CT Surface and landscape
There are many process that made Connecticut’s surface and landscape get its shape. The Plate tectonics, the glaciers, and weathering and erosion are the main causes to the change to connecticut.
Plate tectonics have affected the surface and landscape in Connecticut. The Appalachian mountains is an example of how the landscape changed. The tectonics plates had moved together creating convergent boundaries. So this means that the plates collided and this is the mountains are formed. The Connecticut river valley also has changed the landscape and surface in Connecticut. This is because the valley made a big U in the land. The valley was formed when the tectonic plates moved apart.
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The Wisconsin glacier made the Connecticut River, Long Island Sound, Jobs Pond, and Hammonasset State Park. Jobs Pond was formed by a piece of the Wisconsin Glacier that fell of and created a kettle hole, which then melted and created a pond which filled with rain water. Long Island Sound was formed by a glacier. The glacier reached long island and the glacier could not move any farther. So this would mean that Long Island Sound the glacier could not move any farther so Long Island Sound was a terminal moraine. A terminal moraine mean that this was as far as the glacier could move. Then when the glacier was melting in Long island Sound the water levels got high and then the water went over the dam blocking the Atlantic ocean from Long Island Sound but then this two bodies of water mix creating an estuary. So the glacier made Long Island sound mix with Atlantic Ocean. The Connecticut River was formed by a glacier that covered the entire state of Connecticut. Some of the glacier melted and the water formed The Hitchcock Lake. The lake then pushed through the dam and went into the CT River Valley which formed the Connecticut River. Hammonasset State Park was formed when a mile and a half of ice from the Wisconsin Glacier covered the beach. When the ice reached the water the glacier melted leaving rocks on the shore which is called plucking. These rocks that were left came from different
More specifically, Trois-Rivieres is located in an area with flat and rolling hills, and fertile soils that play a huge part of Trois-Rivieres’s economy. The formation of the Great Lakes-St Lawrence Lowlands happened during the Paleozoic era. “The Great Lakes-St Lowlands were formed by the effects of glaciation. This is caused the city’s rolling landscape where flat plains are interrupted with glacial hills and deep river valleys. After the glacial period, when a large volume of water melted out from the glaciers, the lakes were large, even larger than they are today. However, the lakes shrank to their present size, and flat plains of sediments remained. These sediments formed excellent soil for farming” (Pandya, n.d). This process left behind a large amount of sediment rock, which was beneficial for the manufacturing industry.
Both Mystery and Niagara Cave are made of limestone. Limestone is formed when areas that used to be covered with water, would have contained shelled animals and other organisms. When the animals died, their bodies along with waste matter from other organisms, floated down to the bottom of the water. Over time, it was compressed and formed limestone. Caves are usually made of limestone because it is easily carved out by water. This is the case for Mystery and Niagara
The characteristics that came to shape the life in New England were the rocky, barren soil, the extreme climate and the rich waters. Although there was farming in New England , colonists looked to other means of survival. They looked to the rich waters for fishing and trade. The coastline of New England was very fertile with sealife. So, fishing became a way of commerce and trade providing a steady economy to New England. Because of the rocky soil and extreme climate, the colonists were forced to plant many different crops on a small pa...
Glaciers are an integral part of the world’s climate. In fact, as Richard Armstrong of the University of Colorado says, “Glaciers are key indicators in monitoring and detecting climate change” (Univ. of Colorado, Boulder, 2003, p. 1). Not only are they an important part of monitoring current climate, they can hold many keys to the past. Glaciers are in fact, “a source of paleoclimate data…” (Meier and Dyurgerov, 1980, p. 37). This paleoclimate data can give geologists information on the conditions that were present at the time of the glaciers birth, as well as the approximate age. This has an important role in the geologic time scale of the Colorado Rocky Mountains. These Glaciers played a role in the carving of the present day Rocky Mountains in Colorado, which will be the primary focus of this paper. In addition, glacial formations will be discussed to give the reader background information and the future of the Glaciers in Colorado will close this paper.
