Geology of San Marcos Foothills
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Glossary
Alluvial fanA fan-shaped deposit of sediment when a stream slope is reduced, often at the base of mountains.
BentoniteAn elastic, soapy-textured clay material that swells extensively in water to
form a gelatinous mass several times its original volume.
ChaparralA close growth of low evergreen oaks or other dense thicket.
ConcretionA concentricity of mineral growth around a central nucleus, resulting in a more highly cemented area within the surrounding rock matrix.
Differential erosionA variation in the decomposition rate of a rock, caused by variations in cement strength and resulting in varying surface textures and features.
DepositionThe coming to rest of eroded material, from a higher place to a low place.
ErosionThe transportation of weathered material by wind, water, ice, or gravity.
FaultA break or crack in the earth's crust along which movement has occurred.
FoldsWavelike undulations in rock beds caused by compressional stresses.
ForaminiferaSmall, single-celled organisms which float on the ocean surface (planktonic foraminifera) or live near the ocean bottom (benthonic foraminifera).
FormationA distinct type of rock that covers an area large enough to show on a map.
FossilizationThe preservation in rock of the remains or traces of organic material.
FracturesCracks in rock.
Graded bedsA depositional rock structure characterized by larger grains at the bottom and fining upward to smaller grains at the top; also called a fining upward sequence.
Laminar beddingThin parallel layers of sedimentary rock caused by repeated similar depositional action.
LithificationThe formation of rock by compaction and cementation.
MatrixThe fine-grained portion of a rock that encompasses the larger grains.
MineralA naturally occurring, inorganic crystalline solid with a definite internal structure and a specific chemical composition.
OxidationIn rocks, the chemical breakdown of rock material by exposure to air and water. In chemistry, the removal of one or more electrons from an atom or ion, commonly causing elements to combine with oxygen.
PermineralizationThe preservation in rock of organic material when it is permeated by a resistant substance that hardens and cements the material as a fossil.
RedbedsAny group of oxidized sedimentary rocks characterized by a red or maroon color.
RockAn aggregate of minerals.
SandstoneA sedimentary rock formed from sand-sized grains.
SavannahA plain characterized by coarse grasses and scattered tree growth where rainfall is seasonal.
Sedimentary rockRock formed from the weathered products of pre-existing rocks which have been transported, deposited, compacted, and cemented.
ShaleA fine-grained sedimentary rock formed from clay-sized grains.
SiltA sediment with very fine grains between 1/16 and 1/256 milimeters in diameter.
Spheroidal WeatheringA weathering process that produces a spherical shape from a blocky shape.
SubsideTo sink to a lower level.
Tectonic plateA large, rigid section of earth crust that moves as a unit on the surface of the earth.
TectonicsThe study of the major structural features of the earth's crust, and of the large-scale processes that deform it.
Transgressing seaThe onland movement of shoreline caused by a rise in sea level.
Trace fossilsImpressions left in rock by living things.
WeatheringThe disintegration and compositional breakdown of rock at the earth's surface.

Geology of the San Marcos Foothills by Susan Bartz

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