A Survey On Champaign County

A Survey On Champaign County
Champaign County was first covered by the Illinois Glacier (191,000–130,000 years ago), which
leveled the region and covered it in a deposit of boulder clay. The county's topography was then
formed by the Wisconsin Glacier about 20,000 years ago. As lobes of ice from what is now Lake
Michigan crossed the county, a deep (up to 300 ft) pile of glacial soil was created and topped by
numerous moraines (any glacially formed accumulations of unconsolidated debris) forming small,
flat watersheds with no outlets. The moraines formed as the Wisconsin Glacier advanced and
receded many times over the Midwest. The Champaign moraine system now crosses the county in a
northwest–southeast direction, and between the moraines ridges are broad plains of what used to be
swampy land, most of which has since been artificially drained.
Thousands of years ago, the territory consisted of wet, marshy land. The area currently known as
Champaign County was formerly occupied by the migratory Kickapoo Indians before an 1819 treaty
granted the land to the US government. European settlement of Champaign County was restricted
by the amount of land that required drainage. Since Champaign County is situated on a large and
very flat plateau, it had virtually no natural drainage until the 1870s when settlers began building
drainage ditches. The resulting upland marsh lead to a high incidence of malaria in the region in the
late nineteenth century. About one million acres (10%) of Illinois' pre–columbian
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Essay on The Glaciers of Yosemite National Park
The Glaciers of Yosemite National Park
One of nature's most powerful and influential forces is also one of nature's coldest and slowest
processes. These great icy rivers are called glaciers and have formed some of the most beautiful
scenery on this planet. These enormous frozen bodies of water are often thousands of feet wide and
deep and many miles long. They cover millions of acres of land and drastically change the land into
beautiful mountains with many amazing features. One of the areas where glaciers have been most
influential is in Yosemite National Park in California. Here almost every glacial feature is shown.
However, before this information about glaciers in Yosemite was clear, there was the Yosemite
Controversy with ... Show more content on Helpwriting.net ...
(Muir, 1880, P. 557)
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)
Glaciers take part in two of the Earth's cycles hydrology and the rock cycle. When precipitation falls
at high attitudes where glaciers exist, the rain or snow becomes a part of the glacier and may be
stored in the glacier for up to thousands of years. Glaciers move very slow but are very important in
erosion of rocks. (Lutgens & Tarbuck)
There are different types of glaciers that exist. Valley or alpine glaciers exist in mountain valleys.
They occupy the space where a stream once was and become a glacial stream flowing down the
valley. Ice sheets are a very different type of glacier. They are much larger and are at times referred
to as continental ice sheets. They flow in all directions and cover the land they are on. An ice cap is
another kind of glacier that covers the uplands and plateaus. They cover the surface they are on
totally, but are smaller than ice sheets. The final type of glacier is a piedmont glacier. These cover
the land at the bases of mountains and

Alexandria Geography
Geography of Alexandria, Minnesota Known for the motto, "Easy to get to, hard to leave,"
Alexandria is a welcoming city full of great people and many things to do. Threw–out this paper I'm
going to go threw the physiography, culture, economy, and urban hierarchical position of
Alexandria, Minnesota, and hopefully give you a good taste of what the city is all about. Alexandria
is part of the Alexandria moraine complex, which forms the western and southern boundary of this
subsection of Minnesota. "Steep slopes, high hills and lakes formed in glacial end moraines and
outwash plains characterize this subsection (MN department of natural resources)". "The landform is
filled with ice stagnation moraines, end moraines, ground moraines, and outwash plains are major ...
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These ice chunks then melted into the holes leaving behind lakes and rivers. Alexandria is part of
Otter Tail County which has over 1,000 lakes, and the most lakes of any county in the United States.
All thanks to the vast amount of ice chunks that fell from one of the last glaciers. Although
Alexandria is home to many lakes spread out threw the city, it is most know for it's "chain of lakes,"
which includes Lake Le Homme Dieu, Lake Carlos, Lake Geneva, Lake Victoria, Lake Darling, and
Lake Jessie. Typically these lakes range from around 500–2,500 surface areas, with Lake Carlos
being the largest at 2,520 surface areas and has a maximum depth of 163 feet deep. These lakes are
deep, clean, and full of fish. Alexandria has a humid continental climate with warm summers and no
dry season. Threw–out a typical year, on average, Alexandria receives 25.12 inches of rain, and 43
inches of snow. It's average low temperature is in January is 1 degree Fahrenheit, and has average
high temperature in July at 81 degrees Fahrenheit. Obviously depending

Compass Placement Test
Four years ago, I was happily decided to go Moraine Valley College to take Compass placement test
and be able obtain the goal that I been desired to have, to be Digital Artist. Went I finish the test,
unfortinally I didn't get the results that I was expecting to have, so then my parents decide to find
certain plans for me to get better education. It was really frustrating for my parents to get me into
special programs because I keep denying going with my reckless attitude. Later, my mom usually
suggests me to go certain meetings that will help me to be independent. So she takes me in
programs&meetings as for my own good. They always propose me to have positive judgment of
myself and learn not to be afraid of own shadow. They always believe

Art Analysis: The Ice Age
Introduction
"The Ice Age". Hearing these three words, you might think about the delightful animated kids
movies that our modern culture has come to love. You might think about how old the ice cubes are
that you put in your freezer a while ago. But by the end of this section, in which you will learn about
glacial forces, your appreciation for "The Ice Age" will surpass boundaries that you never dreamt
were possible. While the average human being's understanding of the ice age may remain limited,
you may find yourself becoming what some may call "an expert" on how glacial forces shaped the
Howe Sound – Whistler region.
As the glaciers (about 2 km thick) travelled from north to south, it created many geological features
such as fjords, hanging ... Show more content on Helpwriting.net ...
Ice came out of the hanging valley and into Howe Sound. We can tell this because the granite has
striations. Glacial striations are scratches or gouges cut into bedrock by glacial abrasion. These
scratches and gouges are a result of a moving glacier. The glacial polish is a characteristic of the
rock surfaces after the glacier has passed over the bedrock. Shannon Falls is a Bridal Veil Falls,
formed by the steep drop from the hanging valley to the main valley floor usually creating cascading
waterfalls.
Erratic rock at Shannon Falls 6
In this photo, you can see some erratic rock on the way up Shannon Falls. The scale is shown by the
inclusion of a tasty Fibre 1 bar, now with only 130 calories. The erratic rock differs from the
surrounding rock, as it was brought from a distance by glacial action.
Erratic Rock at the Chief 7
This photo is of some erratic rock found in the forest along the hike up the chief. When the massive
glacier moved through Howe Sound, it brought with it this erratic rock from a long distance away.
This is why this rock appears different than the other surrounding rock. The rock was brought here
through a process known as 'plucking', which is defined as the erosion and transport of large chunks
of rocks. As a glacier moves over the landscape, water melts below the glacier and seeps into cracks
within the underlying

