True
Explanation:
Rock records through time indicates that there were many more volcanic eruptions in the early history of the earth than we have today.
In fact, the earth is experiencing quite a low level of volcanism compared to the time it originally formed.
- Volcanic eruption is the movement of magma from within the earth to the surface where they can cool and become solidified.
- Most of the volcanoes we have today are inactive to dormant. Just a few volcanoes are still active.
- Most of them were even formed several millions of years.
- Little to no new volcanoes are being formed today.
- When the earth originally formed, series of volcanic activities punctuated the surface.
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I think that’s how you write a hypothesis correctly
Answer:
Explanation:
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By weakening and fracturing rock, weathering processes release nutrients and improve subsurface permeability. It is helpful to limit the physical attributes of materials produced by weathering inside the crucial zone in order to better understand these processes.
The permeability, strength, and seismic anisotropy of foliated rocks can be measured geophysically, whereas the first two have effects on hydrology and geomorphology. Characterizing weathering-dependent changes in rock fabric with depth may have a variety of implications because each of these types of anisotropy is connected to rock fabric.
The key points are:
- In the critical zone, seismic surveys of weathered material reveal seismic anisotropy magnitudes that can reach 36% and that change with depth.
- The strike of foliation and fracture planes found in bedrock coincides with the fast direction of wave propagation in weathered materials.
- As bedrock is exhumed toward the surface, in-situ weathering processes probably intensify the anisotropy already existing in the rock.
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Mindanao is the other main island of the Philippines. Borneo contains Indonesia, Malaysia and Brunei, Spratly is claimed by several South East Asian Countries and Irian Jaya is an island of Indonesia