There is no better place to admire nature’s adverse beauty, size, and diversity than the side by side Sequoia and Kings Canyon National Parks. These parks are home to not only a vast array of wildlife and forestry, but to the world’s largest living tree, the countries tallest mountain, and arguably North America’s deepest canyon. (“Harris, Ann”, 1990) These features alone make these parks a worldwide visitor attraction, where visitors can experience a new outlook of the sensational environment for which we live in. The dynamic landscape of the parks has evolved over millions of years and now preserves the largest groves of enormous sequoias. Sequoia and Kings Canyon National Parks contain various landscape features such as exfoliation domes, canyons, and caverns, along with bedrock geology from the late cretaceous batholith, and a tectonic setting similar to that of Yosemite National Park because of the …show more content…
All of the parks are located along the western slopes of the Sierra Nevada, which has been tilted westward. Because of this westward tilt, the eastern edge of the mountain range has steep slopes and the western edge has a more flat regional slope. There is a north-northwest trending normal fault system on the eastern edge. The height of Mount Whitney with an elevation of 14,494 feet, along with the height of Death Valley’s lowest point being 282 feet below sea level, will help explain the extent of this uplifting and downfaulting that is present within the area and its effect on the Parks landscape. (“Geology Overview”, n.d.) The stretching of the crust or lithosphere within the Death Valley is a result of this tectonic setting along the Sierra Nevada range. In fact this fault system is so dramatic that it is estimated to have moved vertically at least 15,000 feet. (“Harris, Ann”,
Harris, Ann G., Esther Tuttle, and Sherwood D. Tuttle. "Katmai National Park and Preserve." Geology of National Parks. 4th ed. Dubuque, IA: Kendall/Hunt Pub., 1990. 441-48. Print.
Committee on Senate Energy and National Resources Subcommittee on National Parks. 3 June 2003: ESBCO. Mission Viejo Library., Mission Viejo, CA. 31 July 2005. http://web31.epnet.com/citation.
In the 1800’s into the early 1900’s a man named John Muir began to explore the western American lands. He traveled down South and up North. But, when he reached Yosemite Valley, his life changed. As said in John Muir’s Wild America, written by Tom Melham, “Following the forest-lined mountain trails, Muir climbed higher into the Sierra Nevada: suddenly, a deep valley enclosed by colossal steeps and mighty water falls yawned before him. Spell bound, he entered Yosemite Valley” (79). Muir’s travels and adventures, highlighted in Melham’s book, explain this man’s love of the wilderness. Yosemite Valley was like a wide, open home to Muir, who, lived alone and discovered new landings and important later landmarks that create the aura of Yosemite National Park. Yosemite Valley was given to the state of California in 1864, part of the continuous idea of Manifest Destiny, later, in 1890; Yosemite became one of the first National Parks (“World Book”). Uniquely, the longer Muir stayed the more that he...
We are so fortunate to live in California and have access to so many of the properties operated by the National Park Service. There are thirteen national parks in California and I have been to seven of them. Enjoying the outdoors is something that is innate to our family. Even before our children could walk they were enjoying hikes through Yosemite in backpacks. This is an amazing fact that I learned from the map given to me in Sequoia National Park; “The only place Giant Sequoias grow now is on the west slope of the Sierra Nevada Mountains in California. The 75 distinct groves are found within a narrow band about 260 miles long and 15 miles wide, at its widest point.” (Sequoia National Park, 2012). Without the National Park Service protecting and maintaining parks like Sequoia National Park, there may not be any place like this for my children to learn about this beautiful country that we live
Petrified Forest National Park is located in the Painted Desert in northeastern Arizona taking up 93,532.57 acres of its land. Before the national park was established, it was founded as a National Monument on December 8, 1906 when President Theodore Roosevelt signed the proclamation. Years later, the Congress passed a bill and established it as a national park on December 9, 1962. Centuries before Petrified Forest National Park was preserved as a national park, the land was preoccupied by the Paleo people. At the onset of the end of the last Ice Age, hunter-gatherers, people who lived by hunting game and only gathering edible plants, roamed the Southwest from 13,500 to 8000 B.C. Although these people enjoy meals consisting of meat and vegetables, they don’t raise livestock and grow crops. During these years of hunting and gathering, the region was cooler with a grassland environment, and people gathered wild plants for food and hunted bison and other large herd of animals. The types of bison these people hunted are now extinct. Nomads used a device called an atlatl to throw their weapons, such as spears and darts, to hunt. By 4000 B.C., during the archaic culture, the climate had changed and became similar to the one of the present. This period of hunting, gathering, and farming had lasted from 8000 to 500 B.C. In contrast to the time of the Paleo people, the climate was warmer, people extended their access to different types of food, and people began to farm and grow their crops. Due to the extinction of animals of the past, people had to expand their source of food, and they had to include many different species of plants and animals into their meals. Two hundred twenty-five million years ago, trees fell and were washe...