Summary Of America's Ice Age
The documentary "America's Ice Age" presented a lot of information, some of which I already knew.
However, I also learned a lot of new information, and still have questions about some of what I
learned. I learned that nearly two thirds of North America was covered in ice when the largest
glaciers were around, and that these glaciers contained 39 thousand cubic miles of water. I also
learned that the glaciers left chatter marks, grooves in bedrock caused by glacial plucking, on the top
of Bear Mountain, 1280 feet above sea level, which meant that 17 million cubic miles of ice covered
North America, equaling about 68 thousand trillion tons. I also learned that a coral stone quarry was
found six miles from the current coast in Florida, and one mile down from the ... Show more content
on Helpwriting.net ...
I knew that both lateral and terminal moraines are formed when rocks and sediment are moved by
glaciers, and that these moraines are left on the sides and front of glaciers, respectively. To me, this
suggests that the rocks could only be deposited in lateral moraines, or in the terminal moraines if the
glacier stops, changes directions drastically, or decreases in weight severely. If none of this occurs,
the boulders will continue to be pushed. Therefore, the boulders mark the farthest outreach of one
glacier, as long as no smaller glaciers occurred afterwards. One question that I have is: how long did
it take for the largest glaciers to retreat to approximately the size of our glaciers today, if it ever did?
Even though the movie repeatedly showed an digital animation showing the amount of snow and ice
coverage in North America, the digital animation didn't have any sort of a time scale. This animation
showed that the glaciers covered most of North America, then retreated at some point, and increased
in coverage again. I still am curious about how long it took for each of these transitions to

Personal Reflection
Before College 101, my concepts of topics such as goal setting and personal behavior were not at
the front of what my college experience would be. However, the lessons taught in this class guide
my actions in academics as well as interpersonal skills. While in high school, I did not set academic
goals for myself. Each homework assignment left more to be said, and test scores reflected the lack
of proper study habits I created for myself. A lesson that resonated with me in this course is
developing a routine of self accountability. In practicing self accountability, responsibility and goal
setting become the leading drives of achieving behavior. Before, I'd run my thought processes in
circles as to why I should not do my homework. Most of my mental energy became dedicated to
procrastination. Now, after learning about the S.M.A.R.T. objective in this class, I've created
purpose of action because it requires me to think critically about my academic and personal life
tasks. Unproductive habits such as procrastination and apathy have now become replaced with goal
setting and organizational actions. For example, I use the S.M.A.R.T. objective to plan my short and
long term goals. This includes generating short term goals that eventually lead to the fulfillment of
long term goals. Previously, I did not realize the importance of short term goals. Although I did have
long term goals, they became seemingly more out of reach because I neglected the daily small
efforts that were

How Glaciers Can Alter The Shape Of A Valley
1. Explain how glaciers can alter the shape of a valley in terms of how the valley looks before and
after the effects of the glacier.
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 ... Show more content on Helpwriting.net ...
For example the Colorado Plateau which covers a large area of Arizona, Colorado, New Mexico,
and Utah. This region consist of sediments that have mounted up to form what are now sedimentary
rocks. "Deeply–formed rocks were uplifted, eroded, and exposed for eons. By 600 million years ago
North America had been beveled off to a remarkably smooth surface. It is on this crystalline rock
surface that the younger, more familiar layered rocks of the Colorado Plateau were deposited"
(Geologic, 2014). Death Valley is part of a percentage of the Great Basin, desert streams to some
extent erode the surrounding mountains and deposited. When faulting does not end it makes the
valley deeper but at the same moment streams can fill them with sediment. Another process is when
tectonic forces create mountains. Prevailing winds, warm moist air rises, rising air generates low
pressure, which leads to precipitation and dry air descends, creating high pressure zone creates a
rain–shadow desert. (Thompson, 2007). Death Valley is one of the areas where a person can find a
rain–shadow

Kettle Moraine State Park Essay
The experiment was conducted in Sheboygan County at three locations of varying distance from
Lake Michigan, where they were surveyed for the occurrence of the invasive tree species black
locust. The first location, Kettle Moraine State Park, is located 20 miles inland west of Lake
Michigan. As its name suggests, this location has a combination of kettles and moraines. Kettles are
steep side impressions in a landscape while moraines are linear deposits that accumulated at the
edge of an ice sheet. This creates a rolling hill landscape that can create quite the diversity of
vegetation. This site was dominated by mostly sugar maple with the occasional red oak and birch.
There was very little ground coverage, due to the dense shade cast by the ... Show more content on
Helpwriting.net ...
What made this location different than the other two locations was that it was set on private land
rather than public land. The vegetation was dominated by sugar maple, with more red oaks than in
the first site. The canopy was not as closed as the first location but still consisted of coverage of
about 90%. Pleasant Mile Woods had less foot traffic than that of the Kettle Moraine State Park,
being that it is a private land, and had more wind than the previous location due to the increase in
farmland surrounding the patch of woods. The final location, Kohler–Andrae State Natural Area, is
right off the shore of Lake Michigan and the part of the site which was surveyed was the woody area
off of Black River Trail. Once again, this area was heavily shaded and dominated with sugar maple.
This site had the most foot traffic due to the occurrence of more trails and surrounding lakeside
suburbs along with having more wind than the other two locations. At each of the locations, square
quadrats of 10 meters in length were sampled using a stratified random sampling technique. At each
location, a total of 25 quadrats were analyzed leading to a total of 75 total

