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Anastasy [175]
3 years ago
5

3. Infer

Geography
1 answer:
Sever21 [200]3 years ago
6 0

Answer:

The Nazca plate is moving in a southwestern direction.

Explanation:

The Galapagos Islands are a chain of islands that have been formed by hot spot volcanism. This means that they are volcanic islands formed on top of a plate, not near the boundary of the plates. The hot spot is static, while the plates move, so as the plate moves one volcanic island away from the hot spot, a new one is formed.

The direction in which the islands are relative to each other is an excellent indicator of the direction in which the plate is moving. The smaller islands are the oldest ones, while the larger ones are the younger ones, so the direction in which the plate is moving is from the point of the largest island toward the smallest islands. In this case, we can see that if we make a line from the largest island toward the smallest islands the direction comes to be roughly in a southwestern manner.

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The Law of Superposition places the youngest rock on top of older rock, except when what two rock formations are present?
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Answer:

The Law of Superposition places the youngest rock on top of older rock, except when faults and igneous rock are present (option 1).

Explanation:

The law of superposition of strata -proposed by Nicolás Steno based on the observations of Avicenna- states that the rock strata observed in the earth's crust are the product of the deposit of rocks progressively over time, leaving the newest rocks in the surface and the oldest in lower strata.

In successive studies and observations made by Steno, this scientist could appreciate the existence of some exceptions to his principle of superposition:

  • <em>The presence of geological faults could cause an alteration in the arrangement of the layers, different from the order they should have. </em>
  • <em>Magma activity is a factor that would lead to the deposit of igneous rocks between the layers of already formed rocks.</em>

The Law of Superposition is, in geology, the basis on which the discipline of sedimentary stratigraphy is based.

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