Fruition : A Long Journey Accomplished

I would like to thank the following peer reviewers for their excellent input on my essay.

Located in present day Collinsville, Illinois is Cahokia Mounds State Historic Site, which was once home to the largest city north of Mexico from 700 to 1400 A.D. Settled by the Mississippian people, today their decline remains a mystery. First visited in 1811 by traveler Henry Brackenridge and considered the “discoverer of Cahokia” only in the sense that he wrote several papers and articles about the findings to the public’s attention. After walking around the mounds, Brackenridge described that the locations of the last inhabitants were clearly visible to him, as were fragments of their tools and utensils. Many extensive archeological excavations and several case study theories have come about through the years as to why this magnificent ancient metropolis faced such demise.

This paper needs to read as an in class write that has been taken home, revised once and computer generated: double spaced, 12 point, three pages minimum, four pages maximum. ( see page three of this document, AP Literature and Composition Draft Requirements)

American archaeologist and anthropologist, Stephen Plog, wrote an account of the pre-Columbian natives of the Americans titled Ancient Peoples of the American Southwest. Plog’s purpose is to communicate the cultural and ritualistic lifestyles of the prehistoric natives of the southwest, which spans across the states of Arizona, Colorado, New Mexico, Utah, and Nevada with some mention of trade with Mexico. The author has demonstrated an effective approach of an objective viewpoint on the lives of the prehistoric south westerners using sources from excursions from previous archaeologists such as, Paul S Martin and David R Wilcox among many others who excavated the vacant villages of the southwest.

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

This study is focus on the 11th Unnamed Cave in Tennessee. This cave was the first of its kind because this cave is the only one that was found to contain pictograph, petroglyph, and mud glyph all in one site. The article explain that the site is significant because there are evidence to showed that the site underwent a series of diverse but interrelated uses. The first out of all the cave sites to contain all three different form of rock art. Also, because the site was found in the eighteenth century which had some form of documentations on the uses of the cave. The authors believes that since the cave showed many different kind of activities, it is possible that the activities reflect a complex behaviors more elaborated and sacred than

This article talks about the study of the Dunbar Cave in Montgomery County, Tennessee to learn more about the varied ways that the cave was used by people. Many of the artifacts that was in the cave linked its usage time to be from the Late Paleo-Indian to the Mississippian period. The article define dark-zone cave art as “the decorations in the areas of the caves that is beyond the reach of external lights”. Mug Glyph Cave art was found in the 12th Unnamed Cave in Tennessee and since then sixty-nine other caves that had dark-zone cave art were found. The artifacts and chronological data from these sites indicates that the tradition of cave art began 6000 years ago.

The objective of the trip to Blount Springs, Alabama was to observe and gather data on the geological structure of the area. Blount Springs is located in the northern part of Alabama just 33 miles north of Birmingham, and lies on the southernmost part of the Appalachian fold belt. The field work began on the morning of Saturday April, 7th at 8:50am. The weather was cloudy with temperatures in the mid 40’s, and the area was wet from rain the previous night. Our materials included a map of the area, list of formations, a Brunton compass, and a Rite in the Rain field book. The procedure of the field work involved 12 stops at outcrops to gather data, one stop was omitted from the original plans. This data gathered included bedding and joint orientations

The project was reviewed and accepted by the Institutional Review Board (IRB), to work with human subjects. Additionally, this project was reviewed and accepted by the Eastern Shawnee of Oklahoma Tribal Administration and the National Historic Landmarks Program of the National Park Service allowing this project to work in accordance with Section 106 of the archaeology guidelines.

The study area was approximately 3,717 acres in size, of which 421 acres (11%) were sampled with field investigations. Sample blocks measuring 360x150 meters in size were distributed among 31 broad pedological units. Forty-nine (49) archaeological resources were investigated, including two that were previously recorded, 33 that were newly identified, and 14 isolated finds. As a result, six sites were recommended for avoidance or additional work to firmly evaluate them for the NRHP. Based on the sampling, a density of one site/nine acres was estimated for the intensive survey phase. This density compared well with the density observed for the western section (Abbott and Davis 1995:130). Two hypotheses were given for the high site density: 1) better preservation as a result of less severe erosion and 2) specific prehistoric/historic settlement

This assignment is being submitted on March 17th, 2013, for Rick Barrett’s B491 course at Rasmussen College by Crystal Pierce.

Even though Teotihuacan has made such a lasting impact on all those who marvel at its grandeur and scale over the past two thousand years, this site in still far from understood. There are many mysteries surrounding this area even after decades of excavations and research. Archaeologists and anthropologists alike struggle to gain a clearer picture of this great Mesoamerican city, although continuing work at the site has provided a wealth of information about the region, occupants, and lifestyles of those who were touched by it.

The story of the Sevier-Fremont people’s evolution and existence in the Great Basin parallels Williams’ life in Utah during the 1980s. They Sevier-Fremont evolved from the Anasazi

A study published June 1, 2005 by the John S. and James L. Knight Foundation