Teacher Interview Research Paper
Interview a Teacher
This past week, I was honored to interview my teacher, Professor Lysaught. He is a outstanding
math instructor at Moraine Valley Community College in Palos Hills, Illinois. It was a wonderful
motivational experience to hear his career change journey. Without a doubt, he instantly became one
of my mentors.
Initially, Professor Lysaught started his career as a trucking company owner. Although, his job was
great and saved enough for retirement, he pursued a further career by continuing college education.
He wanted to try something new and exciting in a different industry.
Unlike many freshmen college students at 18 years old, Professor Lysaught began his college
education in his late 30's. At 38 years old, he earned his bachelor's in Math from Circle Campus,
now known as, University of Illinois at Chicago. After earning his degree, he wanted to become a
teacher therefore, he went back to college. In 1994, he attended Chicago State University, and was
certified as a teacher instructor. ... Show more content on Helpwriting.net ...
After a few years, he left that high school and began teaching at Richard's High School. A few
months later, he realized teaching high school was not right fit for him. Although, things did not go
smooth the first few years, that did not stop him from continuing his search for the right job in
teaching.
It was on a random day throughout the week, Lysaught was browsing the morning newspaper and
found something wonderful. On the back of the newspaper, in the ad section, there was a job
advertisement for Moraine Valley Community College as a math instructor. Without hesitation, he
immediately called the school, was interviewed and got the

How To Drive Persuasive Essay
Kettle moraine is one of the best scenic drives I ever had. There is two way of this drive you can go
either north to south or south to north. As I live in south Wisconsin, we decided to go the farthest
point first so we went to Start point of north to south drive. I would advise you to Download
direction instructions PDF from these link. Kettle moraine scenic drive . The reason why to keep a
print out because if you miss any turn you will get away from the scenic drive. So better to be
prepared I lost my path twice but thank god I had the direction instructions with me. kettle–
moraine–drive–route Start point of north to south drive starts from outside of Broughton Sheboygan
Marsh Park, Tower and Wildlife Area. So we first went to check out

Minnesota Glacier Features
Features Present in Minnesota were Formed by The Wisconsin Glaciation
A glacier is a large mass of ice that flows very slowly. A glacier forms by the compression and/or
crystallization of snow that has stayed in one place year round. Glaciers can be constructive and/or
destructive. Glaciers can be constructive by leaving sediments behind, or destructive by gauging the
earth's surface. Glaciers were once present in Minnesota, thousands of years ago, and as they
retreated, they left behind large amounts of glacial meltwater and various landforms, still present
today. The Wisconsin glaciation started in Minnesota about two million years ago. The parts missed
by the Wisconsin glaciation were the Southwestern and Southeastern corners of Minnesota. There
are four lobes in Minnesota called The Rainy Lobe, The Superior Lobe, The Des Moines Lobe, and
The Wadena Lobe. The Wadena lobe advanced from Northern Minnesota. The Rainy Lobe along
with the Superior Lobe advanced from Northeastern Minnesota. ... Show more content on
Helpwriting.net ...
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

Planning Act 1990
The Planning Act, RSO 1990: The planning context in Ontario follows the rules and regulations of
the Ontario's Planning Act, R.S.O 1990. This legislation sets out the limits of how land uses may be
used to regulate growth and development activities and who may control them. The permission to
adopt local documents, such as an official plan, are contained within the Act, and its contents
provide the basis for considering provincial interest. The Planning Act outlines the rules of
stakeholder participation and procedural deadlines for each planning matter. Provincial Policy
Statements: Provincial interest is always contained in local official plans because local plans must
conform with the provincial policy statements and other provincial plans.

How Water Made A Mitten
How Water Made a Mitten When looking at a map of the United States, finding the state of
Michigan is not a difficult task. Michigan is a unique state in which it has a distinct and familiar
shape, therefore commonly referred to as "the mitten" state. In addition the Lower Peninsula that is
shaped like a mitten, the great state is composed of an addition peninsula. These two peninsulas are
surround by 5 "great lakes", which contains 18% of the world's fresh water supply. The diverse
shape and topography of Michigan can be attributed to the processes of weathering, erosion, and
deposition throughout the area. The beautiful landscape we enjoy today began to take shape over
tens of thousands of years ago under a sheet of ice.
Approximately ... Show more content on Helpwriting.net ...
These drainage basins that formed 6,000 years ago are the origin of the Great Lakes we are familiar
with today. These glacial lakes are thought to much larger than the current bodies of water
surrounding Michigan. The evidence of these lakes can be found, for example, around Saginaw bay
where there are eroded bluffs and plains located far away from the current Lake. Glaciers also left us
many moraines in the state of Michigan. Moraines are land masses where debris, carried by glaciers
has formed ridges or mounds. Moraines can be an indicator of the end of a large glacial retreat.
Moraines are created by the wasting ice sheet and are composed of glacial till. Glacial till (unsorted
glacial sediment) is laid down quickly as the glacier moves and is composed of various sediments
with many rocks and stones. In Michigan there are many famous moraines. As the lucky residents of
Marquette we can look out our windows and see evidence of glaciers because of all of our rolling
hills. Rolling landforms are a typifying aspect of a moraine.
The great lakes have certainly influenced Michigan's unique shape and distinctive mitten shape,
however those lakes aren't the only sources of water that contribute. There are over 36,000 miles of
rivers and streams throughout the state of Michigan that have also helped shape the land we enjoy
today. Rivers help shape landscapes through erosion and the transportation and deposition of

Moraine Lake Research Paper
Moraine Lake is a man made lake, located in Banff National Park, Alberta, Canada. The surface
elevation is approximately 6181 feet above sea level. The lake is home of grizzly bears, ground
squirrels, parrots and many other animals. The lake got its name from the "moraine", a pile of
glacier rocks and boulders that were formed by the Wenkchemna Glacier next to the lake. The lakes
bright, blue–green color is from the light reflecting off the "rock floor." The lake usually doesn't
open until June, when it starts melting, through early September. Moraine Lake was discovered by
Walter Wilcox, a college student at Yale, hired by Tom Wilson to help map out the area around Lake
Louise. Wilcox went out in search for a new route up Mount Temple. After

