s1 Flashcards
Aggregates of one or more minerals
Rocks
Naturally occurring, inorganic solids with a definite chemical composition and crystalline structure.
Minerals
Large, visible crystals. Indicates slow cooling (intrusive).
Coarse-Grained Igneous Rock
Small, invisible crystals. Indicates rapid cooling (extrusive)
Fine-grained Igneous Rock
No crystals, very smooth. Indicates very rapid cooling (extrusive)
Glassy Igneous Rock
High in silica, and light-colored minerals (e.g., granite, rhyolite).
Felsic
Very low in silica, very high in magnesium and iron (e.g., peridotite).
Ultramafic
Over time, sediments are compacted and cemented together to form solid rock.
Compaction and Cementation
Formed from the precipitation of minerals from water
Chemical Sedimentary Rocks
Applies directed stress to the rock, leading to deformation and reorientation of minerals
Formation Process of Metamorphic Rocks - Pressure
Facilitate the exchange of ions, promoting new mineral growth and altering the rock’s composition.
Formation Process of Metamorphic Rocks - Chemically Active Fluids
Occurs when rocks are heated by nearby magma or lava.
Typically affects a small area surrounding the heat source.
Results in non-foliated rocks due to uniform pressure from heat.
Contact Metamorphism
Occurs over large areas due to tectonic forces that produce high pressure and temperature
Common in mountain-building regions.
Results in foliated rocks due to directed pressure from tectonic forces.
Regional Metamorphism
A continuous process of rock formation, alteration, and recycling through geological processes.
The Rock Cycle
- Weathering and Erosion: Igneous rocks are broken down into sediments.
- Transportation and Deposition: Sediments are transported and deposited in layers.
- Compaction and Cementation: Sediments are compacted and cemented to form sedimentary rocks.
From Igneous to Sedimentary