How did humans modify the enviorment by industry and agriculture

1 answer:

4 0

They modified it buy cutting down trees and building factories and buildings in order to grow plants and fruits more effectively in a more precise inviorment!

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Question 5 1 pts Cementation is an important part of the diagenetic process. From the list of minerals below, pick two minerals

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The two minerals that are found in cement are : Silica and calcite.

Explanation:

Different minerals form the composition of cement but the minerals that are most commonly found in cement are calcite which is contained in the limestone.

The other mineral that is used in the production of cement is silica in the form of raw rock type used to make cement which is found in clay. So they form an important part of formation of cement.

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The advantage of a globe is

Ostrovityanka [42]

Answer:

it lets you visually see where a place is exactly instead of on a piece of paper and you can see the whole world at once and keep a mental image

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Use the following stimulus to answer the next question

AVprozaik [17]

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I don't understand your question may be questioned mistakes

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What are the three main sources of income for cuba?

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C. tobacco tourism and sugar

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What is bowens reaction series

lesya692 [45]

Answer:

The ranking of common igneous silicate minerals based on the temperature at which crystallization occurs is called Bowen’s reaction series.

Explanation:

In Bowen’s reaction series the minerals with high crystallization temperature are present at the top layer. This means these minerals are the first to crystallize from the magma and they are mostly unstable. The Bowen's reaction series is represented in the Y shape. The left branch of this Y has minerals containing iron and magnesium. They are called as Ferromagnesium minerals.

The right branch of the Y contains plagioclase feldspars minerals. Temperature gradually decreases down along the Bowen’s reaction series from $1200^{\circ} \mathrm{C}$ to $700^{\circ} \mathrm{C}$ . At certain low temperature, the two branches combine forming minerals similar to felsic rocks such as orthoclase feldspar, quartz and muscovite mica.

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