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
Yosemite and its history, young to old the story of an area of land that is doomed to be mined, forcibly stripped naked of its natural resources. In 1864 Yosemite land grant was signed into act by president Abraham Lincoln, the first area of land set aside for preservation and protection. Yosemite being a very important historical plot of land, some time ago president Theodore Roosevelt visited the park managing to disappear from the secret service with John Muir. Through the years the contrast of ideas between the industrialists and the preservationists have clashed, Yosemite’s history both interesting and mysterious but more importantly inevitable .
The park is an asymmetric mountain range, it is 50 to 80 miles wide and it extends in altitude from near sea level along its west edge to more than 13,000 feet along the crest in the Yosemite area. The highest peek in the Sierra Nevada and in the United States is Mount Whitney, which is located in Sequoia National Park. Yosemite is dominated by a huge amount of granite and so is much of the Sierra Nevada’s. Mount Hoffman and most of what is visible from there is composed of granite. Granite is formed deep within the earth by solidification of molten rock material and is also due to the exposure of erosion of the rocks, which are overlaying.
Every year, over nine million hikers and adventure seekers travel to the Great Smoky Mountains National Park making it the most visited national park in the United States. There are abundant reasons for this, but many popular reasons include over 150 hiking trails extending over 850 miles, a large portion of the Appalachian Trail, sightseeing, fishing, horseback riding, and bicycling. The park houses roughly ten thousand species of plants and animals with an estimated 90,000 undocumented species likely possible to be present. It is clear why there was a pressing interest in making all this land into a national park. My research was started by asking the question; how did the transformation of tourism due to the establishment of the Great Smoky Mountains National Park affect surrounding cities such as Gatlinburg and Sevier County, and in return, its effect on the popularity of the park?
The geology, its history, and the presence of past civilizations contribute to much of the significance of Mesa Verde National Park. The interconnectedness of these aspects should also be noted. If not for the weathering processes and changes in sea level this formation would not exist. Without it, the ancient people would not have been able to reside within Mesa Verde. This National Park now serves as a tool to help conserve the remains of these past civilizations as well as to help educate today’s society on the significance behind this astonishing geologic
Many Americans love to hike. There are many hiking trails located in the United States. One of the most well known trails is the Appalachian Trail. The Appalachian Trail, with its distinct history, requires much conservation for the safety of its many hikers.
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...
Boom! A once ice-capped mountain peak explodes as ash fills the air. “‘Vancouver, Vancouver, this is it!’”Those were the last words of expert geologist David Johnston (Gunn 561). In 1980, Mount Saint Helens of the state of Washington erupted, filling the air with ash and causing mudflows powerful enough to lift tons. It decimated everything in its path. The eruptions, mudflows, and ash caused great damage on the landscape, yet it gave us information on how catastrophes happen and how they affect society and the surrounding landscape. The data acquired can also help us understand the way the landscape was formed. Mount Saint Helens caused much damage, but also helped people understand the science behind it.
The 6.7 magnitude earthquake was felt throughout most of southern California and as far away as Utah and Mexico with a max acceleration of 1.0g in several different areas and the highest at Tarzana with a recorded value of 1.8g. The earthquake also deformed over 1500 square miles of the Earth’s crust, forcing the surface upward in a dome shape. The Susana Mountains sustained the most soil deformation with an uplift of around 15cm causing numerous rockslides, blocking many roadways. Soil liquefaction was observed in the Simi Valley area and other parts of the Los Angeles Basin. After all the term oil ended the preliminary cost estimate of damage was between 15 and 20 billion U.S. dollars. Today, Geologists remain to search for thrust faults throughout the southern California area by using a 3 dimensional modeling system to view folds and upli...
I am about to describe to you a walk in the park. That being said a few details are required for you to fully picture the likes of what I am about to describe. The time of day is a little past noon and the wind is howling. The sky is a pastel blue, almost as if a wash of blue light was covering a white canvas. The sun is vibrant and concentrated. You can sense the gentle warmth of the sun on your skin and see the lively colors of the world all around you. Alert to the dancing light that surrounds you, your journey begins. Searching for your starting point you choose to begin walking down a gravel pathway that has a clearing of trees a few hundred feet away. The day has a familiar, inviting glow and all around the gentle colors of green, yellow and red surround the pathway. The sun a luminous