Question

If two continental plates slide past each other at a transform boundary, then_____ may occur.

A. earthquakes
B. faults
C. ocean formation
D. mountains
E. volcanoes
F. island chains
G. seafloor spreading

Answer 1

When oceanic or continental plates slide past each other in opposite directions, or move in the same direction but at different speeds, a transform fault boundary is formed. No new crust is created or subducted, and no volcanoes form, but earthquakes occur along the fault. The transform fault boundaries connect spreading centers and subduction zones, which are the other elements of the jigsaw puzzle of the Earth’s plates.

Answer 2

If two continental plates slide past each other at a transform boundary, then (A)earthquakes may occur.

Explanation:

• Plate borders are significant because earthquakes and volcanoes are frequently associated with them.

• Huge amounts of energy can be unleashed in the form of earthquakes when the Earth's tectonic plates grind against one another.

• Because molten rock from deep below the Earth, known as magma, can move upward at these plate intersections, volcanoes are frequently found near plate boundaries.

• Plate borders come in a variety of shapes and sizes.

• Plate boundaries, for example, can converge and collide (a "convergent" plate boundary), split apart (a "divergent" plate boundary), or slide past each other (a "transform" plate border).

• Different geological features are linked with each of these types of plate borders.

• As Earth's crust is crushed and pushed upward, convergent plate boundaries, such as the one between the Indian Plate and the Eurasian Plate, generate towering mountain ranges like the Himalaya.

• A convergent plate boundary, on the other hand, can sometimes result in one tectonic plate sinking beneath another.

• An older, thicker tectonic plate is forced deep into the planet beneath a younger, less dense tectonic plate in a process known as "subduction"." A trench">ocean trench can emerge when this process occurs in the ocean.

• These trenches are among the deepest in the water, and they are frequently the epicenter of powerful earthquakes.

• A transform fault boundary is generated when oceanic or continental plates slide past one other in opposite directions, or move in the same direction but at different rates.

• Although no new crust is formed or subducted, nor are volcanoes formed, earthquakes do occur along the fault. Spreading canters and subduction zones, which are the other pieces of the Earth's plate jigsaw puzzle, are connected by transform fault boundaries.