Social Security Numbers: A Case Study
great idea but the thing is with social security number is that they are very sensitive information that
is often stolen and the healthcare field is trying to move away from using social security numbers
because of identity theft. We also had to provide them with an example of how years ago one's
medical card had bits and pieces of you asocial security numbers on it that were being used to
commit identity theft. The measures we are currently taking in I–Care do exactly what number 8 on
the essential public health services states; it assured the competent public and personal health care
workforce. Following the webinar I went on another summit with my boss and colleague. Again we
would be heading for Chicago, IL at a community college by the

Facts About Glaciers Research Paper
Glaciers is familiar to most people, thinking as a big rigid piece of ice. However, under pressure,
glaciers act like a soft plastic. They can bend and flow downhill like slow–motion river of ice.
However, ice caps, ice sheets and really any masses of ice which remain year round are also
considered glaciers. For typical glacier, snowfall builds up on its surface. Overtime, all the layers of
snow press down on the layers beneath compacting the snow crystals into ice. This ice form the
main body of the glaciers. Glaciers gain ice from snowfall. They lose ice through surface melting,
melting from beneath and in some cases, by gradually flowing into lakes or oceans and breaking off
into icebergs. In winter, new snow weighs down of the glacier pushing

Reflection On Colors
I have been really focusing on colors for past 4 years, almost one–fourth of my entire life. I believe
that each of different colors can change someone's life. It sounds unreal, almost. Well, there is
someone who got affected by colors. It's me. In fact, I was not always interested in colors until
Eighth Grade. I used to be a person who did not focus on colors in everyday life, just like most
people do, but now I care colors so much because of situations I have experienced.
Thankfully, everything in the world has a color, and it used for many different purposes. Human
eyes can see many different colors because they are very sensitive. For me, the color is something
that impacts and changes my state and thoughts. I love looking at colors because it supports the
words I am saying and gives me many different moods. I remember the times that I realized how
much colors impact on me.
When I was in eighth grade in South Korea, I got a chance to visit DMZ, or 38th parallel. DMZ
stands for the Demilitarized Zone, where it divides Korea into a half. While I was in DMZ, I felt like
I was in 1970s. South Koreans lived in DMZ, but it was a lonesome place. When I came back to
school, my teacher wanted me to explain the difference between North Korea, DMZ, and South
Korea, and I could not find ways to explain. Suddenly, I thought of colors, only because they were
simple. Then, I immediately started to color the south side of Korea as Blue, North as Red , and
DMZ as Light Purple. I said that Red indicates the communism and blood. Blue as a peace, and
Purple as a confusion. Everyone can guess Red as something about violence, and Blue is something
about peace. However, people don't know what Purple describes because it can be anything. Purple
is certainly the mixture of Red and Blue, but people don't go deeper. I said light Purple because
DMZ was a very clean place. The word confusion came to my mind, because I was confused if I
saw DMZ as more of South side or North side, and I used it to explain the meaning of colors to my
teacher. It was a total success! That's how I started to use them to support my opinion. (I use color to
to give a detail often)
I went to Canada this summer, and I traveled Banff and Vancouver. In Banff,

Glacier and Citrus College Chapter Essay
ESCI 118 – Physical Geography Citrus College Chapter 17 – Solution Processes and Karst
Topography 1. How does carbonic acid form? It forms when water and carbon dioxide combine and
react. 2. What is meant by dissolution? Dissolution is the action of being dissolved. 3. What kinds of
rock are most susceptible to solution processes? Why? Limestone and dolomite are most susceptible
to solution processes because the water, which is slightly acidic, reacts with rock and dissolves the
co2 gas carrying away or dissolving some of the sediment. 4. How does the underground structure
of the bedrock influence the dissolution process? Bedrock that is made of carbonate is more ... Show
more content on Helpwriting.net ...
In an arid land, there is less precipitation than the potential evaporation which is not the case in
humid regions. 2. What is meant by an impermeable surface and how does such a surface influence
the results of rainfall in a desert? An impermeable surface cannot be penetrated by any element.
Such a surface will not allow rain to percolate into the desert soil leaving no plants with root
systems able to survive unless specifically adapted to the climate. 3. What is a basin of interior
drainage? The land is uplifted crust blocks that form parallel ranges but surface water doesn't run to
the ocean. Instead, it evaporates over time leaving a salt flat. 4. What is the difference between an
ephemeral stream and an exotic stream in a desert? An ephemeral stream is a stream that only exists
during rainfall. Exotic streams come from an origin outside of the desert. 5. Although there is very
little rainfall in deserts, running water is still the most important process of erosion and deposition in
arid environments. Describe and explain at least two special conditions in deserts that tend to
increase the likelihood of fluvial erosion whenever it does rain. Any rainfall increases fluvial
erosion. When rain does fall, this creates ephemeral streams causing water erosion due to fast forces
of water. Flash floods are possible as well creating even more erosion. 6.

Koffler Hill Essay
The Koffler Scientific Reserve at Joker's Hill is located at the western end of Oak Ridges Moraine
(ORM), hence they share common geological features. Therefore, just as in the rest of the ORM, the
parent material or bedrock of Joker's Hill is Ordovician shale and limestone (Johnson et al., 1992).
570 million years ago, what is now southern Ontario was under warm shallow seas (Rock Ontario,
1994, p.49). Between 401–417 million years ago, the sea started to recede and left sand, clay and silt
deposits in the region. With time, the materials left behind were compressed into sedimentary rocks.
After the retreat of the sea, coral reefs eventually became the coral rocks and the marine species
eventually became carbonated rocks––both types of which contain calcium. After long term erosion,
the calcium and carbonate rocks became the main composition of the limestone (Goreau, 2006).
During the Pleistocene, about 2 million years ago, the Wisconsin glacier advanced across southern
Ontario, depositing glacial sediments directly ... Show more content on Helpwriting.net ...
Then above the limestone, the deep buried sand and gravels are overlapped by the sandy gravel till.
The upper layer is deposited silt, sand and gravel (Hilts & Mitchell, 2005). They were deposited in
the Oak Ridges Moraine during the advance and retreat of the glaciers, and were eroded by the
meltwater during these processes. Nowadays, the sand, silt and gravel sediments are covered by
organic accumulations (Barnett et al., 1998). Because of the composition of the ORM, the rain water
is able to go through the the permeable Newmarket Till to the underground water system (Dyke,
1999). 70%–80% water collected in Newmarket Till goes to the northern and southern river streams
from this watershed (Gerber & Howard, 2002). Because the rivers and the lakes are all connected
with the underground water system, the pH value of the soil in the ORM, the rivers and the pounds
are close to each

