Answer:
(A) True
Explanation:
The Cascadia subduction zone is 1,100 kilometers long, and its characteristics of youthful oceanic plate and strong coupling with the overriding plate are similar to situations in southwestern Japan and southern Chile where very large earthquakes have occurred. The Cascadia subduction zone is a convergent plate boundary that stretches from Northern Vancouver Island to Cape Mendocino California, It results from the subduction of the Juan de Fuca Plate beneath the North American plate. The Cascadia subduction zone is stable with no significant seismic activity.
Western Europe is more developed than Eastern Europe because <u>the market economy of Western Europe provides an economic advantage</u>
Explanation:
Stark differences persist between the western and eastern part of Europe. While western Europe was under the influence of Capitalism mode of production (led by the US and Great Britain), the eastern part was led by the erstwhile USSR following socialist mode of production.
Under the market economy, open competition and adaptive hand-holding by the US, western European countries prospered by leaps and bound. Marshall plan prepared by the US helped in post-war reconstruction of western Europe. On the other hand, eastern countries fell prey to the despotic rule of dictators, political instability and socialisation of assets. There were no such private assets and the important assets were nationalised. In the long run, the socialistic model of the market could not stand up to capitalism and fell in 1991 when the USSR disintegrated.
There are many people in urban areas. If there are floods, it could kill a lot of people. Also, floods sometimes damage buildings. If the buildings collapse, it would cause a big problem.
Acid rain from Los Angeles changed the chemistry of the river, resulting in the death of many fish.Due to human activities in Los Angeles, pollution is not anymore shocking. The acid rain would be distributed to the river which would change the environment of the aquatic life.
