactites and stalagmites are common speleothems.
Plutons of roughly the same age which that intruded several tectonic terranes after the terranes were faulted together. The plutons do not really "sew" the terranes together, but they help record when terranes were assembled.
Stope blocks form when injection of intrusive igneous rock weakens the solid rock surrounding it, causing blocks to loosen and sink into the molten mass.
A process of erosion where one stream erodes headward, diverting some of another stream's drainage into its own channel. Also called stream piracy.
A thin, discontinuous mineral vein or rock layer.
Process of one crustal plate sliding down and below another crustal plate as the two converge. The subduction zone is the area between the two plates, somewhat like a giant reverse fault.
Fan or cone-shaped accumulation of sedimentary debris--sand, gravel, mud--under the ocean along the edge of the land, either a continent or a volcanic arc. Fans may be a few miles to a hundred or so miles across.
Any loose, unconsolidated sedimentary deposit lying on bedrock.
A upward-curving (concave) fold in rock that resembles a trough. The central part contains the youngest section of rock.
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