Inside the earth Flashcards
Lithosphere
- Outermost, rigid layer of the earth (15-300 km thick).
- Made up of the crust and outer mantle.
- Divided into pieces called tectonic plates.
Asthenosphere
- 250 km thick.
- Plastic layer of the mantle on which pieces of the lithosphere move.
- Made of solid rock that flows very slowly.
Mesosphere
- 2550 km.
- Strong, lower part of mantle.
- Extends from the bottom of the asthenosphere to the earths core.
Outer Core
- 2200 km.
- liquid layer that lies beneath the mantle and surrounds the inner core.
Inner Core
- 1230 km thick.
- Solid, denser center of Earth.
Seismic Waves
- The inside of Earth is mapped with seismic waves from earthquake
Oceanic Crust
the relatively thin part of the earth’s crust which underlies the ocean basins. It is geologically young compared with the continental crust and consists of basaltic rock overlain by sediments
Continental Crust
the relatively thick part of the earth’s crust that forms the large landmasses. It is generally older and more complex than the oceanic crust
Density
the degree of compactness of a substance
Alfred Wegener
was a German polar researcher, geophysicist and meteorologist. During his lifetime he was primarily known for his achievements in meteorology and as a pioneer of polar research
Continental Drift
the gradual movement of the continents across the earth’s surface through geological time
Convergent Boundary
are areas on Earth where two or more lithospheric plates collide. One plate eventually slides beneath the other causing a process known as subduction. there caused by earthquakes
Divergent Boundary
a divergent boundary or divergent plate boundary is a linear feature that exists between two tectonic plates that are moving away from each other. Divergent boundaries within continents initially produce rifts which eventually become rift valleys.
Transform Boundary
is a plate boundary where the motion is predominantly horizontal. It ends abruptly and is connected to another transform, a spreading ridge, or a subduction zone.
Sea-floor Spreading
the formation of new areas of oceanic crust, which occurs through the upwelling of magma at midocean ridges and its subsequent outward movement on either side.