Pursuing My American Dream
I am not a bricklayer, but a builder; building upon my parent's dedication to pursue a better life for
themselves and for their children. As the son of a naturalized Arab–American father, whose
Palestinian origins show me the meaning of being a minority, and a Palestinian immigrant mother,
who inspires me to continue pursuing my aspirations amidst the daunting and unknown road ahead,
I endlessly strive to achieve my American dream.
Working with the financial aid department at Moraine Valley Community College, I was eligible to
receive a few grants; I decided to take out loans as well, to make sure I would not only be able to
complete my education once I began school, but also not to burden my family's miniscule resources.
As a first generation Arab ... Show more content on Helpwriting.net ...
Despite the ongoing pension funding issue, these teachers were tremendously grateful that they had
an advocate fighting for their rights. That advocacy experience was when I realized that providing
legal services to persons of limited means was my passion. I am always reminded of how Jackie
would open and close her speeches with words from John F. Kennedy: "Let us think of education as
the means of developing our greatest abilities, because in each of us there is a private hope and
dream which, fulfilled, can be translated into benefit for everyone and greater strength for our
nation." A unique moment still influences me; as we were preparing to leave one of our roundtables,
a retired 11th grade chemistry teacher told me that she was going to share this information with her
friends and colleagues. I did not think much about what she told me at that moment, however as I
was riding the train on my way home, I pondered her exact words. Thinking to myself, I hoped that I
encouraged at least one student at the Aid Alliance, who one day might champion for the next
generation of underprivileged

The Importance Of Competitive Cheerleading
Competitive cheerleading is very demanding both physically but also mentally. Men and women
have to pretty much put their life the hands of their team. When flyers on the team are being tossed
into the air they have to trust their team to catch them and not drop them on their face. If hitting the
ground wrong it could end your season in the sport or get security hurt. So people might say you
could get hurt too bad you just have to get back up, brush it off, and start again. However like any
fall it could be fatal it you hit the ground just right. Thank makes you think how many people do
you know that you would be will to put your life in their hands. When competing at that level of
cheerleading how could not call it a real sport. In Kettle

Large Lake Essay
Michigan's literally translation from the Ojibwa nation is "Large Lake" but the natives know it by
the "Great Lakes State." These names come from the history and prominence of the water features
throughout the state. The beginning of shaping the current landscape of the state was with the
glaciers. Glaciers are large bodies of ice that travel across land leaving behind deposits and
reshaping the land as it moves. The most common features are moraines, drumlins, eskers, till
plains, valley trains, kames, and kettles.
Moraines are "are long lines of ridges and festoons of hills composed essentially of boulder–clay or
till which was dumped from the ice front during relatively long intervals when the backward melting
was equal to the forward ... Show more content on Helpwriting.net ...
The present day physical landscape of Michigan was not accomplished until the late Pleistocene.
The Midwest was dominated by four massive glaciers with Michigan's average glacial drift ranging
from 200 to 300 feet and a thickness of 1,000 feet in some locations (2017, DNR). Michigan's
glacial deposits are estimated to three hundred over the entire state (2009, Berquist).
The melting allowed the liquefied water to carry the various rocks and soils in landscape deposits.
As the melting increased, the weight of the glacier on the Michigan basin was decreasing. With less
pressure on the basin, it began to rebound into its original shape while maintaining the integrity of
the glacial deposit landforms. About fourteen thousand years ago, the Wisconsin Glacier covered the
entirety of Michigan with its "northernmost head" at the Hudson Bay and stretching to the "banks of
the Ohio River" as shown in Figure 1 (2017, DNR). These glacial movements were guided by the
pre–glacial rivers that were further carved by the massive ice sheets to carve valleys. Although
drainage was occurring in the Great Lakes region during the pre–glacial area, it is nearly impossible
to reproduce its exact original features (2009, Berquist). Many lobes of the glaciers sculpted the
current boundaries of the Great Lakes. One of these was the Huron,–Erie Lobe which shaped the
basins of lakes Huron and Erie (2009, Berquist). Lake Superior was modified through

Ohio's Ice Age
Although difficult to imagine, Ohio has at vari– ous times in the recent geologic past (within the last
1.6 million years) had three–quarters of its surface covered by vast sheets of ice perhaps as much as
1 mile thick. This period of geologic history is referred to as the Pleistocene Epoch or, more
commonly, the Ice Age, although there is abundant evidence that Earth has experienced numerous
other "ice ages" throughout its 4.6 billion years of existence.
Ice Age glaciers invading Ohio formed in cen– tral Canada in response to climatic conditions that
allowed massive buildups of ice. Because of their great thickness, these ice masses flowed under
their own weight and ultimately moved south as far as northern Kentucky. Oxygen–isotope analysis
... Show more content on Helpwriting.net ...
Lake deposits are primarily fine–grained clay– and silt–size sediments. The most extensive area of
lake deposits is in north– ern Ohio bordering Lake Erie. These deposits, and adjacent areas of wave–
planed ground moraine, are the result of sedimentation and erosion by large lakes that occupied the
Erie basin as Wisconsinan–age ice retreated into Canada. Other lake deposits accumulated in stream
valleys whose outlets were temporarily dammed by ice or outwash. Many outwash–dammed lake
deposits are present in southeastern Ohio far beyond the glacial boundary. Peat deposits are
associated with many lake deposits and formed through the accu– mulation of partially decayed
aquatic vegetation in oxygen–depleted, stagnant water.
The term glacial drift commonly is used to re– fer to any material deposited directly (e.g., ground
moraine) or indirectly (e.g., outwash) by a glacier. Because the ice that invaded Ohio came from
Canada, it carried in many rock types not found in Ohio. Pebbles, cobbles, and boulders of these
foreign rock types are called erratics. Rock collect– ing in areas of glacial drift may yield granite,
gneiss, trace quantities of gold, and very rarely, diamonds. Most rocks found in glacial deposits,
however, are types native to

