Answer:
It is evident from the distinct magnetite orientation that these two rocks came from the mid ocean ridges.
If the rocks were obtained at the same time, sample A which is the rock with wider band of distinct magnetite orientation (2m) must be from the Easy Pacific Rise and the rock sample B with the shorter band of distinct magnetite orientation (1m) is from the Mid-Atlantic Ridge.
Explanation:
The Mid-Atlantic Ridge is a slow spreading center (leading to broader bands of magnetite orientation). It spreads 2-5 centimeters (0.8-2 inches) every year and forms an ocean trench about the size of the Grand Canyon.
The East Pacific Rise, on the other hand, is a fast spreading center (wide band of distinct magnetite orientation). It spreads about 6-16 centimeters (3-6 inches) every year. There is not an ocean trench at the East Pacific Rise, because the seafloor spreading is too rapid for one to develop!
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Answer: (conduction), liquids and gases (convection), and electromagnetical waves (radiation).
Explanation:
<u>Answer:</u>
The climate in Eastern Europe is to blame for why there is not as much agriculture in Eastern Europe as can be found in Western Europe.
<u>Explanation:</u>
- Most of the western European countries are neighbored by the Atlantic Ocean. This makes the climatic conditions in Western Europe comparatively more favorable for agriculture than in Eastern Europe.
- The climate in Eastern Europe is characterized by prolonged and severe winters. Thus, not much agriculture is possible in Eastern Europe.
A line joining places of equal pressure on the sypnotic wether map are called isobars
