Answer:
(A) When two oceanic plate moves in the opposite direction, it leads to the formation of new crust and the boundary along which this new crust is formed is known as the Mid-Oceanic ridge. For example Mid-Atlantic ridge.
(B) When an oceanic plate crashes with a continental plate, then the oceanic plate being heavier sinks below the continental plate, producing a subduction zone is created, which is commonly known as the Benioff zone. It is marked by deep trenches and deep-focus earthquakes are generated.
(C) When two continental plates share a divergent plate boundary, if slowly undergoes rifting and with the increasing time, the plates get separated from one another forming a rift valley. For example, the East African rift valley system.
(D) Strike-Slip fault zone is the boundary along which two continental plates slide past one another. Shallow-focus earthquakes are generated in this region. For example, The San Andreas fault.
(E) When two continental plates converges then it forms the sandwich pattern, where high mountain ranges occur. The area undergoes extreme thrusting and folding. for example, The Himalaya.
Answer:
you said you had more so I answer
people who live longer than the world average
Explanation:
A country scores a higher HDI when the lifespan is higher, the education level is higher, and the gross national income GNI (PPP) per capita is higher
Answer:
Position 4
Explanation:
Position 1 and 3 are easily identifiable as Summer and Winter as the Americas are are facing directly at and away from the sun. Position 2 is Spring as North America is getting more sunlight that position 4, leaving position 4 to be autumn/fall
Hope you can follow that mess of logic :/
Answer:
PERMAFROST LAYER
Explanation:
Permafrost layer is usually defined as the thick layer of soil that is mixed with the broken rock fragments and other sediments, and are covered by ice throughout the year. These are mostly found in the higher latitudinal region, where the thickness of these layers ranges from a few meters to tens and hundreds of meters. The melting of these layers in these regions leads to an increase in the sea level.
For example, the permafrost layers of tundra and subarctic zones in Russia and its nearby areas, which have a thickness of about three meters.
The P wave is the primary preliminary wave because it is the first to arrive at a seismic station after an earthquake.
