Plate tectonics Flashcards
Lithosphere
the solid, outer layer of the earth that consists of the crust and the rigid upper part of the mantle
Asthenosphere
the soft layer of the mantle on which the tectonic plates move
Mesosphere
the strong lower part of the mantle between the asthenosphere and the outer core
Inner Core
The Earth’s inner core is the Earth’s innermost part. It is primarily a solid ball with a radius of about 1,220 kilometers, which is about 70% of the Moon’s radius. It is composed of an iron–nickel alloy and some light elements
Outer Core
The outer core of the Earth is a fluid layer about 2,300 km thick and composed of mostly iron and nickel that lies above Earth’s solid inner core and below its mantle.
Seismic waves
a wave of energy that travels through the earth and away from an earthquake in all directions
Oceanic waves
In fluid dynamics, wind waves, or wind-generated waves, are surface waves that occur on the free surface of bodies of water. They result from the wind blowing over an area of fluid surface.
Continental crust
The continental crust is the layer of igneous, sedimentary, and metamorphic rocks that forms the continents and the areas of shallow seabed close to their shores, known as continental shelves.
Density
the ratio of the mass of a substance to the volume of the sunstance
Alfred Wegener
Alfred Lothar 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 hypothesis that states that the continents once formed a single land mass, broke up, and drifted to their preset locations
Convergent boundary
In plate tectonics, a convergent boundary, also known as a destructive plate boundary, is a region of active deformation where two or more tectonic plates or fragments of the lithosphere are near the end of their life cycle
Divergent boundary
In plate tectonics, a divergent boundary or divergent plate boundary is a linear feature that exists between two tectonic plates that are moving away from each other.
Transform boundary
Transform boundaries are places where plates slide sideways past each other. At transform boundaries lithosphere is neither created nor destroyed. Many transform boundaries are found on the sea floor, where they connect segments of diverging mid-ocean ridges. California’s San Andreas fault is a transform boundary.
Sea-floor spreading
Seafloor spreading is a process that occurs at mid-ocean ridges, where new oceanic crust is formed through volcanic activity and then gradually moves away from the ridge. Seafloor spreading helps explain continental drift in the theory of plate tectonics