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11 Cards in this Set

  • Front
  • Back

Chemical Weathering

Alteration of chemical composition

Mineral

A solid inorganic substance of natural occurrence.

Mechanical Weathering

the breakdown of rock into smaller pieces by physical means

Sedimentary rock

A type of rock that forms when particles from other rocks or the remains of plants and animals are pressed and cemented together

Igneous rock

rock that forms when magma cools and solidifies

Metamorphic rock

rock that has been changed by heat and pressure

Watershed

An ecosystem where all water runoff drains into a single body of water

Specific Gravity

SG = w / Δ V



'w' is a mineral's weight in grams (g) and Δ V is the volume of water it displaces.


In other words, SG refers to a mineral's density. Minerals with lower SG for example would feel relatively light for their size.

Detrital

rocks form by sediment (debris, rock fragment, minerals, etc.) accumulation.


Key properties:


Mineral Composition: stability of minerals in rocks at the earth’s surface


Stable: resistant to weathering


Unstable: weathers quickly


Texture: refers to features of a rock’s particles (not the rock they compose)


Sorting: average particle size


Well-sorted = mostly same size particles; poorly-sorted: variety of particle sizes


Shape: indicative of transport history


Longer transport history smoother particle (more weathering)


Size: indicative of environmental energy


Example: rivers contain high energy, so they can move larger particles; lakes contain low energy (they move less) and so can move only smaller particles

Chemical

rocks form by substance crystallization or precipitation.


Subcategories:


Organic: rocks develop from accumulated plant/animal remains under water


Inorganic: no plant/animal remains involved in rock development

Lithification

The process through which sediment becomes rock


Two key types:


Compaction: rock forms from pressure of sediment above


Cementation: mineral agents bind sediment