Answer:
Following WWI, the Treaty of Versailles screwed Germany by forbidding them from having an army, taking away part of their country, and making them accountable for all war costs. Germany was deeply in debt, and inflation was out of control. People were agitated, and the scene became chaotic. Hitler reasoned that by using propaganda to make the Jews appear as the adversary and as nasty, wicked humans, he could play on the fear of the German population and other (used as a verb) the Jews, and since the Germans were so eager for a solution, they couldn't see where it was going.
I hope this information is useful.
Explanation:
Answer:
the answer is d
Explanation:
landslides are just rock and dirt falling after being disturbed, and a landslide disturbs it causing it to fall
Answer:
The tectonic plates are continuously moving and earthquakes are happening all the time.
Explanation:
An earthquake is the seismic waves travelling through the lithosphere. They occur along tectonic plate boundaries and faults. In areas that are far from these plate boundaries and faults, earthquakes are less likely to be felt. The size of the earthquake is mostly unnoticeable. Bigger earthquakes happen with a build of tension that is suddenly released. It does not happen as often because it takes time to build up the pressure.
Answer:
<u>e. All convergent plate boundaries are subduction zones</u>
Explanation:
- It's well known that any place either on land or ocean when is subdued into the earth's mantle is formed by a subduction zone where the plate boundaries collide either oceanic or continental boundaries this collision can result from the earthquake and volcanic eruptions.
- These collisions thus lead to the creation of mountains and volcanoes at greater altitudes as the place gets elevated and as a result of the slab push and pull as many earthquakes generally occur in this shallow zone also named as the Benioff zone.
- Plates dip here at an angle of 45 degrees and thus form these internal subduction zones that lead to lithospheric density differentiation