Oak Ridges Moraine
The Oak Ridges Moraine is landform located in south central Ontario, Canada. It expands from
Caledon and Rice lake river. Furthermore, it covers about 1,900 kilometers in Geographic area and
is the most important landforms in Ontario. The Oak Ridges Moraine is made out of 4 wedge shaped
structures running east to west ( Uxbridge, Pontypool, Rice Lake, and the Albion Hill wedges ). The
wedges are separated from east to west and was formed by sedimentation, the Rice Lake wedge is
separated from the other three moraines and is south of Rice Lake. The moraine is made out of
major geophysical structures that shape the Oak Ridge Moraine. The western portion of the moraine
is by the Niagara Escarpment, the escarpment channels give a way for a

The Wisconsin Glaciation: The Formation Of Glaciers
Glaciers are made up of fallen snow, that over many years compresses, into large, thickened ice
masses. Glaciers begin to form when snow remains in the same area year round where enough snow
accumulates to transform into ice. The sheer weight of a thick layer of ice, or the ice's mass, causes
glaciers to flow very slowly. Movement along the underside of a glacier is slower than movement at
the top due to the friction created as it slides along the grounds surface, and in some cases where the
base of the glacier is very cold, the movement at the bottom can be a tiny fraction of the speed of
flow at the surface.
Glaciers were once present in Minnesota thousands of years ago, and as they retreated, they left
behind large amounts of meltwater and various landforms still present today.
The Wisconsin Glaciation began seventy five thousand years ago. Four lobes from the Laurentide
Ice Sheet in nornether Canada moved into Minnesota. The Wadena lobe, Rainy lobe, Superior lobe,
... Show more content on Helpwriting.net ...
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

How Did Connecticut Get Its Shape
Connecticut got its shape in three major ways. Those are ways are glaciation, plate tectonics, and
weathering and erosion. One major way Connecticut got its shape was from glaciation. For example,
glaciation formed Jobs Pond. Jobs Pond is a giant kettle hole, which is a depression caused by the
impact of a massive chunk of ice, or a glacier. According to The Mystery Of Jobs Pond, geologists
and hydrologists the water level rises and falls with the groundwater level in the area, because
porous sand and gravel make up the bottom of the pond. A kettle hole is formed by a glacier, so
glaciation formed Jobs Pond. Another landscape formed by glaciation is recessional moraines. A
recessional moraine is a pile of rocks left behind when a glacier recedes, or moves back. As a glacier
moves, it picks up rocks in a process called plucking. Then, as the glacier starts to melt, it recedes.
As it does this it drops off rocks, forming a recessional moraine. Recessional moraines, formed from
glaciation, are found all along the Connecticut shoreline. ... Show more content on Helpwriting.net
...
For example, The appalachian Mountains were formed by a massive continental collision over 300
million years ago. According to page 88 in my science notebook, the rocks in the Chattooga River is
evidence of the continental collision. Mountains are formed when two continental plates collide, and
form the mountains. The Appalachian mountains, were formed during Pangea. The North American
Plate and the African Plate collided. When this happened the Appalachian Mountains were formed.
These mountains then grew bigger, but as soon as it started growing, it also eroded. Erosion and

Minnesota's Glaciers
The Wisconsin Glaciation of Minnesota
A glacier is a large body of ice that moves slowly across land and are formed by there being a higher
snow gain rather than a snow melt. Glaciers move by a small amount of ice melting and the glacier
sliding. Glaciers can help and destroy the landscape in front of them but they can also shape the land
into something amazing. Glaciers were once present in Minnesota thousands of years ago and
played a massive role on the landscape we live on today, and as they melted they left behind large
amounts of water and formations. The glaciation is very confusing to those who don't know about
glaciers so here is some background information. The last glacial advance started about 75,000 years
ago and the last ... Show more content on Helpwriting.net ...
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

Eastern Cascade Biome Comparison: Anthropological Analysis
and come apart and allow for countless sheets of lava to be transferred out over the land (Hay,
1992). Through time the ice caps frequently collected and spread over enormous extents in North
America. In this timeframe, movements to the south would occur making the ice push and relocate
expansive quantities of soils and rocks. This movement effected how the great glacial streams would
flow (Hay, 1992). With the extremely large rains and glacial ice melting valleys and flooding played
a great role in the Pleistocene.
Eastern Cascade Biome Comparison
When looking at specifically Washington States Eastern Cascades and how the Pleistocene affected
the biogeography, there are several areas worth investigation. Leavenworth would be one of note.
This Eastern Cascade location has shown evidence of an east–flowing cascade glacier system during
the Pleistocene. So such a place is key to seeing flora and fauna comparisons. During the Mount
Stuart glaciation phase, it is thought that glaciers built up copious amounts of moraines in Icicle
Creek valley and several of the other southern tributaries in the area. One at the mouth of Rat Creek
was described as a "perfect horse shoe shape" (PORTER, Et al., 2004). The idea here is that seeing
direct evidence of glaciation in the Eastern Cascades proves that there is no ... Show more content
on Helpwriting.net ...
This area, according to figure 3, shows signs that the area was likely a subalpine parkland in the
areas not covered by the ice sheet or other kinds of permanent ice. In the upper areas of elevation
around 3300–4300 meters, in the Central and Eastern Cordillera and along the slopes of the Sierra
Nevada de Santa Marta; a pluvial alpine tundra occurred as well as subalpine forests (Hooghiemstra
Et al., 2004). This is very comparable due to the similar Pleistocene climates, even though they are
rather different in their current lower elevations (Hooghiemstra Et al.,

