Teacher as a Professional

Out wash has small sediments sorted in layers, and Till has large sediments not sorted into any layers. Till can leave behind features like Kame, Drumlins, and Moraines. Drumlins are elongated hills of till. Drumlins can be found in Central Minnesota and/or South of Brainerd. Moraines are very large ridges of Till. Moraines can be found in West/Central Minnesota. Outwash can leave features behind like Outwash Plains and Eskers. An Outwash plain formed by melt water of a glacier. Outwash plains are important because they are very great for farming which is a huge part of America. Glaciers can leave behind features like Kettle Lakes. Kettle Lakes formed by ice chunks falling off the main glacier, causing an indent on the earth's surface. Then the ice chunk will melt causing the hole to fill up with water. Most of Minnesota’s Kettle lakes are in Moraine/Terminal Moraine

In a study done by Huston et al. (1989), it was found that television was the center of the majority of children’s time and attention. This particularly applied to children in low-income and minority families who did not have the financial resources to provide other activities and media sources to occupy their children’s time. This article stated that television has an impact on children in three main ways: as an educator, a source for social learning and a way to advertise and sell products. The article also discussed many of the public

Outwash and till are similar but different at the same time and this is why they are both deposited by glaciers, but the way they are deposited is what makes them different. Till is simply the sediment left by the ice, outwash is deposited by the running water coming off of the melting glacier. Because water can sort sediment, and ice cannot, that is why the till is unsorted. Sorting just means when the rocks are sorted by size, bigger pieces together on the bottom, smaller pieces together on top. Glaciers are constructive and deconstructive they are deconstructive because they tear up land and the glacier does not stop for anything but it is easy to avoid. Glaciers erode the land and create landforms such as kames, eskers, and drumlins those terms will be explained a little bit later. Glaciers create valleys by shearing away the mountainside and moving it away. Some of the landforms that glaciers produce are drumlins, terminal moraine, outwash plain, and an erratic. Drumlins are elongated, teardrop-shaped hills of rock, sand, and gravel that formed under moving glacier ice. A terminal moraine is where the glacier reaches its max and starts receding making a deposit of till. An outwash plain is a flat area made by meltwater carrying outwash from the leading edge of the glacier. An erratic is a rock or boulder carried from a place where the Rock is common to an area where the rock is not

E. Choose five of the following terms and give a brief definition of each. (2 points each, 10 total)

a) Mountains were formed by the movement of the Earth’s crust. b) The Ice Age left glaciers in most of northern Canada and America. (1) Lakes formed from melted glaciers. (2) Basins were also formed. B. People the Americas 1.

A glacier occurs when the climate of an area is so cold that new snow does not completely melt each summer and more snow is added in the winter. After many winters the accumulation of this snow becomes compact and re-crystallizes, thus forming a glacier. Currently, glaciers cover about ten percent of the Earth's surface. Yet, in the past, glaciers covered much more land and were thousands of meters thick. (Tierney)

The moraines is a “general term for glacier-deposited landforms composed of till” (526). The features usually are irregular and is normally longer than wider. The three types of moraines in glacial deposition of ice sheets are terminal, recessional and ground. Terminal moraine is the front part of a glacier where all the power is. Although glaciers may appear to stop moving forward, the internal part of the glacier continues to give strength to its movement. Recessional moraine is right behind the terminal moraine where the ice would spread out putting pressure out to the edges in bulges. The last type is called ground moraine and that is when “large quantities of till are laid down from underneath the glacier rather than from its edge” (527). A feature we see from the glaciers deposition is an “elongated hill” (527) called a drumlin. These long, small hills that are usually in groups, are much smaller than moraines but still made predominantly of

Chasing Ice is a modern documentary about the human impact on the Earth’s glaciers. Following James Balog and his team the Extreme Ice Survey (EIS), the group aims to provide visible evidence of human impact on the Earth’s glaciers, as they trek through harsh conditions in Alaska, Greenland, and Iceland.

Can you ever find some things for entertainment, information and communication all at once other than television ?. The answer more likely is no. As the matter of fact, researcher show that ninety nine percentage of household that possesses at least one television. Additionally the average of youth and adult spend time watch television is more than one thousand hour per year. These number is higher than everyone expect. With those statistic show above, its prove that television is one of the most important material to human life in both sociology and psychology. Since the television was developed, human life was changed enormously. In brief, without television, human life would take a slow process in development

Many locations around the world in places where its snows throughout the year temperature stays cold and frosty. This will cause snow not to melt but sometimes creates a firn. When the snow gets suppressed deeper in the snowpack it can turn in to a glacier ice. “Glacier is massive, long-lasting, moving mass of ice compacted snow and ice” (Thompson, 2007). These gigantic moving mass can only be made on land where the quantity of snow is more abundant than the snow that had previously melted in the summer. Glaciers are influenced by geologic forces, temperature changes, and snowfall (RioLearn, 2016). There are two types of glaciers the first type is an alpine glacier and the

The Wisconsin glacier began began 75,000 years ago. 4 lobes from the Laurentide Ice sheet in northern Canada. They all went through Minnesota and their names were Superior lobe, Rainy lobe, Wadena lobe, and Des Moines lobe. 14,000 years ago the last glacier occurred and 11,000 years ago the was when the ice completely

They also make a lot of things to. Till is an unsorted and non-layered sediment, and outwash is a sorted layered sediment. You can tell tell the difference because outwash is nice, sorted, and neat. Till is like garbage just thrown to the side. Outwash is deposited by meltwater, and till is dropped off directly by the glacier. Glaciers are both destructive and constructive. They are destructive because as they move they tear down anything in their path. They are also constructive because they make stuff to like drumlins. Drumlins can be found in Brainerd, and Central Minnesota. Terminal Moraine can be found in Itaska, and St. Croix. Outwash Plains can be found in Rosemount, and Jackson Pine Barrens Woodlands. They are found in Central

Glaciers are large bodies of ice that are constantly moving. They cover 10% of the Earth's surface and are stretched across 40 different countries, among which are Greenland, Canada, Iceland, US etc.

These formations are made up of sediment deposits called till and outwash. Till is a large unsorted, and unlayered sediment dropped off directly by the glacier. Till cannot be moved because of the massive size. Outwash is small layered, and unsorted sediments deposited by meltwater flowing from glaciers. Outwash is small enough to be carried away. A drumlin is an elongated hill with steep sides facing the direction the glacier came from. You can find drumlins in Otter Tail county located in northwestern Minnesota. A moraine is ridges of till that mark glacial movement. As the glacier scrapes along, it tears off rock and soil from both sides of its path. The most common part of Minnesota that has Moraines is located in West central Minnesota. Kettle lakes form from ice. A chunk of ice falls off making an indent on the ground, then when the ice melts it makes a kettle lake. Kettle lakes are common all over

Glaciers are essentially frozen rivers. They are common in the Northern Hemisphere as well as at high altitude.