The development in the two societies was apparent throughout the start of each colony and through the events occurring throughout its developmental period. New England and the Chesapeake colonies arose as separate states with separate motives and separate resultants with each method having its pros and cons for certain people. The beginning motives, the decisions made throughout each settlements respective history, and the method of forming a better community surrounded the top grounds for different societies arising.
...the only major geologic event in the history of the Appalachians. Several glaciers have covered parts of the Northern Appalachians over the last three million years. (Appalachian tales) The mountains have been there ever since and that is how they were formed.
Like Massachusetts, Connecticut was made by the Puritans. It was an early agreement between the other community colonies, that established a representative of government based on the number of people who lived in Massachusetts. The purpose was to describe the government set up and setting its structures and power. They were the first of the thirteen colonies to allow religious freedom. They felt people of Connecticut believed that people shouldn’t be persecuted for their religious beliefs the way they were in England.As more and more of the English were coming over the Natives started to see that they we outnumbered and became frustrated.The war between the two ruined not only the peace between the settlers and the Natives, but also killed a lot people on both sides. This was a sad time for both the Natives and
As colonies of the British Empire, both the New England and Chesapeake regions were inhibited by innumerable immigrants of English origin. Despite this common characteristic, the two areas greatly differed from each other. New England was more tolerant and community based whereas the Chesapeake was focused more directly on personal wealth and land. While they both drew from British influence, the distinct conditions in each region caused them to develop separately and become unique in their own way.
Continental drift- led to the change in the physical features of land, its position and a change in ocean currents.
5 Narratives of the Indian Wars 1675-1699, edited by Charles H. Lincoln, Ph.D: A World Wide Web Site Containing Information About the Biology, History, and Geology of New England's Largest River (http://www.bio.umass.edu/biology/conn.river/), University of Massachusetts, Amherst.
...oncerning the way people live and interact in America today. From why California has so many earthquakes with the San Andreas Fault, to the formation of America’s national treasure Yellowstone Park, and even why certain crops are located where they are, it is important to know just how geology affects the United States. There are many different ways how America has changed throughout time, but the evolution in geology is the changing face of America.
The average elevation in the Hudson Plains is 120m above sea level. It is a flat lowland area. The land is made up of mineral soils, with few outcrops of underlying sandstone and shale. This land was created when the weight of glaciers depressed the Hudson Bay region and the ocean waters flooded areas up to 300 km inland from the current coastline. Then, during the retreat of the huge continental ice sheets, drainage into the Hudson Bay was blocked and lakes (Agassiz and Ojibway for example) were formed along th...
The main theme in Rising from the Plains is the formation of the Rocky Mountains. “Topography grows, shrinks, compresses, spreads, disintegrates, and disappears” (McPhee 27). The physical features of the Earth are temporary and are always changing. The
Ice dams in the Clark Fork area that backed up Glacial Lake Missoula actually caused some of the largest floods known to man. As ice will float, these ice dams would periodically rise up and burst, catastrophically flooding the Rathdrum Prairie, eastern Washington and into northern Oregon. Locally, these floods brought in glacial till and deep deposits of outwash that obliterated the St. Joe River once running through the Rathdrum Prairie. The southernmost edge of these deposits terminated where Coeur d’Alene exists today, damming the old St. Joe River and creating Lake Coeur d’Alene (Alt and Hyndman, 73). The new lake received the entire flow of the Coeur d’Alene and St. Joe Rivers, more than could be absorbed through the gravel deposits, thereby causing the lake to overflow and seek a new course, now known as the Spokane Ri...
This landscape was made millions of years ago during the ice ages, when moving glaciers of ice made deep valleys, steep mountain slopes and long lakes. The southern and eastern parts of Britain are made up of smaller rocks that have weathered and become fertile farmland.