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Sholpan [36]
3 years ago
15

Solve for the value of p. |(3p+1)° (p+7)

Geography
1 answer:
shutvik [7]3 years ago
4 0

Answer:

P=43

Explanation:

As, the both angles are linear, so if we add them, we will get 180°.

So, p+7 + 3p+1 = 4p + 8

So, 4p + 8 = 180

So, 4p = 180 - 8

4p = 172

P= 172/4

P = 43

So p+7 + 3p+7 = 43 + 7 + ( 3x43 + 1) = 180

Therefore, p = 43

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Explanation:

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3 years ago
Which concept best explains why most major religions have followers though the world?
Archy [21]
<span>d)cultural diffusion, because people mix and exchange ideas and beliefs. 
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7 0
3 years ago
The large-scale motions in the atmosphere show a convection cell (convective loop). The bold dark arrows show that air is rising
omeli [17]

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Explanation:

The weather conditions of the water and in the air during El Nino changes, while the air pressure is higher in the central pacific during normal conditions, it changes during El nino and is lower in the center of the pacific than to the west.

Due to these changes, trade winds get weaker and the flow of the water goes in the opposite direction, thereby sinking in the east.

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What do scientists call a region of Earth that contains an unusually large number of species that are threatened by habitat loss
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Answer:

These areas are called as Biological Hotspots

Explanation:

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7 0
3 years ago
Read 2 more answers
When sediments are first weathered from their source rock, they are ___________________________ and ___________________________
Ivan

Answer:

Eroded; poorly; abrasion; coarse-grained; well.

Explanation:

A rock cycle can be defined as a concept used to describe the continuous process that leads to a rock's creation, formation, transformation from one form to another, destruction and reformation over a specific period of time. The natural phenomenons that influences the rock cycle are weathering, plate tectonic activity, erosion, etc.

Basically, the three (3) main types of rocks are; igneous rock, sedimentary rock and metamorphic rock.

Weathering can be defined as the physical and chemical breakdown of rock into smaller pieces called sediment. Weathering can be classified into two categories namely;

I. Physical weathering : it is the process of breaking rocks into pieces without affecting its chemical composition e.g temperature, abrasion and frost action.

II. Chemical weathering : it is the process of breaking rocks into pieces by chemical action which leads to changes in its chemical composition e.g carbonation, hydration, plant acid and oxidation.

When sediments are first weathered from their source rock, they are eroded and poorly sorted. As they travel, they impact against each other or against bedrock, a process that abrasion off sharp corners and wears down the sediment size. Sediments that are finer, coarse-grained, rounded, and well sorted indicate that the sediments have traveled a long way from the source.

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3 years ago
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