Earth's Interior Flashcards
What are the 2 main types of evidence that geologists use to learn about Earth’s interior?
Direct evidence from rock samples
Indirect evidence from seismic waves
*(rock samples and seismic waves)
Direct evidence from rock samples
Rocks drilled from deep inside Earth; allows geologist to make inferences about conditions
Indirect evidence from seismic waves
Seismic waves produced by earthquakes allow scientists to measure the speed in which they travel giving clues to the structure of the planet
What are the 3 main layers of Earth that vary greatly in size, composition, temperature, and pressure
The crust
The mantle
The core
The crust
- layer of solid rock that forms Earth’s outer “skin”
- includes both dry land (continental crust) and ocean floor (oceanic crust)
- rocky outermost layer of earth
- least dense layer of the geosphere
- continental crust is about 4 times thicker than the oceanic crust
Oceanic crust
Consists mostly of basalt
Continental crust
Consists mainly of granite
The mantle
Middle layer of the earth Layer of solid, hot rock 40 kilometers beneath the surface divided into layers: - lithosphere - asthenosphere - lower mantle
Lithosphere
- Earth’s crust & mantle
- broken into giant plates
- plates rest on somewhat fluid part of mantle called “asthenosphere”
Uppermost part of the mantle and the crust for a ridge layer about 100 kilometers thick
Asthenosphere
- lies below lithosphere
- upper part of mantle
- begins at 75 miles –> 125 miles
- partially molten rock
- ‘asthenes’ in Greek means “weak”
- can be pushed and formed like silly puddy
Softer part of mantle which is hotter and under increased pressure
Lower mantle
Solid material extending all the way to Earth’s core
The core
- made mostly of the metals iron and nickel
- consists of two parts:
~ outer core
~ inner core - extremely drguhihtfyguhihigutfy
movement of liquid outer core creates Earth’s magnetic field
Outer core
Layer of molten metal that surrounds inner core
Inner core
Dense ball of solid metal
“Pan”=
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