City Council Meeting Essay
What exactly goes on in your local city council meeting? On October 22nd, I visited the Moraine
City Council, located in the Moraine Municipal Court Building, to find out. The meeting started at 6
p.m. and lasted about thirty minutes and they are held the second and fourth Thursday of every
month. The agenda, which was found at the entrance of the meeting room, listed all the topics that
would be covered. In this essay, I will cover the people in attendance/process, the items discussed,
and what I learned from this experience. The process involved is fairly simple and there are a few
important people who play a large role. The meeting kicked off with the Clerk of Council, Ms.
Werbrich, doing roll call. She called each member's name to make sure they were present. The Clerk
of Council then began addressing the issues listed on the agenda and the mayor, Ms. Allison, would
then ask for the issue to be motioned, which seemed to be her main job. The council members would
then say either yes or no on whether to discuss the topic. If the a majority said yes, the ... Show more
content on Helpwriting.net ...
I was able to learn about many issues which our city is faced with, issues of which they and the city
must solve. There were more issues than I would have ever imagined. I believe this meeting covered
almost ten issues, even though not all issues were resolved this meeting; a lot of thinking goes into
the solution of each issue. Also, prior to this, I had no clue how our local police departments paid for
replacement equipment. I mean, I figured the taxpayers provided the funding, but I had no clue it
went through the council. This also applies to many things. I had no clue our local government had
such a large impact on the community. I always thought it was the federal government that had the
largest impact and influence on the community. It was definitely a unique experience, which was as
interesting as any teenager would imagine it to

The Physical Geography of Kalamazoo
The Physical Geography of Kalamazoo
Physical Geography of Michigan Kalamazoo, Michigan has been around officially around since the
eighteen thirties. It has long since a agricultural producer and has been growing steadily throughout
the years as a metropolitan area. This paper will focus on the actual land itself mainly looking at the
geological history, glacial formations, streams, wind landforms, groundwater, climate, soil,
vegetation, agriculture, tourism, and a small summary of the community of the area of Kalamazoo.
For the first paragraph we shall have a quick focus on the geological history of the area of
Kalamazoo. The main deposits and formations of the Kalamazoo area where formed during the
Wisconsin glaciation period. Now the deposits are actually due to two lobes during this period, the
lobes are the Lake Michigan and Saginaw lobe. Kalamazoo is actually know as a "reentrant district"
due to the presence of two different lobes materials. During the middle of the Wisconsin Ice Age the
Lake Michigan lobe was extending southeastward, while the Saginaw lobe was extending
southwest. With the meeting of the two lobes an interlobate developed between the terminals of the
lobes. It is also thought that the two lobes overlapped each other. With the Saginaw lobe covering
the Kalamazoo area first and then retreating while the Lake Michigan lobe then covered the area.
There are also some bedrock formations in the area as well, these formations were established
during

Breaking Point In The Film Touching The Void By Kevin...
In the film "Touching The Void" by Kevin Macdonald, the idea of Breaking Point is conveyed
through film techniques in the moraine dam scene. The idea of breaking point is conveyed through
talking–heads, Music, Editing, and Camera Angles (Dutch Angle). The effect of these film
techniques are used to strongly convey the main character's (Joe) breaking point. During the
interviews of the film, talking–heads were included to show Joe's breaking point. While Joe retells
his memory in the moraine dam, he becomes emotional and wipes off a tear. During this moment, an
Extreme Close Up was shot to capture the essence of his emotion clearly. Through the Extreme
Close–Up, It shows how horrible and dark the experience in the moraine dam really was for Joe. "I
stopped looking at the watch, and everything started falling apart'' The Extreme Close–Up and
quotation clearly shows Joe's breaking point in the Moraine Dam. ... Show more content on
Helpwriting.net ...
When Joe struggles to get across the moraine dam, he suddenly hears music from Boney M that
blasts his ears with intense volume, Joe explains that he doesn't like Boney M and he has no control
over the looping music in his head, showing how weak and agonised he is at this point and his
inability to control himself mentally. During the voice–overs, the background music is layered with
soft, long and sustained violin tunes. "That moment when no–one answers the call... I lost
something. I lost me.'' The music style and quote further exemplifies the emotion, depressing
atmosphere and Joe's breaking

Wisconsin Glaciation Research Paper
The Wisconsin Glaciation had effected Minnesota heavily, like it formed moraines that cover many
different counties. The glacier also left lakes and drumlins. This glaciation was the most recent
Glaciation in Minnesota, it still happened tens of thousands of years ago.
The Wisconsin Glaciation started in Minnesota about 75,000 years ago. This glacier was fully
melted about 12,000 years ago, when the climate began to heat up. The glacier was at it maximum
about 14,000 years ago. This glacier travel so far south that had made its way to the middle part of
Iowa. Even though the glacier flattened out much of Minnesota it missed parts in Middle East and
southeast parts of Minnesota. Some lobes that were present in Minnesota were the Des Moines, ...
Show more content on Helpwriting.net ...
Till is a mixture of many different sediment sizes all mashed together. Till is usually located on the
sides and the end of a glacier. If a glacier makes enough till it can be called a moraine. A moraine is
a large ridge of till that could stretch counties to states long. One common moraine is the Mille
Lacs/Right/Cromwell/Highland moraine. Another feature made from till is a drumlin, a drumlin is a
hill of till that faces the direction that a glacier came. Two drumlin fields are the Pierz and Toimi
drumlins. When glaciers melt they leave behind kettle lakes. The kettle lakes are often formed in the
depressions that the glacier made and then melted in. The kettle lakes are most common in
northwestern Minnesota. The Wisconsin Glaciation may of happened a long time ago but it helped
form this great state of Minnesota. The melting of the glacier made ten thousand lakes, making
Minnesota a unique state. After the glacier had melted it left huge features that would pathe the way
for settlers. Some features are the ten thousand lakes or the Mille Lacs moraine. Learning about
glaciers and erosion can tell us a lot about our past and what animals roamed here in the northern
United

The Wisconsin Gliciation: The Last Glaciation In Minnesota
The Wisconsin Glaciation was the last glaciation in Minnesota. The rolling hills of Minnesota are all
attributed to the Wisconsin Glaciation. All of the lakes of Minnesota are also he because of the
Wisconsin Glaciation. The beginning of the Wisconsin Glaciation started about 75,000 years ago.
The glacial maximum happened 14,000 years ago. The glacier was completely melted in Minnesota
11,000 years ago. There were four lobes in the Wisconsin glaciation. The Des Moines lobe extended
into southern Minnesota, but missed the southeast and southwest corners of the state, which are
known as Driftless areas. The extent of the Des Moines lobe to the south of Minnesota is marked by
the Bemis moraine line. A glacial lake formed

