Ancestral Novo National Park Essay

Read excerpt # 3 The Anasazi: Chaco Canyon and Mesa Verde and excerpt # 4 The Mississippians: Cahokia and Moundville (pp.29-33) by following the link Pre-Columbian America (Learner.org). Type responses to the following questions on Google Doc and save.

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

115-miles south of Moab is a land revered by generations of climbers, hikers, and adventurers. It’s a land known as the Bears Ears, a series of buttes that constitute jeep trails, sacred archeological sites, unique sandstone formations, and the cherished climbing walls of Indian Creek. Not only loved by outdoorsman, the Bears Ears is also an important area to the Navajo, Ute, and Pueblo Native American tribes. Excavations here have revealed rock art, pottery, and cliff dwellings, documenting over a millennium of human habitation. The Bears Ears are loved but unprotected, and they are at a pivotal crossroads.

The Grand Canyon is one of the greatest natural creations our planet has to offer. Have you ever been mesmerized by the giant cliffs, massive ridges, or the wide array of beautiful colors? If you answered yes, this paper is just for you! After reading this, you will be well educated about the Grand Canyon.

Chaco Canyon, located in what is New Mexico today, closer to Arizona, is one of the archeological sites with many hypothesis and conclusions full of contradiction because of its complexity of what was happening there during Chaco’s economical peak. It is one of the prehistorical places that hold the history of the humans and how complex the organization between social, religious and economical was. The remains of the amazing tall and complex buildings surrounded with roads helped the archeologists to hypothesize the use of those buildings and those roads that surrounded them.

This book, The Haunted Mesa, was written by author Louis L’Amour, under the publishing company Bantam Books. It was published in New York in 1987 and the story of the book takes place around this time as well. The significance of the title is to hint at the central idea of the story, which revolves around a mesa in the deserts of southern Utah. The place is very odd, having bizarre occurrences described by both the main character and another character in the story. These occurrences advance the plot astronomically. Not only this, the setting is what pulls the reader into the book, intriguing and making the reader curious for more.

Of all the features upon the earth there are some ascribed with special significance. These features, whether caves, lakes, deserts, outcroppings, or something else entirely, hold tremendous relevance for the groups that dwell near them. Such beliefs in the worth and importance of such sites are entrusted from one passing generation to the next. These beliefs, and the physical objects they rest upon, become increasingly vital to that group’s identity as a people. One such group is the Teton Lakota of the Sioux Nation in South Dakota, an area that has been home to them for hundreds of years and, while their entire homeland is precious to them, of particular importance are the Black Hills, or Paha Sapa as they are called in Lakota.

The oral history of these people talk about how groups or bands of people were entrusted to care for the environment and resources within their ancestral territory (About The Hualapai Nation, 22). They are descendants of a group called the Cerbat (“Hualapai Tribe”). The tribe’s ancestral territory estimated to be about five million acres (About The Hualapai

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.

Around 650 A.D., the Mesa Verdean peoples initiated construction of apartment-style homes, termed by Spanish explorers as pueblos. The Puebloan architecture is original in that it utilized the local stone and mud deposits of the region to maintain the structural integrity of their burgeoning developments. As this community evolved into the twelfth century, Mesa Verdeans further integrated the geology of their environment into their lifestyles by building homes, known as cliff dwellings, within the naturally formed alcoves of Mesa Verde. By the thirteenth century, the Mesa Verdeans vacated this region due to severe droughts and subsequent social instability. Despite the later abandonment of their cliff dwellings, it is clear that the geology of Mesa Verde National Park impacted the lives of the Ancestral Puebloans significantly. The following sections provide detailed information regarding the rock formations that make up the geological

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

Located on the borderline of the Colorado River, in the early days of Palo Verde Valley, the Yuman, Northern and Southern Dieguno Tribe,

Another important thing to mention in this picture is the vegetation that is growing on top of the cliff since it is so close to the coastal line. This picture is only a glimpse into what surrounds these cliffs since there are many different landmarks and lithosphere actions considering it is close to the san andreas fault, the monteray bay fault and the palo calorado

This unique park is often described as an urban wilderness because its 130 acres of trails are nestled just two blocks from Hollywood Boulevard. Entrances to the park can be found on Fuller Avenue, Vista Street, and Mullholland Drive. There are a number of trails of varying difficulty, many of which lead to breathtaking views of the city and surrounding area. A wide road can be found at the Vista Street entrance for those looking for an easier stroll. Hikers can choose to enter the canyon from the south then climb upwards either clockwise or counter-clockwise for varying levels of strenuousness. Both will allow you to take in Inspiration Point and Clouds Rest. Entering the canyon from the north will give you the option of several short hikes, one of which includes Indian Rock, the highest point in the canyon. If you want to allow your dog to roam off leash, choose the western trail which can be found from the Vista entrance.

The vast forest of western United States covered in lakes and various different living being a certain type of being lived there also; they are known as the Menominee Indians. They have lived in the western United States for thousands of years. Menominee means Wild rice people people, which fits because they used to harvest wild rice for food (Schmittroth and Ryan, 5 ). This tribe has a unique history that goes back thousands of years before the pyramids were built. With the thousands of years of rich history there are tremendous amount of heritage, struggles and overcoming of this wonderful tribe.