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miskamm [114]
3 years ago
9

Select all that apply.

History
1 answer:
djyliett [7]3 years ago
6 0

c juries is the answer!


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Objective: Examine the different strategies to achieve civil rights in the 1950’s and 1960’s. (PLEASE help me with this, thank y
sineoko [7]

Answer:

There were essentialy three strategies

  • Judicial strategies: this consists in suing a school, person, institution, or even state, on the basis that a civil right was violated. These kind of cases often led to landmark decisions by the U.S. Supreme Court such as Brown v. Board of Education.
  • Civil protests: This were peaceful protests, mostly led by students in the South, who demanded for civil rights such as the right of black people to enter any college that they wished.

Intellectual discusion: intellectuals like Martin Luther King, and decades before, W. Du Bois, wrote articles and books, and gave speeches where they gave arguments that supported civil rights for everyone.

7 0
3 years ago
In the early 1920s, Lenin established the New Economic Policy, which
ad-work [718]

The policy of War Communism was in effect since 1918. New Economic Policy(NEP) was the policy introduced from 1921 to 1928. The measure of this new policy were in the favor of most agriculture, retail trade and small scale of industry in the cities. Foreign trade was also introduced by the people who were then called as NEP Men. It result in huge change in economy while communists were happy and held their power by it.

7 0
3 years ago
Iready question:
spayn [35]

Answer: best taught in the home, free time

Explanation: I got them both right when I took the Iready quiz. Hope this helps you!! Best of luck.

3 0
3 years ago
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Ottoman empire ended as a result of boxer rebellion
ozzi
"Hurricane" redirects here. For other uses, see Hurricane (disambiguation).<span>For technical reasons, "Hurricane #1" redirects here. For the band, see Hurricane No. 1.</span>Hurricane Isabel (2003) as seen from orbit during Expedition 7 of the International Space Station. The eye, eyewall, and surrounding rainbands, characteristics of tropical cyclones in the narrow sense, are clearly visible in this view from space.<span><span>Part of the nature series</span>WeatherCalendar seasons<span>WinterSpringSummerAutumn</span>Tropical seasons<span>Dry seasonWet season</span>Storms<span>BlizzardCloudDownburstDust stormExtratropical cycloneFirestormIce stormLightningSupercell<span>Thunderstorm (Thundersnow)</span>TornadoTropical cyclone (Hurricane)WaterspoutWinter storm</span>Precipitation<span><span>Drizzle (Freezing drizzle)</span>GraupelHail<span>Ice pellets (Diamond dust)</span><span>Rain (Freezing rain)</span><span>Snow <span>Rain and snow mixedSnow grainsSnow rollerSlush</span></span></span>Topics<span>Atmospheric riverAir pollutionClimateCloudCold waveFogHeat waveJet streamMeteorologySevere weatherWeather forecasting</span><span> Weather portal</span><span>vte</span></span>

A tropical cyclone is a rapidly rotating storm system characterized by a low-pressure center, a closed low-level atmospheric circulation, strong winds, and a spiral arrangement of thunderstorms that produce heavy rain. Depending on its location and strength, a tropical cyclone is referred to by names such as hurricane (<span>/<span>ˈhʌrᵻkən</span>/</span> or <span>/<span>ˈhʌrᵻkeɪn</span>/</span>[1][2][3]), typhoon <span>/<span>taɪˈfuːn</span>/</span>, tropical storm, cyclonic storm, tropical depression, and simply cyclone.[4] A hurricane is a storm that occurs in the Atlantic Ocean and northeastern Pacific Ocean, a typhoon occurs in the northwestern Pacific Ocean, and a cyclone occurs in the south Pacific or Indian Ocean.[4]

Tropical cyclones typically form over large bodies of relatively warm water. They derive their energy through the evaporation of water from the ocean surface, which ultimately recondenses into clouds and rain when moist air rises and cools to saturation. This energy source differs from that of mid-latitude cyclonic storms, such as nor'easters and European windstorms, which are fueled primarily by horizontal temperature contrasts. The strong rotating winds of a tropical cyclone are a result of the conservation of angular momentum imparted by the Earth's rotation as air flows inwards toward the axis of rotation. As a result, they rarely form within 5° of the equator.[5] Tropical cyclones are typically between 100 and 2,000 km (62 and 1,243 mi) in diameter.

Tropical refers to the geographical origin of these systems, which form almost exclusively over tropical seas. Cyclone refers to their cyclonic nature, with wind blowing counterclockwise in the Northern Hemisphere and clockwise in the Southern Hemisphere. The opposite direction of circulation is due to the Coriolis effect.

In addition to strong winds and rain, tropical cyclones are capable of generating high waves, damaging storm surge, and tornadoes. They typically weaken rapidly over land where they are cut off from their primary energy source. For this reason, coastal regions are particularly vulnerable to damage from a tropical cyclone as compared to inland regions. Heavy rains, however, can cause significant flooding inland, and storm surges can produce extensive coastal flooding up to 40 kilometres (25 mi) from the coastline. Though their effects on human populations are often devastating, tropical cyclones can relieve drought conditions. They also carry heat energy away from the tropics and transport it toward temperate latitudes, which may play an important role in modulating regional and global climate.

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Contents <span> [hide] </span><span><span><span>1Physical structure</span><span><span>1.1Wind field</span><span>1.2Eye and center</span><span>1.3Size</span></span></span><span><span>2Physics and energetics</span><span><span>2.1Secondary circulation: a Carnot heat engine</span><span>2.2Primary circulation: rotating winds</span><span><span>2.3Maximum potential intensity</span><span><span>2.3.1Derivation</span><span>2.3.2Characteristic values and variability on Earth</span></span></span><span>2.4Interaction with the upper ocean</span></span></span><span>3Major basins and related warning centers</span><span><span>4Formation</span><span><span>4.1Times</span><span>4.2Factors</span><span>4.3Locations</span></span></span><span><span>5Movement</span><span><span>5.1Environmental steering</span><span>5.2Beta drift</span><span>5.3Multiple storm interaction</span><span>5.4Interaction with the mid-latitude westerlies</span><span>5.5Landfall</span></span></span><span><span>6Dissipation</span><span><span>6.1Factors</span><span>6.2Artificial dissipation</span></span></span><span>7Effects</span><span><span>8Observation and forecasting</span><span><span>8.1Observation</span><span>8.2Forecasting</span></span></span><span><span>9Classifications, terminology, and naming</span><span><span><span>9.1Intensity classifications</span><span><span>9.1.1Tropical depression</span><span>9.1.2Tropical storm</span><span>9.1.3Hurricane or typhoon</span></span></span><span>9.2Origin of storm terms</span><span>9.3Naming</span></span></span><span>10Notable tropical cyclones</span><span>11Changes caused by El Niño-Southern Oscillation</span><span>12Long-term activity trends</span><span>13Global warming</span><span>14Related cyclone types</span><span>15In popular culture</span><span>16See also</span><span>17References</span><span>18<span>External links

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7 0
3 years ago
What us foreign policy did Bush promise to enforce?
LuckyWell [14K]
President Bush laid out a few principles of what is known as the "Bush Doctrine" as it relates to foreign policy. The first principle was that the American people should not distinguish between terrorists and the nations in which they live; both should be held accountable. Bush also supported taking the fight to the enemy before they could attack first. He also believed in confronting what he deemed as threats before they were actually made. Finally, Bush believed in advancing "liberty and hope" in reaction against the enemy's beliefs of fear and repression. 
8 0
3 years ago
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