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bearhunter [10]
3 years ago
6

What is erosion? How is erosion different than weathering? What are the different types of water erosion? What factors contribut

e to the rate of water erosion? How are different climates affected by water erosion What are the short-term effects on the land? (Flooding, costal dune erosion, etc.) What are the long-term effects? (Desertification, loss of habitats, poor soil quality, etc.) How does water erosion affect humans? What are the short-term effects to humans? (Property damage, contaminated water, damage to crops, etc.) What are the long-term effects to humans? (Health issues, transportation difficulties, etc.) How can humans affect the rate of water erosion?
Geography
2 answers:
erica [24]3 years ago
5 0

Answer:

1. Is a natural process of the minerals and things inside of rock but is not being destroyed, rather moved.

2. Weathering breaks down the material while erosion just moves it.

3. Gully,rill, and sheet

4. Climatic characteristics( rainfall,wind and atmosphere"temp")

5. They're effected by temp and perspiration(rain) there will be more flooding for a mid temp and rainy area, a dry and hot area will have more rocky areas.

6. Wet areas will erode away and have less land to use while the dry areas will have low nutrients dirt and more rocks than actual dirt.

7. It makes soil lose nutrients and cause tons of farmland to lose a good quality of use.

8. Farmland won't produce as much because there's nothing to fuel the plant growth.

9. Farmers and humans will need to move around more/tear down more natural land to find suitable soil or else there will be famine all over.

10. Since farmers have to move massive amounts of soil in order to fertilize the land, it can cause erosion from the wind rain etc. causing land to fail because mudslides etc. Famine would start to set in because there would be no more suitable land for farmers because they'd move around and destroy the land to where it's unusable.

Explanation: I went in and edited the answer above mine so I could spare you the trouble of editing. Have a great day :)

BARSIC [14]3 years ago
3 0

#1 is a natural process of the minerals and things in rock is not destroyed but rather moved.

#2 weathering breaks down the material while erosion just moves it.

#3 <em><u>gully,rill, and sheet</u></em>

#4 climatic characteristics( rainfall,wind and atmosphere"temp")

#5 they are effected bye temp ans perspiration(rain) there will be more flooding for a mid temp and rainy area while a dry and hot area will have more rocky areas

#6 wet areas will erode away and have less land to use and the dry areas will have nutrient low sand and more rocks then actual dirt

#7 it makes the soil loose the nutrient s and casue tons fo farmland to loose a good quality of use.

#8 farm land wont produce as much cause there is nothing to fuel the plant growth.

#9 farmers and humans will need to move around more and tear down more natural land to find suitable soil or else there will be famine all over

#10 since farmers have to till massive amounts of tops soil in order to be able to use the land it cause erosion from the wind rain etc. causing land to fail cause mudslides etc. then famine start setting in cause there would be now more suitable land for farming cause farmers would move around and use up all the land.


i hope these are right if one is wrong then put in comments

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raketka [301]

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3 years ago
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Identify three ways boundaries are created and provide a specific example of each one
AleksandrR [38]
<span>There are three kinds of plate tectonic boundaries: divergent, convergent, and transform plate boundaries.
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A divergent boundary occurs when two tectonic plates move away from each other. Along these boundaries, lava spews from long fissures and geysers spurt superheated water. Frequent earthquakes strike along the rift. Beneath the rift, magma—molten rock—rises from the mantle. It oozes up into the gap and hardens into solid rock, forming new crust on the torn edges of the plates. Magma from the mantle solidifies into basalt, a dark, dense rock that underlies the ocean floor. Thus at divergent boundaries, oceanic crust, made of basalt, is created.

When two plates come together, it is known as a convergent boundary. The impact of the two colliding plates buckles the edge of one or both plates up into a rugged mountain range, and sometimes bends the other down into a deep seafloor trench. A chain of volcanoes often forms parallel to the boundary, to the mountain range, and to the trench. Powerful earthquakes shake a wide area on both sides of the boundary.

If one of the colliding plates is topped with oceanic crust, it is forced down into the mantle where it begins to melt. Magma rises into and through the other plate, solidifying into new crust. Magma formed from melting plates solidifies into granite, a light colored, low-density rock that makes up the continents. Thus at convergent boundaries, continental crust, made of granite, is created, and oceanic crust is destroyed.

Two plates sliding past each other forms a transform plate boundary. Natural or human-made structures that cross a transform boundary are offset—split into pieces and carried in opposite directions. Rocks that line the boundary are pulverized as the plates grind along, creating a linear fault valley or undersea canyon. As the plates alternately jam and jump against each other, earthquakes rattle through a wide boundary zone. In contrast to convergent and divergent boundaries, no magma is formed. Thus, crust is cracked and broken at transform margins, but is not created or destroyed.

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On Christmas Day 1991, Soviet President Mikhail Gorbachev shocked the world with these words, announcing the dissolution of the Soviet Union and his resignation from its top post. After more than 40 years of the world seeming to teeter on the brink of a nuclear holocaust, the Cold War between the Soviet Union and the United States had ended.

What had been the world’s largest communist state—and the counterweight to the United States—broke into 15 independent republics, making America the sole global superpower. And although at its peak the Soviet Union had more than 5 million soldiers stationed internationally and enough nuclear power to destroy the human race, members of the Soviet high command abdicated power without a shot being fired.

Soviet President Mikhail Gorbachev on the second day of the extraordinary session of the Supreme Soviet in Moscow on August 27, 1991. He threatened to resign if the republics refused to sign a Union Treaty to hold the Soviet Union together. (Credit: Vitaly Armand/AFP/Getty Images)

Soviet President Mikhail Gorbachev on the second day of the extraordinary session of the Supreme Soviet in Moscow on August 27, 1991. He threatened to resign if the republics refused to sign a Union Treaty to hold the Soviet Union together. (Credit: Vitaly Armand/AFP/Getty Images)

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When he became president of the Soviet Union in 1985, Gorbachev inherited both a moribund economy and a crumbling political system. Many historians believe that the two policies he put in place to address the nation’s challenges, glasnost (“openness”) and perestroika (“restructuring”), hastened the dissolution of the Soviet system, which was already in decline.

Glasnost, begun in the late ’80s, was a push for transparency in governance. It curbed state censorship, allowing Soviet media to report painful, long-covered-up truths—such as the fact that alcoholism and infant mortality were rising, life expectancy at birth was declining and standards of living in the West were outpacing those in the USSR. It also allowed non-Communist parties to take part in elections.

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The measures were met first with enthusiasm: When a McDonalds restaurant opened in the nation’s capital in January 1990, Muscovites marveled at “three-story sandwiches” and smiling fast-food cashiers. But when the growing pains of perestroika led to a new wave of shortages and economic hardship, newly empowered regional leaders of the non-Russian Union Republics, such as Lithuania and Ukraine, used their freshly opened political process to demand autonomy from the Kremlin, ultimately leading to the USSR’s demise.

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Explanation:

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