<u>Answer:</u>
<em>Glacial deposits found where glaciers no longer exist
</em>
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<u>Explanation:</u>
Scientists found the fossils of numerous indistinguishable showing up species on generally isolated main lands. They had two hypotheses for this. Initially, they conjectured that different species grew indistinguishably over the distant, a profoundly improbable idea. The subsequent theory was that the landmasses had been in contact with one another a large number of years prior, and had by one way or another, floated separated.
These landmasses were in contact at some point previously, enabling species to wander unreservedly, bite the dust, be covered, and become fossilized over these central lands.
Answer: The release of methane from thawed permafrost
Explanation:
With increasing global warming, permafrost in the arctic is melting. The carbon and methyl clathrates present in permafrost escape into the atmosphere to form carbon dioxide and methane, both greenhouse gases.
In the Arctic, molecules of methane are trapped in ice crystals as methyl clathrates. When the temperature increases, these crystals release methyl clathrates which become methane when in contact with the atmosphere.
The cause of the increasing atmospheric 
is due to the the thawing of dead organisms present in the permafrost. As the permafrost melts, these organisms decay and release into the atmosphere.
For earthquakes, there is a lapsed time between the arrival of the
p-wave and the s-wave, because the waves travel at different speeds. The length
of this period of time determine the
distance to the epicenter.
Earthquakes create seismic waves. P waves are faster than S
waves. As the P and S waves move out from an earthquake, the P waves get ahead
of the S waves. The distance of a seismic station from an earthquake can be
determined from the time difference between the time of arrival of the first P
wave and the first S wave.
Energy because it will make things live way more
