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Q: _____ waves cannot pass through ____ substances. Mapping the locations where these and other waves transmitted following an earthquake allows for the determining the layers of the _____, as well as
the epicenter of an earthquake. (Points : 3) P / solid / earth S / liquid / earth P / solid / atmosphere S / liquid / atmosphere
A: The answer is P / solid / atmosphere. Ask again!
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User: _____ waves cannot pass through ____ substances. Mapping the locations where these and other waves transmitted following an earthquake allows for the determining the layers of the _____, as well as the epicenter of an earthquake. (Points : 3) P / solid / earth S / liquid / earth P / solid / atmosphere S / liquid / atmosphere

Weegy: The answer is P / solid / atmosphere. Ask again!
rpatricia|Points 40|

User: Which of the following forms of evidence was used to formulate Wegener's theory of Continental Drift

User: Which of the following forms of evidence was used to formulate Wegener's theory of Continental Drift? (Points : 3) the jigsaw-like pattern of continental coastlines magnetism of the ocean basin rocks discovery of the Mid-Atlantic Ridge radiometric dating of the basaltic rocks

Weegy: Evidence for the movement of continents on tectonic plates is now extensive. Similar plant and animal fossils are found around different continent shores, suggesting that they were once joined. [ The fossils of Mesosaurus, a freshwater reptile rather like a small crocodile, found both in Brazil and South Africa, are one example; another is the discovery of fossils of the land reptile Lystrosaurus from rocks of the same age from locations in South America, Africa, and Antarctica.[21] There is also living evidence?the same animals being found on two continents. Some earthworm families (e.g.: Ocnerodrilidae, Acanthodrilidae, Octochaetidae) are found in South America and Africa, for instance. The complementary arrangement of the facing sides of South America and Africa is obvious, but is a temporary coincidence. In millions of years, slab pull and ridge-push, and other forces of tectonophysics will further separate and rotate those two continents. It was this temporary feature which inspired Wegener to study what he defined as continental drift, although he did not live to see his hypothesis become generally accepted. Widespread distribution of Permo-Carboniferous glacial sediments in South America, Africa, Madagascar, Arabia, India, Antarctica and Australia was one of the major pieces of evidence for the theory of continental drift. The continuity of glaciers, inferred from oriented glacial striations and deposits called tillites, suggested the existence of the supercontinent of Gondwana, which became a central element of the concept of continental drift. Striations indicated glacial flow away from the equator and toward the poles, in modern coordinates, and supported the idea that the southern continents had previously been in dramatically different locations, as well as contiguous with each other.[12] ]
miEr12|Points 70|

User: The following field of science studies the waves of movement in the crust of the Earth:

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Asked 12/25/2012 7:14:21 AM
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