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The following are the events in a story of how people have interacted with a landscape put into chronological order:
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1. Dense forest with large trees on steep hills: There were steep hills covered by forests made by large trees. The roots of these trees ceased soil erosion from happening.
2. Hand logging near lakes: People began to cut trees for wood but the pace was not as fact.
3. Mechanized logging throughout hills: Techniques of mechanized logging were developed and which helped in clearing the trees from over the hills within months.
4. Erosion fills lakes with silt: Clearing of forests from over the hills caused soil erosion and the silt from the hills flowed down with rainwater runoff.
The Battle of the Atlantic took place throughout the northern region of the Atlantic Ocean. Once the United States entered the war the battle spread all the way to the coast the United States and the Caribbean Sea. The battle lasted over 5 years and 8 months from September 3, 1939 to May 8, 1945. The control of the Atlantic had a major impact on the outcome of the war. Keeping Britain supplied helped to keep the Germans from taking over all of Western Europe. The losses in the battle were staggering. Over 30,000 sailors were killed on each side. The Allies lost around 3,500 supply ships and 175 warships. The Germans lost 783 submarines.
Fun Facts:
Winston Churchill first called it the "Battle of the Atlantic" in 1941.
It was estimated that at least 20 supply ships needed to arrive each day in Britain in order for them to continue to fight the war.
The Allies lost 1,664 supply ships in 1942.
The Germans sometimes used a "wolf pack" tactic where a number of submarines would surround and attack a supply convoy at once.
Allied planes used a large spotlight called the Leigh Light to spot submarines that had surfaced at night.
HOPES THIS HELPS YOU!!
CAN YOU MARK MINE AS BRAINLIEST??
Answer:
Fast flowing waters .
Explanation:
the coriolis effect causes storms to spend in a counterclockwise direction . Jet Streams are narrow currents of fast-moving air in the upper atmosphere. They are created by the flow of air in the upper atmosphere which gets bent and channelled to the East Coriolis effect
