Red Rock Canyon Research Paper

Ever since my dad was a young boy he has wanted to visit all the National Parks in the United States. We’ve already been to The Grand Canyon in Arizona, The Badlands in South Dakota, Biscayne in Florida, Mesa Verde in Colorado, and many more! This time we were headed for Colorado where National Park, Black Canyon of the Gunnison, is located. I was really dreading this trip. I’d never heard of this park before and neither had my friends. All the other parks we’d been to have been really interesting and enjoyable, but Black Canyon of the Gunnison most likely won’t be.

Approximately ten miles from downtown Atlanta, one thousand six hundred eighty-three feet above sea level stands Stone Mountain. Stone Mountain is, simply, an enormous rock that is made of granite. The mountain can be seen from Kennesaw Mountain (West), Amicalola Falls State Park (North), and Mount Yonah (Northeast). Surrounding Stone Mountain is the city of Stone Mountain. On February 21, 1958 the governor of Georgia, Marvin Griffin, signed the bill which authorized Stone Mountain to become a state-run park and allowed it the authority to receive money from bonds granted by the state. Since that day, the park has added many different attractions and hosted multiple different events which, to this day, are very popular.

Rock Canyon is an excellent site for geologic research and has been investigated by geologists from around Utah and neighboring states. With outstanding extrusions of quartzite, tillite and limestone, it’s a favored destination for hikers, rock climbers and scientists. The quartzite is considered the most unique feature of Rock Canyon as it’s one of the few clear and distinct examples of the sedimentary processes involved with a shallow marine setting. The tillite beneath the quartzite draws attention to the ancient glaciers to the past. In conjunction with the active Wasatch Fault found at its doorstep, Rock Canyon is an important place in Utah for geologists.

Lockegee Rock near Morehead Kentucky holds a stunning view of the Daniel Boone National Forest!

On this day in 1863, Union troops capture Lookout Mountain southwest of Chattanooga, Tennessee,as they begin to break the Confederate siege of the city. In the “battle above the clouds,” the Yankees scaled the slopes of the mountain on the periphery of the Chattanooga lines.

Little Cottonwood Canyon is a site bursting with geological history, rock formations earthquake potential on the fault, prehistoric glacial formations, landslides, and many hazards associated with it. The Wasatch fault is bound to have a enormous earthquake in the future and has left behind numerous scars. The mountains have been engraved by glacial formations dated back to the Ice Age (~14,000 years ago). Rock falls and landslides have left hefty boulders as indication of erosion and moisture in the rocks. The hazards on this mountain range are mass wasting, radon, earthquakes, and flooding of Little Cottonwood Creek.

Mesa Verde National Park on the Colorado Plateau contains many geological aspects of interest, including its sedimentary rock layers, its canyons, its alcoves utilized by ancient people and how these alcoves were formed. Mesa Verde National Park is located in the southwest corner of Colorado, close to the Four Corners area, on top of a high mesa overlooking the Mancos River (Harris et al. 2004). The park, covering 81 square miles, consists of several main sedimentary formations that are characteristic to the park (Encyclopedia Britannica 2015). Canyons are carved into the sedimentary rock, with the cave dwellings found high on their steep walls. These dwellings are an especially unique aspect to the Mesa Verde National Park, and are built out of large alcoves. The alcoves were produced by weathering and erosion of the sedimentary rock type. To better understand how these alcoves formed, we must understand the geology of Mesa Verde National Park and how it has developed over history.