The Impact Of The Human Impact On Glaciers
In this letter, I will be telling you about the human impacts on glacial changes and about glaciers
itself. By the time you will be reading this, the world's environmental factors would have changed
greatly. Now you must be thinking that I'm crazy, but glaciers actually existed and there is evidence
of their existence. There are many pieces of evidence that support the evidence of glaciers, but the
following are some of the more common pieces of evidence. Glaciers are a slow moving ice–masses
that are formed by the accumulation, compaction, and recrystallization of snow on mountains or
near the poles (extremely cold regions). When the water solidifies, it pushes pieces of rock in the
outward direction. The rock is at that point plucked and carried out by the streaming ice of the
moving glacier. With the weight of the ice over them, these rocks can scratch profoundly into the
underlying bedrock, making long, parallel grooves in the bedrock, called striations. Striations are
evidence of glaciers because they indicate the direction in which the ice is moving and it can
probably tell us how far a glacier has moved in a certain period of time. Waterfalls are also subtle
pieces of evidence that glaciers existed. Hanging valleys are typically formed when the main valley
has been widened and deepened by glacial erosion, leaving the side valley cut–off from the main
valley. Smaller tributary streams flow into the main glacier to form smaller and shallower U–shaped
valleys. Larger

Stories of Our Earth: Causes for Ice Ages and Their...
Will the ice ages happen again? Ice Ages are dramatically landform changing points in time when
the temperatures around the world, including the atmosphere and the surface of the Earth, are
consistently cold for spans of over thousands of years. Ice ages force a glacial period (when thick,
large sheets of ice cover a massive portion of the Earth's northern hemisphere). Studies show that ice
used to cover approximately 30% of the Earth during our last ice age. A point in time can be
classified as an ice age as long there are permanent ice sheets, ice glaciers of size over 50,000 km2.
That's roughly 9 football fields. So technically, we're in the middle of an ice age because we still
have large ice sheets such as Greenland and Antarctica. ... Show more content on Helpwriting.net ...
Changes in land formations during the ice ages happened in different ways, but most of them relate
to the process of glaciation. During the Ice Age, glaciation, the process of being covered by ice
sheets took place over giant land masses and entire continents which is known as "continental
glaciation". As this large scale glaciation took place, changes in land formations occurred, that of
which are uncommon to be formed today. They include moraines, drumlins, kames, eskers, and
Kettle Lakes. Most of the evidence that was discovered has to do with the Earth's geography, the
physical features of the Earth. The ways these glaciers affected the landscape were separated into
three different categories: erosion, transportation and deposition.
Moraines are rocks and debris carried by glaciers, which are large masses of flowing ice and water
that flow because of their heavyweight, and put into areas, especially near where they are rarely
found. From this point, the debris that the moraines consists of can be classified as till, which is
unsorted, randomly arranged material mixed together. This is similar to when sand is washed by sea
tides, and the sand is shaped in to a hill near the shore. Most of these are created by transportation of
the debris and deposition.
There are many different types of glacial moraines including ground, lateral, medial,

Glaciers-The Identity Of A Glaicer
The Identity of a Glaicer Glaciers have helped define the topography of earth for many years. A
glacier is a large mass of ice that has been compacted of snow and ice for a long period of time. The
ice age we will be focusing on is the Pleistocene era, which was "a period that began about 2.5
million years ago and ended about 10,000 years ago" (513). This was the most recent ice age where
it helped formed our present–day lands. During this time, ice covered about 19 million square miles
which was about 1/3 of earth's land surface (515). Many parts of all the continents were covered
with ice and that had a great effect on our topography due to the glaciers it created. The two primary
types of glaciers are continental ice sheets and mountain ... Show more content on Helpwriting.net
...
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

Personal Narrative: The Imposing Team Kettle Moraine
The day was loud and cold. The air was lingering with the smell of hotdogs from the night before.
Everyone was cheering as the game was about to begin. The stands we're full upon the kick to begin
it all. There were people on both sides cheering for their team. The whole first quarter of the game
we played was blank, there was no scores or anything that big of a play. But in the second quarter
they opposing team Kettle Moraine took over. They were just driving on us the entire quarter. With
the ending score of the half them up 14–0. During the break in between 2nd and 3rd quarter
everyone was angry about how we weren't able to stop them. After are stretches we got ready to play
again. Upon the kick being received in 3rd quarter it was about

Barrier Beaches of Long Island, NY Essay
Barrier Beaches of Long Island, NY There are many different types of coasts that exist throughout
the United States. The south shore of Long Island has a unique types of coast known as a barrier
beach. Barrier beaches are long narrow land forms that are composed of sand and other lose
sediments. These sediments are brought together by the actions of waves, currents and storm surges.
Barrier beaches are subject to constant changes by the same forces. Sand is constantly eroded in one
area an deposited in another. Barrier coasts are important for a number of reasons; they protect the
mainland of Long Island from the open ocean and flooding during storms, for recreational use and
the unique ecosystems which exist on barrier ... Show more content on Helpwriting.net ...
Long Island is famous for its sandy ocean beaches. Between the barrier beach and the main coast is
the Great South Bay. The beaches and dunes have very different characteristics. The sandy beach is
the junction of land and ocean. The sandy beach consists of two zones, the swash zone and the drift
line. The swash zone is the area of wet sand, caused by the incoming wave. The drift line is formed
by the dead seaweed and other aquatic plants. Behind the sandy beach is the primary dune. The
primary dune's main function is to absorb the force of the ocean and protect the great south bay and
the island's main coast. In some cases secondary dunes form. These dunes are behind the primary
dune and are therefor protected from the ocean. This provides the stability necessary for plant
growth. Many time a maritime forests will form on secondary dunes. Barrier beaches are not static,
they are constantly being changed (Coastal Change ) by the forces that formed them; waves and
wind. One change effecting barrier beaches is they are moving closer to the main coast. This
movement is caused by the rise in sea level. As the sea level rises waves crash higher and higher
upon the beach, as they do this the dunes are pushed back. There are also seasonal changes in the
barrier beaches. During stormy seasons sand is removed from the beach and deposited off shore on
the longshore bar. During calm season waves redeposit sand upon the beach and the beach grows.

A Survey On Champaign County

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