Lithosphere Flashcards
A naturally occurring inorganic solid with a definite structure and composition
Mineral
Mineral identification tests (4 types)
Hardness, luster, streak, cleavage and fracture
Hardness of a mineral can be tested by:
Scratching the mineral with a set hardness level
Defines as metallic or nonmetallic
Luster
Streak
The color of the mineral when it is broken up and powdered
Cleavage
Smooth, flat breakage
Fracture
Rough, jagged breakage
Rock formed from cooled magma
Igneous
Intrusive igneous rocks
Rocks that forms when magma cools under the earths surface
Extrusive igneous rocks
Rocks that formed above the earths surface
Dense, heavy, dark colored igneous rock that is rich in iron and magnesium. Found at seas
Basaltic igneous rocks
Light colored rocks with less density than basaltic rocks. Rich in silicon and oxygen
Granitic igneous rocks
Rocks that have compositions between granitic and basaltic rocks
Andestic igneous rocks
Metamorphic rocks
Rocks that undergo great pressure and heat at tectonic plate boundaries
Mineral grains flatten and line up in parallel bands
Foliated metamorphic rocks
Rock where no banding occurs, but the grains are smaller.
Non-foliated metamorphic rocks
Rocks made from cemented sediment particles
Sedimentary rocks
Detrial sedimentary rocks
Made from broken fragments of other rocks
Chemical sedimentary rocks
When solution evaporates, the minerals left behind cements together to form a rock
Shield volcano
Quiet eruptions, and spreads basaltic lava in flat layers. The lava flows. Ex. Hawaiian islands
Cinder cone volcanoes
Explosive eruptions that have a steep-sided loose slopes. More mountainous
Magma cooled in air
Tephra (small- cinder large- bombs)
Composite volcanoes
Alternates from quiet and explosive eruptions. Later forms of tephra and slow moving magma. Ex. Mount Saint Helens
Steps of sedimentary rock formation
Weathering (breaking down), erosion (movement), deposition (putting it there), lithification (cement together)
Agents of erosion
Wind, water, gravity, glaciers
Wind
Carries fine sand particles and created dunes
Water
Carries fine sand to pebbles. Creates V shaped valleys
Gravity
Can bring down a ton of sediments down at once. Landslides
Glaciers
Can carry any sediment sizes. It carves U shaped valleys and creates large lakes
Law of original horizontality
Sediments are deposited in flat, horizontal layers. (Steep dips or folding indicates tectonic disturbances)
Principle of superposition
In horizontal layers, the oldest is at the bottom
Law of continuity
A layer will spread across unless: sediment thins our at edge of basin, stops at barriers, or runs into a different type of sediment
Principle of cross-cutting
Faults and igneous intrusion are younger that the rock they cut
Tectonic plates pulling apart makes
Trenches (or volcanoes at the bottom of the ocean; hydrothermal vents)
Tectonic plates running into each other creates
Mountains and volcanoes
Fault lines create
Earthquakes