What is plate tectonic explain with diagram?
What is plate tectonic explain with diagram?
Plate tectonics is a scientific theory that explains how major landforms are created as a result of Earth’s subterranean movements. The theory, which solidified in the 1960s, transformed the earth sciences by explaining many phenomena, including mountain building events, volcanoes, and earthquakes.
What are the 5 stages of an earthquake?
What are the 5 stages of earthquake? The fives stags of an earthquake are elastic strain, dilatancy, influx of water, earthquake, and aftershocks. Elastic strain occurs as the rocks build up strain as plates move. Dilatancy occurs as rocks break and increase in size.
What is the plates of an earthquake?
what are tectonic plates? Tectonic plates are gigantic pieces of the Earth’s crust and uppermost mantle. They are made up of oceanic crust and continental crust. Earthquakes occur around mid-ocean ridges and the large faults which mark the edges of the plates.
What are the 3 types of tectonic earthquakes?
Three Kinds of Earthquakes
- Shallow fault earthquakes. A fault is a break in the rock beneath our feet.
- Subduction zone earthquakes. The largest earthquakes ever recorded are subduction zone earthquakes.
- Deep earthquakes. Deep earthquakes occur in the subducting ocean slab, deep beneath the continental crust.
What are the 4 types of tectonic plate movement?
What are the major plate tectonic boundaries?
- Divergent: extensional; the plates move apart. Spreading ridges, basin-range.
- Convergent: compressional; plates move toward each other. Includes: Subduction zones and mountain building.
- Transform: shearing; plates slide past each other. Strike-slip motion.
What are the 4 types of earthquakes?
There are four different types of earthquakes: tectonic, volcanic, collapse and explosion. A tectonic earthquake is one that occurs when the earth’s crust breaks due to geological forces on rocks and adjoining plates that cause physical and chemical changes.
How earthquakes are formed step by step?
The tectonic plates are always slowly moving, but they get stuck at their edges due to friction. When the stress on the edge overcomes the friction, there is an earthquake that releases energy in waves that travel through the earth’s crust and cause the shaking that we feel.
How do tectonic plates move?
The plates can be thought of like pieces of a cracked shell that rest on the hot, molten rock of Earth’s mantle and fit snugly against one another. The heat from radioactive processes within the planet’s interior causes the plates to move, sometimes toward and sometimes away from each other.
