Geomorphology Flashcards
What is geomorphology?
Study of the crust of the Earth and the forces that effect it from inside and out.
What is responsible for changes on the outside of Earth?
Forces generated inside of Earth
What makes up the surface of the earth?
Areas of land (continents)
Areas of water (oceans) 70% of Earth’s surface
How thick is continental crust?
90 km thick
How thick is ocean crust?
5 km thick
Out of what parts does Earth consist?
Crust
Mantle
Outer core
Inner core
What is the composition of the crust?
Thin outer layer consisting of solid rock/soil
6 - 90 km thick
Thinner under oceans; thicker under continents
Least dense layer
What is the composition of the mantle?
About 2 900 km thick
More dense
Rocks in hot, thick, molten state (magma) - can move and flow
Magma, lava coming from volcano, comes from mantle
What’s the composition of the inner core?
1 200km thick Extremely hot, but solid metallic ball Temperatures 5 000 - 6 000*C Solid, because of enormous pressure from other layers Iron and nickel
What is the composition of the outer core?
2 000 km thick
Very dense, still molten state
Name the three types of major rock.
Igneous
Sedimentary
Metamorphic
What are igneous rocks?
Lava runs down sides of mountain will in time cool down to form very hard rocks.
The two names for magma and why they differ.
Inside crust: magma
Reaches surface: lava
How does magma reach the surface?
Faults or cracks form path along which the magma can reach the surface or spread in between the different rock layers of Earth.
What is intrusive igneous rocks?
Cools down slowly to form course grains with large crystals.
The fault line does not reach the surface, so the magma spreads between the different rock layers.
What is extrusive igneous rock?
Cools down quickly to form fine grains and small crystals.
Pressure is relieved as magma travels up fault lines and erupts to form a volcano on surface
What are the characteristics of igneous rocks?
Massive
Hundreds of meters or km wide
Doesn’t form layers
After millions of years of erosion and weathering, these structures start to appear above surface
Examples, Spitzkoppe (Usakos)
Brandberg (Uis)
Why does crystalline form in igneous rocks?
Many chemical elements in magma
During cooling, these elements combine to form crystals of minerals