The large-scale movement of waters in the basins of the ocean is known as ocean circulation. The wind mediates surface circulation and the sinking and cooling of water in the Polar Regions mediate deep circulation. The conduction of warm upper waters towards the poles from the tropic is done by surface circulation.
1. In the given question, if large amounts of water are supplemented in the Polar Regions as glaciers melt then the warm water will exhibit a more difficult time in flowing towards north.
2. The effect it could impart in the area is that the local temperature would increase more.
Answer:
Non-foliated rocks have grains that are arranged randomly, and grains that do not split into layers.
Explanation:
I'm not sure what the question was asking, but I just gave phrases that described non-foliated rocks. I hope that helps?
Answer:
sounds good , but I don't get you
Because we learn over time how things work and how they don't work.
Two examples include Cyanobacteria streptococci. Prokaryotes don’t really create systems into higher orders of living things so they create chains like the two I mentioned
