Answer:
d.is movement along a fault without an accompanying earthquake.
Explanation:
Fault creep is movement along a fault without an accompanying earthquake.
Well the same thing that i have physical features with mexico would be we got oceans and they have oceans and i we also got places of hot climates and i also believe we both have mountains i live in america too, and the differences of us and mexico would be the have hot climates all year round <span>The ancient Maya civilisation used the cenotes for rituals and burials. Just off the Caribbean coast is the island of Cozumel with brilliant coral reefs.</span>
Answer:with a boat or plane
Explanation:
Oceanic and continental plates are colliding.
Explanation:
On the image, we can see an oceanic plate on the left, and a continental plate on the right, moving toward each other and colliding. Because the two plates have different densities, thickness, and elevation, one of the subducts below the other, that being the oceanic plate. As the oceanic plate subducts below the continental plate, it gradually moves down in the mantle layer, getting melted, recycled, and maybe the same material be pushed toward the surface again.
On the plate boundary, convergent in this case, there is intense geological activity. Magma manages to rise through the cracks and gaps, and it forms volcanoes, creating a continental volcanic arc. Also, there are lot of earthquakes at such boundaries, as there is constant adjustment of the crust.
Such boundaries can be found between the:
- Pacific and North American plates
- Pacific and Eurasian plates
- Pacific and Australian plates
- Pacific and Philippine plates
- Nazca and South American plates
- Cocos and North American plate
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Answer:
<em>Mantle convective current</em>
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Explanation:
The North American Plate is a tectonic plate that covers most of North America, Greenland, Cuba, the Bahamas, extreme northeastern Asia, and parts of Iceland and the Azores. It is Earth's second largest tectonic plate, behind the Pacific Plate. It is thought to be moved by the very slow creeping motion of Earth's solid silicate mantle caused by convection currents carrying heat from the interior to the planet's surface.
