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    as the water that flowed from it played a vital role in the previous inhabitants of the Los Angeles area. Today‚ the river can barely even be called a river because when you look at this so called river‚ all you see is concrete and maybe a small stream of water. This will not be the case for long‚ as conservation plans are being made to restore the river back to its days of glory. Believe it or not‚ the Los Angeles river was well known by the inhabitants and was actually filled with water. The river

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    Watershed

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    of a watershed are defined by hills or mountains‚ which create a natural divider‚ because water cannot flow up that surface. These are known as “watershed divides”. An example of a watershed is the Etobicoke River Watershed. Streams of water flow downward‚ to form larger streams of water‚ which will eventually lead into the Etobicoke River. The Etobicoke River would then lead into Lake Ontario‚ which would lead the water through the St. Lawrence River‚ opening into the Atlantic Ocean. Everything is

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    Geography rivier

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    INTRODUCTION AIM: To investigate how selected parameters change downstream on the Afon Caerfanell. Hypothesis: 1. The velocity of Afon Caerfanell increases downstream 2. The velocity of the river increases down the stream as the angle of the slope increases. RIVER DEFINITION A river is the natural course of the water‚ which goes from a higher point‚ to the lowest point‚ usually the sea‚ ocean‚ lake or another river. There are few cases

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    School

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    What is a Wetland ? Wetlands are habitats that fall somewhere on the environmental spectrum between land and water. Since wetlands lie at the interface of terrestrial and aquatic habitats‚ they possess a unique mixture of species‚ conditions‚ and interactions. As a result‚ wetlands are among our planet’s most diverse and varied habitats. Wetlands are defined by the soils‚ hydrology‚ and species that occur within them. Wetland soils‚ also known as hydric soils‚ are shaped by water. These soils

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    along the numerous streams found in the estates‚ where it relaxes‚ especially in the afternoons. Those who catch fish from these streams have‚ therefore‚ to be on the look-out for cobras. All this I did not know until I came face to face with a cobra one day‚ while fishing with my brother. My brother and I were then spending our holidays in an estate where our father was employed. In the afternoons‚ my brother‚ who loves fishing‚ and I would go out to catch fish from the streams not very far from

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    watershed. • Depending upon the relief‚ geological structure and climatic conditions of the area‚ the streams form different patterns. Drainage Pattern: • Drainage of an area is concerned with the study of main rivers and their tributaries with respect to their size‚ number‚ direction of flow‚ drainage basin‚ slope of the valley. • A drainage system refers to the origin and development of stream through time. • Drainage pattern means spatial arrangement and form of drainage system in terms of different

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    north and covered by alluvial sediments. All the streams of the area are structural controlled and start from the foot of mountains and join finally Alwuha River which is the tributary to Awash River. Most of these streams join the main river at a angular pattern that show E-W running secondary faults dissecting the S-N running primary faults. Most streams of the area are intermittent except Tikur-wuha‚ which is the principal collector of streams found west of the town and downstream makes Alwuha

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    Brush Creek Lab

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    Brush Creek Report April 24‚ 2006 Surveyed March 27‚ 2006 Section V03 Instructor-Brigitte Thompson Partners-Britney and Jordan Introduction Brush Creek is a nice river that we are trying to figure out what kind of pollution and other things in the creek. The purpose is to see if Brush Creek is at the level for people to able to get into it and be safe. My hypothesis is that the creek will have little pollution around the site area. The expected outcomes are that we will find

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    water river and how they are formed due to erosion and deposition at each stage of the river? Discussion How tributaries cause the velocity to be greater? A tributary is a stream or river that flows into a main stem river or a lake. Velocity downstream increases when there are more streams feeding the main stream. The load of a river is the total amount of material carried or transported by a river. The bedload is the load transported along the bed of the river‚ mainly pebbles‚ gravel‚ boulders

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    Phto

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    The sky began to brighten in the north on that early-March day‚ as the roiled‚ greasy-gray clouds of the allnight storm began their retreat to the south and west. We sloshed our way along the bank of the creek‚ "our creek’ to us‚ a pair of ten-year-old males. We had decided on a tour of inspection of our holdings to see what damage the storm had wrought. And the creek was still there‚ still wandering its earnest‚ four-foot-wide way through the meadow‚ which was spongy underfoot with the gray-green

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