Wait a second!
More handpicked essays just for you.
More handpicked essays just for you.
Geological investigation in geology
Geology 111 study
Don’t take our word for it - see why 10 million students trust us with their essay needs.
Recommended: Geological investigation in geology
Geology field trip Journal On Tuesday, October 25, 2016, our Geology class visited the Hammonds Rocks, in South Mountain, Cumberland County, Pennsylvania. The main goal of the trip was to observe real life examples of geological concepts and principles, that we have studied over the course of this semester. Throughout the trip, my classmates and I were able to see different geological features that resulted from geological processes such as erosion, transportation, and deposition. Along the way to the site, our professor tried to show and explain to us some of the real life examples of the differential erosion process along the Susquehanna river, and near the site at South Mountain park, where we were able to see, through a broad view of the Cumberland valley, the features resulting from differential erosion along the valley. …show more content…
This exercise gave me an opportunity to put into practice geologic concepts, such as sorting, rock texture and environmental indicators like joints in determining the geologic history of a rock. With the help of our professor, my classmates and I were able to determine that the rock, which was a congramerate sedimentary rock composed of sandstones gravels and milky quartz minerals. The outcrop was composed of beddings consisting of layering of fine followed by coarse particles. This observation indicated that the rock might have resulted from deposition of sediments by a river with seasonal variation in the volume of water, particularly, a braided river. Also, by observing the orientation of some of the rock particles on the outcrop and sorting of the rock sediments, we were able to determine the evidences for flooding and variation in the force that transported the particles as they were deposited to for the
The Starved Rock Member of the Saint Peter Sandstone is preserved as a northeast-southwest trending belt of strata that is ...
1. 225 MY : Weathering and erosion of very old folded rocks on an area
Sedimentary rock from the older Silurian Period is further from the river banks (Geological map of Victoria, 1973). Mudstone, inter-bedded shale and greywacke depositions indicate the Maribyrnong River may have previously taken a different shape, and younger sediments have replaced the older sediments in more recent geological periods.
The site visited on this day was informally known as the Bedrock Knob (NTS grid reference: 120 342). It is in an area where patches of limestone and exposed bedrock are common. The bedrock is part of the Preca...
Gabrysch, R. K. and C.W. Bonnett. "Land Surface subsidence at Seabrook, Texas US." Geological Survey 1977: 21-74. 48 pp.
Quartzite is a non-foliated metamorphic rock. This rock is intrusive and forms when exposed to extreme amounts of heat and pressure. Over a billion years ago, there was an ocean where Kamiak Butte is. This ocean floor was made of sand, as time went on oceans receded and the exposed sand underwent processes that turned it into sandstone – or as we learned in class the process of lithification. Years later, this sandstone would morph into the quartzite that is present now.2
In conclusion these various factors explain the theory that Kaibab Plateau is actually much older than the Colorado River and that the lake overflow theory best explains the multiple processes that contributed to this natural features current landscape. Lake Bidahochi would have flooded from time to time and combined with the lowest elevation on the Kaibab Plateau, the incision would have started. Considering major rivers have the capability to erode materials such as basaltic bedrock, going through the Kaibab Plateau would have proven possible. With circular scarps retreating from the plateau, the meandering of both rivers are explained and the presence of Colorado River limestone in a sequence of ancient basins today prove the river was younger than the uplift that took place in this region.
Froede, Carl R. “Stone Mountain Georgia: A Creation Geologist's Perspective.” CRS Quartely 31, no. 4 (March 1995): 6.
Traveling north on an Indian trail, the first sign of the area’s cataclysmic past would have appeared out of place from the rolling hills typical of the Western Pennsylvanian landscape. Peering down into a valley over 400 feet deep, the mighty gorge was littered with enormous boulders, framing the Slippery Rock Creek. These relict boulders of rock types foreign to the area are known as “glacial erratics” and are indicative of the strength of the encroaching glacier. As defined by the National Snow and Ice Data Center, “Glacial erratics are stones and rocks that were transported by a glacier, and then left behind after the glacier melted. Erratics can be carried for hundreds of kilometers, and can range in size from pebbles to large boulders.
...ified rocks are usually inclined due to the structure folding and faulting because of the Paleozoic rock. (Adams, Butts, 23). Charles Butts states, “In its general relations the Paleozoic area of Alabama falls into the large geographic division of the eastern United States known as the Appalachian Highlands which extends from the Coastal Plain on the east to the Interior Lowlands of the Mississippi Valley region on the west.” (Adams, Butts, 43)
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...
Life is colorful and adventurous, especially if you belong to the military life style. Belonging to the military community for nearly two decades has given me a different outlook on each place we end up. Outdoor enthusiasts, like most military families are, make Colorado Springs a desirable duty stationed. The perfect location Colorado Springs has. The weather offers many clear, beautiful days, allowing Colorado Springs to be a playground to enjoy most of the year round. Many points of interest and vacation sights that can be done in or around Colorado Springs make it a favorite in the military community.
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
regions of the earth can indicate which rock layer is older than the other. Trilobite fossils
The first known freshwater fish, and fish with jaws appears. The Silurian strata contains fossils that indicate the previous presence of life during that period. The law of superposition was used to determine the sequence of the rocks, hence the relative ages of the rocks. When speaking of the