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Grand canyon research paper
Grand canyon research paper
Grand canyon research paper
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The Grand Canyon is one of the greatest natural creations our planet has to offer. Have you ever been amazed by the giant cliffs, massive ridges and the wide array of beautiful colors. Well, after reading this you will know how the Grand Canyon became what it is today. The Grand Canyon is in the northwest corner of Arizona, bordering Utah and Nevada. More than five million people visit Grand Canyon National Park per year. The Grand Canyon is roughly 280 miles long, 18 miles wide, and in some places more than 1 mile deep! The estimated volume of this enormous park is estimated to be over 5.5 trillion cubic yards, trillion that’s 12 zeros! While the Colorado River carved this canyon 5-6 million years ago, some scientific evidence brings the …show more content…
The truth is that no one knows for sure exactly how it was formed, but with scientific research and theories most scientists agree to the same basic ideas. The most powerful forces impacting the creation are erosion and weathering. Which is heavily due to the Colorado River running right down the majority of the canyon. Since the Grand Canyon is located in a desert climate the soil in the Grand Canyon is baked by the sun and it tends to become very hard and cannot absorb water, when the rain come. So while the Colorado River is gushing through the rocks and the root systems are pretty weak over time the erosion really builds up. The Grand Canyon is basically an enormous sedimentary rock. Sedimentary rock is formed from other rocks being weathered, either chemically or mechanically into sediments or rock fragments. These rocks are then gone through erosion, which is the process of moving sediments from one place to another. Then, these sediments are deposited all at one place and over time they start to converge and cement as layers which are also known as strata. As time keeps going new sediments deposit and cement together over old ones forming new layers. The process just keeps repeating itself and then finally there are all these layers that make up a Sedimentary …show more content…
Now, the million dollar question is where did all the rocks com from? The answer to that question is The Continental Drift. The Earth's continents are not fixed in place but rather float on a sea of molten rock, meaning that they move around quite a bit. Over 250 million years, quite a bit can turn into land masses moving thousands of miles. The Earth is made up of 20 Tectonic plates. Seven of these plates are very large and consist of entire continents or sea floors. The plate that the Grand Canyon is located on is called “The North American Plate”. At one time this plate was considerably further south and in result had a very different climate than today. As Tectonic plates collide they can form three different boundaries, one which is a Convergent Boundary. This boundary often leads to mountain building. A much older range of mountains now form the base of the Grand Canyon. The rocks that made up these mountains are now estimated to be around one and a half billion years old. When the sea level rises, land areas which are by the coast and relatively have a low altitude are sometimes submerged in water. This was the case area of the Grand Canyon and is why so many different sedimentary rock layers exist. Each of these was formed by a different period in which the ocean came in flooded the land, stayed for a while, and then pulled back to normal
...e morphed it into the quartzite that is seen surrounding the butte (4). Rocks that undergo this process are called metamorphic rock, which is the same as the rock seen years ago by dinosaurs and other extinct creatures. The quartzite rocks were formerly seafloor sediment that was forced upwards, and then surrounded by lava basalt flows. Once erupted through fissures and floods through out most of the area, lava flow eventually created enough basalt to form a thickness of about 1.8 kilometers (1). All of this basalt flow eventually led to the covering of most mountains, leaving the buttes uncovered. The igneous lava flows and loess is reasons that the Palouse consists of such sprawling hills, and rich soil for farming (2). In result of the lava flows, the Precambrian rock Quartzite was formed. And lastly covered by the glacial loess, which were carried by the wind.
Many people know ‘Lake’ Powell as a fact of life. Since its creation in 1963, the reservoir, known as Lake Powell, is just there. Few people that are alive today have had the opportunity to see the true beauty of Glen Canyon, which rivals the Grand Canyon. Glen Canyon, equivalent to one hundred eighty river miles with dozens of side canyons, was flooded for the purpose of power and water resources. ‘Lake’ Powell also generates an enormous cash flow due to the tourism it receives. Although the ‘lake’ has a few reasons to remain in existence, there are many more reasons to drain it.
Canyonlands National Park, immense amounts of wilderness and rock, is located at the heart of the Colorado Plateau (Canyonlands National Park-Geology). Millions of years have formed specific features to the rock and surrounding wilderness that make it so special. Throughout the park, you will find that the sedimentary rock has formed many features such as hundreds of colorful canyons, mesas, buttes, fins, arches, and spires. The Green and Colorado rivers have played a major role in the formation of many of these features. These rivers cut through the park forming two massive canyons. This further splits the park into three distinct zones. “Island in the Sky” sits to the north while “The Maze” sits off to the west and “The Needles” to the east (Canyonlands National Park Information Guide). “Island in the Sky” serves as Canyonlands’ observation tower; it allows tourists to see overwhelming vistas of the rest of the land. “The Maze,” as hinted at by the name has been described as a “30 square mile puzzle in sandstone” (NPS: Nature & Science» Geology Resources Division). This section of the park often ranks as one of the most remote and inaccessible areas of the United States. Lastly, “The Needles” is known for its diversity in rock features. Throughout this land, features such as sculptured rock spires, arches, canyons, grabens, and potholes can be seen. The varying names hint at the diversity of the land as a whole. As said by The National Park Service’s Geology Resources Division, “Traces of the Anasazi can be found in almost every canyon in the Needles. Many of their stone and mud dwellings and storehouses are remarkably well-preserved. Tower Ruins, built high on a cliff ledge in a side canyon of Horse Canyon, is an outstanding ex...
