Answer:
B. Europe
Explanation:
The establishment of the European Union after the sign of the Maastricht Treaty eliminate customs for goods, services and people withing a great portion of Europe since early 1990s.
Answer:
-The feature was most likely caused by one oceanic crust subducting under a leading edge of a continent.
-It is most likely a deep-ocean trench because they are common along the margins of the Pacific Ocean.
-It is most likely a deep-ocean trench because they are common along the active continental margins.
Explanation:
Subduction is a geological process that leads to the creation of several geological features. It usually occurs when there is a movement of one plate against another plate that is caused by a high potential energy. This kind of geological processes usually occurs at regions known as subduction zones which has the highest crash events all over the world.
Answer:
Slumping is the process that has a big influence on the river channel, as it can change its flow and volume.
Explanation:
Slumping happens when the erosion moved the bottom of the valley. This is the ground moving towards down when the rocks and mass of ground are moving downhill. This process influences the river, as the rock is, for example moving down, and the water runs into the rock, the water will go around the rock and that way change the flow.
Explanation:
impacts them greatly. We wouldn’t even have tropical cyclones if it weren’t for the Coriolis Effect.
Tropical cyclones begin as masses of disorganized showers and storms in/near the Tropics. As wind speeds pick up in these shower/storm masses, a circulation begins to form. The circulation only forms because of the Coriolis Effect, which causes cyclones to spin counterclockwise in the Northern Hemisphere (and clockwise in the Southern).
As the system matures, winds around its central eye strengthen. Rain becomes more intense. If the storm makes landfall, you might hear a TV meteorologist warn viewers about the “northeastern quadrant” or the “eastern side” of the storm.
This is because the Coriolis force adds momentum and energy to that side of the storm. On the east side of a low pressure system (in the Northern Hemisphere), your wind (which is caused by the pressure gradient force, or differences in air pressure) will be helped along by the Coriolis force. On the west side, the Coriolis force acts against the wind.
Thus, the Coriolis effect ensures that the worst part of most tropical cyclones is the east side, and particularly the northeastern quadrant. This is where the worst winds and heaviest rain will be located.
