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Rock Cycle Process
is a continious process where rock transform from one type to another due to geological forces
Igneous rocks
form when magna cools and solidifies
weathering and erosion
breaks rock into sediments, which compact and cement to from "sedimentary rocks"
metamorphic rocks
Intense heat and pressure beneath the earth's surface
Igneous rocks
are formed through the solidifcation of magna, lava or pyroclastic materials
latin word= Ignis or fire
Intrusive
magna cools slowly undersground, forming large crystals
Extrusive(volcanic)
Lava cools rapidly on the surface, forming small crystals or glassy texture
Common location of Igenous Rocks
-Major parts of the contintents and almost all oceanic crust at around 4/5
-Near convergenet and divergent plate boundaries
Types of Magna
-Felsic
-Intermediate
-Mafic
-Ultramafic
Felsic
Contains more than 65% silica
ex. Granite, Rhyolite
Intermediate
Contains about 53% to 65% silica and has a composition between mafic and felsic
example. Diorite, Andesite
Mafic
Contains about 45 to 52% silica
ex. Basalt and Gabbro
Ultramafic
Contains less than 45% silica
ex. Peridotite
Sedimentary Rocks
Formed from sediment, which originates through process of weathering, erosion, and deposition
Derital Sediment
soild particles broken of other rocks
Chemical Sediment
Subtances extracted from solutions through inorganic processes
Detrital sedimentary rocks
formed from the accumulation of particles like gravel, sand, silt, and clay.