At the end of the last ice age windblown silt covered the lava and basalt deposits. This silt would go on to create the fertile rolling hills of the Palouse. This soil is more than a hundred feet deep in places. Soon, enough time passed for vegetation to take place and more soil started to form.1 The lava flows would end up damming streams flowing from the mountains; in turn forming the current lakes of the region. Layered between the flows of basalt are sand and gravel deposits that washed down from mountains.1
The geological arrangement was largely influenced by the Western Interior Seaway, which swept through the continent millions of years ago. It was during this time when frequent alterations in climate caused the waters to surface and withdraw. The Dakota Sandstone deposited within the sedimentary profile of Mesa Verde is in large part due to these events.
Yellowstone Park is the world’s first national park and the 8th largest national park in the United States. The park is primarily located in Wyoming and parts of Idaho and Nevada (56 Interesting Facts About . . . Var Addthis_config = ) It is a tourist attraction due it’s 5,000 to 15,000 years old geysers, over 45 waterfalls, canyons, rivers, hot springs, and its massive concentration of natural wildlife. Two of the most popular park attractions are the Old Faithful geyser and the Grand Prismatic springs. ("Fun Facts." - 32 Interesting Facts Yellowstone National Park.)
Zig-zag, back and forth, down, down, down, Jonathon, Dad, and I went into a mysterious new world. Now that I have gone into this hot, dry canyon surrounded by monstrous hoodoos, I have seen what it is really like to leave the small town of Seymour, and emerge into the greatness of this world. I have now seen several other National Parks on one of the most renowned places on earth for mysterious creations, the Colorado Plateau. Of all the beautiful places on it, even the Grand Canyon, I have found my favorite one. Bryce Canyon National Park. I thought it was amazing, because it was the most diverse to anything I have ever seen before. We hiked down into it and I felt like I was surrounded by skyscrapers. We trekked around a little, but we didn’t
The Little Missouri River eroding the mountain range is the reason that the park is as it looks today. The park is believed to be <60 million years old. Over 60 million years ago volcanos all over the west were erupting and spitting out amounts of ash. The rivers near the volcanos were gathering. The rivers began to dry out, leveeing the ash behind. The ash was being dried in layers and turned into sandstone, siltstone and mudstone while the ash layers became bentonite clay. This Bentonite clay is dangerous because it gets people stuck, like quick sand it is located throughout the park. It can pull the car tires un...
The world has been shaped by many events. Like a sculpture each piece was a result of an event that made it that way. The Snake River Canyon is no different, most of upper Utah and part southern Idaho show the scars of an event that rocked the landscape into what it is today. When researching and digging in the region you can find remnants of an old marine environment, from sediment deposits to river terraces hundreds of feet high. It’s confusing to think of the area as a giant lake with sandy beaches and powerful waves, but the overflow of this huge lake is what created most of the landscape you can see today. The great Bonneville flood was the world second largest flood, emptying over 32,000 square miles of lake volume. (Utah Geological Society) The flood that the this overfill caused carved through many areas and created the beautiful valley that can be seen there. However, this didn’t just happen over night. The pre-flood history, flood event, specific flood deposits all played an important role in shaping this large Geological marvel. Understanding what happened back then can give us a good glimpse into better understanding the region today, which can lead to better predicting and preserving for the future.
Established as a National Park in 1933 under President Franklin Delano Roosevelt, Death Valley is the largest national park in the continental United States even though its total length is no more than approximately 100 miles in length. The valley is located in the Mojave Desert in eastern California and is surrounded by the Amargosa Range on the east, the Panamint Range on the west, and the Sylvania Mountains and Owlshead Mountains on the northern and southern boundaries. The topography of this region is varied and complex; and has a lengthy geologic history that explains why it is riddled with a variety of sand dunes, craters, and flood-carved canyons to name a few. The total area of the valley is about 3,000 square miles with the lowest elevation being located at the Badwater Basin at 282 feet below sea level. Interestingly enough; however, the highest elevation of the region is 14,494 feet above sea level.
The Interior Plains is a region in west-central Canada, in the Mountain and Central time zones. It is the fourth largest region of Canada. Majority of the Interior Plains is prairie land with lots of flatlands. The total area of this region is 1, 900, 000 km². Approximately nineteen percent of Canada’s population lives in the Interior Plains region. This region includes certain points of interests and attractions such as city areas like downtown Calgary and natural sightseeing areas like the Rocky Mountains. The majority of the Interior Plains is prairie land, with many trees and grass. Most of this area is wide, open spaces and flat land. Some of the animals living here include deer, wolves, and
Blakey, R. C. (1996). Geologic history of western us. Informally published manuscript, Northern Arizona Univ, Flagstaff, AZ, Retrieved from http://www.jan.ucc.nau.edu
...erospace and transportation. Also important are high-technology researches and development, communications and service industries. Since the 1920s and 1930s the importance of the tourist industry began to grow and it is still one of the most important sources of income of Arizona. The mountains in the northern and central regions of the state have 1,286,900 hectares of commercial forests. These forests are owned by the U.S. government for 95% and are used for lumber and building-materials industries. The state forests and the national forests attract millions of tourists each year. Other famous tourist spots are the Grand Canyon, the Painted Desert, the Petrified Forest, meteor craters, ancient Native American ruins, the Spanish colonial ruins and the Navajo and Hopi reservations. Golf courses and other leisure facilities attract a large amount of tourists as well.
same liquid rock matter that you see coming out of volcanoes. On Earth's surface, wind and water can break rock into pieces. They can also carry rock pieces to another place. Usually, the rock pieces. called sediments, dropped from the wind or water to form a layer.
Schoolbooks called it one of the greatest wonders of the world, bringing to mind pictures of a far away, unattainable place. It seemed like a larger-than-life miracle of nature. As a child, I believed that Niagara Falls, like Mt. Rushmore and the Grand Canyon were all very real attractions of the United States. I was given the facts and numbers, but never could my young mind comprehend the actual size and greatness of the falls.