Our hike will start here, at the north rim of the Grand Canyon. We will go all the way to the bottom of the canyon. But first, a description of this area. The Grand Canyon is one on the most visited and studies sites for geologists on Earth. There are almost forty major sedimentary rock layers exposed in the Grand Canyon. Some of these rocks layers are two hundred million years old or two billion years old. Most of the sediment that makes up the rocks was deposited by oceans and seas, which now, are long gone. We know this because there are many fossils and and other records on large bodies of water in the Grand Canyon. The Grand Canyon is found in the Colorado Plateau. The Colorado Plateau is lifted almost two miles, or four and a fifth kilometers. It started to lift up seventy-five million years ago. This started a mountain-building period of time called the Laramide orogeny. During this period, the Rocky Mountains were created. The main types of rocks found in the Grand Canyon are limestone, siltstone, shale, and sandstone. Many of the layers are made up of limestone. Some examples of these are the Kaibab Limestone, the Redwall Limestone the Temple Butte Limestone, and the Muav

Designed by Lee Schmidt and Brian Curley, this 18-hole championship golf course proves the perfect course for any player. Maintained to the highest of standards, the wide fairways and wavy greens prove to be easily playable, and have become a trademark at Copper Canyon. If this doesn't encourage you to play here, perhaps you will be indulged by the surrounding landscapes that prove to make Copper Canyon a truly special course. You will also find that the surrounding landscapes is not all that this golf course offers in regards to its beauty, as over 11 beautiful lakes are featured on the course itself, making an all round mesmerizing golf course.

Providence Canyon, is located in Georgia's southwest. The canyon was officially named a state park when the government did not want to name it a national park in 1971. There are a few reasons why Providence canyon should be named a national park. This canyon has many different types of sand and rocks with in it, which could be used for education in science. Trips could be planed by schools to take students and study the rocks that are their. Also by making it a national park tourism will be raised and the people could spend money in local businesses. Providence canyon was a dense forest before it was a canyon. Farmers in the early 1800s started growing cotton in that area, they cut all of the trees and plowed to plant seed. They planted with long straight lines, which started the events

I am going to be going to attend Big Morongo Canyon Preserve to volunteer a day on September 30th. I am a 10th grade student that is currently going to Yucca Valley High School. First task I need to do is receive permission from my guardians to go to the preserve. I have discussed with my parents today September, 12 what I am doing and they are one hundred percent on board. My parents are willing to be my transportation there and back.

Smith Rock State Park is awesome. It is located near my home in Central Oregon. It is a frequent place for locals and visitors from all over the world. The spectacular spires and walls are carved out of 30-million-year-old welded tuff and rhyolite rocks that formed from the ash explosions and lava flows of an eruptive volcano. Geologists have identified a 230-square mile depression, called a caldera, that is all that is left of this ancient volcano. A caldera is a giant crater that forms when a magma chamber beneath a volcano erupts a large volume of material. The top of the volcano literally collapses into the newly emptied chamber, creating a huge depression. Smith Rock State Park is on the northwest corner of what is now known as

Stone mountain has remained a very influential monument of Georgia; a gem of what may say to the state’s tourism and a landmark of American history throughout the ages. Stonewall Jackson, Robert E. Lee , and Jefferson Davis on top of their valuable steeds represent the Confederate nation and its tie with Stone mountain as they are carved meticulously in the world’s largest exposed granite; however, the peaceful serenity of the lake and nature that envelops the mountain and its visitors remained a very important ceremonial location for native americans. The complete history of Stone Mountain is interwoven into the treads of historical events that have occurred throughout and even before the great nation , United States of America, was formed. Currently, it’s one of the most famous attractions in Georgia known for the breathtaking view of metropolitan Atlanta at the peak of the mountain. It is clear as rich as the beauty of stone mountain is,undeniably, it has a strong historical importance to American history and exquisite backround.

The Rocky Mountain National Park is only an eighth the size of Yellowstone National Park. I am also going to camp in the Rocky Mountains. There are 5 campgrounds with 585 campsites in the national park. I finally get there and see the most beautiful sight in my entire life. There

The landscape is stark, but the beauty startling. The expanses seem to welcome, even beg you to explore. It’s a call you are unlikely to be able to resist (assuming it’s not scorchingly hot and you are not hungover from a big night in moments-away Las Vegas), nor is it one you should. In front of you is one of America’s grand spectacles, Red Rock Canyon.