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zimovet [89]
3 years ago
8

Hurry pls 1 min left!

Social Studies
1 answer:
mojhsa [17]3 years ago
7 0

Answer: The answer is D

Explanation:

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Following a systematic plan for the preparation of an e-mail, memo, letter, or oral presentation will make the composition proce
krok68 [10]

Answer:

Organizing, drafting, editing and proofreading (in this sequence)

Explanation:

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4 years ago
“How many soccer players left the field?” Is an example of a(n) ______ question.
jenyasd209 [6]
B.out of left field so the answer is b I think good luck
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3 years ago
identify three surface process that are part of the rock cycle. Explain the role of each process in the cycle.
Galina-37 [17]

Answer:

PLEASE MARK ME BRAINLIEST!!!!!!!

Explanation:

There are three main types of rocks: sedimentary, igneous, and metamorphic. Each of these rocks are formed by physical changes—such as melting, cooling, eroding, compacting, or deforming—that are part of the rock cycle.

Sedimentary Rocks

Sedimentary rocks are formed from pieces of other existing rock or organic material. There are three different types of sedimentary rocks: clastic, organic (biological), and chemical. Clastic sedimentary rocks, like sandstone, form from clasts, or pieces of other rock. Organic sedimentary rocks, like coal, form from hard, biological materials like plants, shells, and bones that are compressed into rock.

The formation of clastic and organic rocks begins with the weathering, or breaking down, of the exposed rock into small fragments. Through the process of erosion, these fragments are removed from their source and transported by wind, water, ice, or biological activity to a new location. Once the sediment settles somewhere, and enough of it collects, the lowest layers become compacted so tightly that they form solid rock.

Chemical sedimentary rocks, like limestone, halite, and flint, form from chemical precipitation. A chemical precipitate is a chemical compound—for instance, calcium carbonate, salt, and silica—that forms when the solution it is dissolved in, usually water, evaporates and leaves the compound behind. This occurs as water travels through Earth’s crust, weathering the rock and dissolving some of its minerals, transporting it elsewhere. These dissolved minerals are precipitated when the water evaporates.

Metamorphic Rocks

Metamorphic rocks are rocks that have been changed from their original form by immense heat or pressure. Metamorphic rocks have two classes: foliated and nonfoliated. When a rock with flat or elongated minerals is put under immense pressure, the minerals line up in layers, creating foliation. Foliation is the aligning of elongated or platy minerals, like hornblende or mica, perpendicular to the direction of pressure that is applied. An example of this transformation can be seen with granite, an igneous rock. Granite contains long and platy minerals that are not initially aligned, but when enough pressure is added, those minerals shift to all point in the same direction while getting squeezed into flat sheets. When granite undergoes this process, like at a tectonic plate boundary, it turns into gneiss (pronounced “nice”).

Nonfoliated rocks are formed the same way, but they do not contain the minerals that tend to line up under pressure and thus do not have the layered appearance of foliated rocks. Sedimentary rocks like bituminous coal, limestone, and sandstone, given enough heat and pressure, can turn into nonfoliated metamorphic rocks like anthracite coal, marble, and quartzite. Nonfoliated rocks can also form by metamorphism, which happens when magma comes in contact with the surrounding rock.

Igneous Rocks

Igneous rocks (derived from the Latin word for fire) are formed when molten hot material cools and solidifies. Igneous rocks can also be made a couple of different ways. When they are formed inside of the earth, they are called intrusive, or plutonic, igneous rocks. If they are formed outside or on top of Earth’s crust, they are called extrusive, or volcanic, igneous rocks.

Granite and diorite are examples of common intrusive rocks. They have a coarse texture with large mineral grains, indicating that they spent thousands or millions of years cooling down inside the earth, a time course that allowed large mineral crystals to grow.

Alternatively, rocks like basalt and obsidian have very small grains and a relatively fine texture. This happens because when magma erupts into lava, it cools more quickly than it would if it stayed inside the earth, giving crystals less time to form. Obsidian cools into volcanic glass so quickly when ejected that the grains are impossible to see with the naked eye.

Extrusive igneous rocks can also have a vesicular, or “holey” texture. This happens when the ejected magma still has gases inside of it so when it cools, the gas bubbles are trapped and end up giving the rock a bubbly texture. An example of this would be pumice.

 

5 0
3 years ago
At the tactical level, rules of engagement (roe) are tied to the _____.
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ROE stands for Rules of Engagement. Those are military directives meant to describe the circumstances under which ground, naval, and air forces <span>will initiate and/or continue combat </span>engagement.<span>
At the tactical level, rules of engagement (ROE) are tied to the mission profile.</span>The ROE are tailored to the specific mandate of the mission and the situation on the ground.

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3 years ago
Read 2 more answers
If you can make your own state what would be the geographic distribution of power with your government?
shtirl [24]

Answer:In addition to the type, or form of government

that exists in a society, there are other factors

that play a role in the overall function of a

government, including the geographic

distribution of power, and the relationship

between the legislative and executive branch.

Geographic Distribution of Power

In every system of government the power to

govern is located in one or more places

geographically. From this standpoint, three

basic structures exist: unitary, federal, and

confederate.

Unitary Government

A unitary government is often described as a

centralized government. All powers held by the

government belong to a single, central agency.

The central (national) government creates local

units of government for its convenience. Those

local governments have only those powers that

the central government chooses to give them.

Most governments in the word are unitary in

form. Great Britain is a classic example. It has a

single central organization, the Parliament,

holding all of the government’s power. Local

governments exist solely to relieve Parliament

of the tasks that would be difficult or

burdensome to do. Though unlikely, Parliament

could get rid of those agencies of local

government at any time if it wanted to.

Be careful not to confuse a unitary government

with a dictatorship. In the unitary government

all forms of power are held by the central

government, but that government can still

elected by the people, and if so, would only

have the powers that the people allowed it to

have. So, a government could be both unitary

and democratic.

Federal Government

A federal government is one in which the

powers of government are divided between a

central government and several local

governments. An authority superior to both the

central and local governments make this

division of powers on a geographic basis, which

cannot be changed by either the local or

national level alone. Both levels of government

act directly on the behalf of the people through

their own sets of laws, officials, and agencies.

In the United States, for example, the Federal

Government has certain powers, and the 50

individual states have others. This division of

powers is set out in the Constitution. The

Constitution stands above both levels of

government and cannot be changed unless the

people agree to that change.

Australia, Switzerland, Canada, Mexico,

Germany, India, and some 20 other stats also

have federal forms of government today. In the

United States, the term ‘Federal Government’ is

often used to refer to the National Government,

but note that the 50 state governments are

unitary in structure, not federal.

Confederate Government

A confederation is an alliance of independent

states. A central organization, the confederate

government, only handles those matters that

the state assigns to it. Typically, confederate

governments hold limited powers in such fields

as defense and foreign commerce.

Most often, the confederacy has not had the

power to make laws that apply directly to

individuals, at least not without some further

action by the member states. A confederate

structure makes it possible for the several

states to cooperate in matters of common

concern and also retain their separate

identities.

Confederations are very rare in today’s world.

The Confederate States of America (1861-1865)

are one example in past times. A possible

modern example is the European Union (EU),

which is an assembly of 28 nations, mostly in

Europe. Through its institutions, the EU has

established free trade among its members,

launched a common currency (the Euro), and

coordinates the foreign trade and defense

policies of its members. Recently in news,

United Kingdom voted to remove itself, or exit,

from the EU for more independence, a situation which was often referred to as “Brexit”.

Explanation:

4 0
3 years ago
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