River Stinchar Research Paper

The results shows us that the hypothesis between the river Loughton brook and the erosion shows that it gets wider and deeper due to many reasons such as vertical erosion, lateral erosion, hydraulic action and abrasion of rocks.

The Devon River is clean, freshwater, and well dammed up. It is described as being a small, narrow river fringed by pine and birch (pg. 42) On the other hand, the Naguamsett River is described as muddy and

This route has a delightful blend of woodland and river scenery. We visit the cosy little village of Lartington and explore the sylvan valley of Deepdale Beck where a wide range of flora and fauna can be enjoyed.

New Kinord has not yet been excavated and many questions are still left unanswered, however the site has been surveyed by Sir Alexander Ogston. This survey identified the features of New Kinord (Aberdeenshire council sites and monuments record - Aberdeenshire - New Kinord Group). The settlement consists of five main circles that have boundaries marked out by rocks and stones, these stones are believed to be the remains of houses. There are also two paths, one path runs along the outside of the settlement and the other path separates from the outside path and goes through the middle of

The Neuse River, which means “peace” in the language of the Native Americans of the area, is located in the heart of North Carolina. The river has been flowing for over 2 million years and has helped provide energy and resources to the surrounding areas since before colonial times (North Carolina). Located just above Durham, NC where the Eno and Flat Rivers combine, the Neuse River is a vital part of a greater watershed area of central and southeast North Carolina.

Suwannee River is the place where strangers are turned into friends. Suwannee River has been around for many years, Suwannee River was formed in December 21st, 1858. Stephen Foster never visited, but, named the Suwannee River “ Swanee River” after his song “Old Folks at Home” written in 1851. “Old Folks at Home” became Florida’s official state song in 1913.

The great flood of the Mississippi river in 1927 prompted the severing of class divisions and the extension of racial oppression. The flood caused over $350 million in property damage, 246 flood-related deaths, and a home loss of 130,00. Many african americans fled north to escape the racial oppression that resulted from the disastrous flood. Police held black african americans at gun point until they agreed to help raise the levees to protect buildings and houses from rising flood waters. After African americans started refusing to work, one got shot in the back and all the african americans fled north to escape the hardships that were brought about when the river flooded. After Hoover won presidency, he did not keep his promises to ensure

Much of the diversity of Putney’s soils can be attributed to the movements of the Laurentide ice sheet that, 20,000 years ago, covered the region in several thousand feet of ice. As the glaciers proceeded south, they reconfigured the land’s surface layer by scraping away the existing soil. As the world’s climate warmed, the ice retreated, redepositing glacial till across the landscape. Topography played an integral role in the distribution of soil following glaciation. In the hills, this unsorted till, a collection of boulders, cobbles, gravel, sands, silt, and clay, began the slow process of pedogenisis (soil formation) as plants and animals brought life to this barren world. In the valleys, material was sorted by the water from the melting ice as it flowed down from the hills (Stewart 55). Below, in figure 1, the areas of unsorted till are represented in orange while areas of sorted sediment such as gravel, sand, outwashes,

Running water moves sediment in the processes of erosion and deposition, causing different types of landforms. As you can tell in the picture above, Michigan’s topography plays a huge role on where the faster and slower flowing rivers are located and the transportation of the materials in the water depends on the speed of the rivers. Erosion is the breaking down of those materials by the agent, water. The water can erode the channel laterally and vertically, in the end, making the channel wider and deeper. There are different types of erosion: hydraulic action, corrasion, corrosion, cavitation, and attrition. Hydraulic action (above on the right) takes place at rapids and waterfalls because the force of the water removes rock particles from the bed and banks of the river. A great example of this in Michigan is Canyon Falls on the Sturgeon River. At the waterfall, the water is rushing at a high velocity, especially in the spring, causing rock particles to move downstream, creating a wider and deeper river. Eventually the rivers velocity begins to decrease and particles start to deposit. This could also occur because lack of precipitation or an increase in evaporation. The deposition of materials at different locations of the river that they began changes the shape of the river, and effects Michigan as a whole in the end. The particles can travel all the way to the mouth of the river, in this case, Lake Superior, causing

The Stawamus Chief is located just about five to 10 minutes out of Squamish, giving you easy access to the crags. Take at least an hour or two to just examine the face of the monolith to get a feel for creating an appropriate ascension route. There are plenty of handholds to help you ascend, as well as tough areas for attaching

Now that the definition of stream has been defined and a few of its key characteristics discussed, the specific geographical characteristics of Plaster Creek

Scotland is located in northern Europe, sharing its only land border with England. It comprises the northern third of Great Britain and the 790 islands surrounding it. Despite its high latitude, Scotland’s climate is actually quite temperate. Distinguished by the Highland Boundary Fault, the topography is split into two distinctive regions; the Highlands and the lowlands. The Highlands, located in the north and west of Scotland, are characterized by a more mountainous terrain that is difficult to cultivate. In contrast, the lowlands, located in the south and east, are flatter, more fertile, and are home to most of Scotland’s population. Out of the country’s 7.71 million hectares of land, 5.6 million are used for agriculture. Of that 5.6 million,

Information that was used to develop my conclusions were relative to the history of Clearwater River such as the average normal discharge of 40,000cfs, the fact that the river can accommodate 55,000cfs before flooding will occur, and that with every increase of 2600cfs the river rises one foot. For example, this information helped to determine that four of the thirteen noted Peak Flood Discharges listed on the worksheet were not at flood stage as the river is able to accommodate discharges less than 55,000cfs. However, nine of the thirteen Peak Flood Discharges listed on the worksheet were at flood stage or drastically above; with the maximum rise of 17.77 feet above and a discharge rate of 101,200cfs. The average discharge rate of the top three noted floods per information on the Stream Gauge Data of Peak Flow Discharges is 93,613cfs, which is resourceful later in determining the extrapolated 75-year flood.

Further upstream we pass Oulston Reservoir, whose dam holds back the head­waters of the river Foss. However, the source of the Foss rises in Foss Crooks Wood about three-quarters of a mile east of the dam. The area around the lake is very tranquil and supports a broad range of waterfowl including mallard, coot, greylag and Canada geese, and a pair of mute

The Repton Long Barrow Site is a Neolithic burial mound in Repton, Bluffshire, U.K. The Repton area sits on top of a large, thick layer of chalk, with native soils that overlays this chalk base. Originally, this site sat isolated in the flood plain of the River Esk which lies to the south. It appears that the Repton Long Barrow is of the early Neolithic burial mound building complex that began appearing in the archaeological record of Britain in 4000 BP. The entire site itself is roughly 50 meters long and tapers from 9 meters wide in the west to 15 meters wide in the east. As seen on the overview map of the site there appears to be an indication there is a ditch that was dug around the barrow leaving the eastern edge unfinished of during of