World Geography 3202 Understand how running water acts as an agent of erosion and deposition. (Chapter 2)

1.3.1 Define the term drainage basin. (p. 26) Drainage Basin is the area of land drained by a river and its tributaries. The Amazon Basin is the planet's largest body of fresh water with 1100 tributaries 17 of which are more than 1000 miles long. Many of the tributaries begin in Colombia and Peru.

Nile River Basin The Nile river in Africa is the longest river in the world. The green are on the map marks the Nile River basin.

1. 3. 1/3. Describe the three stages in. the life cycle of a river. (P Rivers change over time and seem to go through three stages: 1st Youthful rivers 2nd Mature rivers 3rd Old rivers

Young Rivers Usually found in highland or mountain regions Steep slope (high gradient) Small volume of water Rapid flow of water Rapid erosion Narrow “V” shaped valley (usually erodes deeper not wider) Water falls & rapids common

Mature Rivers Most high relief eroded Gentler slope Many well developed tributaries Broad flat river valley Well developed flood plain More lateral erosion than vertical Meandering results

Old River Almost no slope Very little relief Elaborate meandering Often swampy areas around river Very muddy due to slow speed Most susceptible to flooding because of large flood plain.

Red River

Late River Maturity Remember the stages are not distinct. These changes occur over long periods of time.

1.3.2 Describe two ways in which water erosion occurs. (P. 31) Vertical erosion makes rivers deeper as is the case in young rivers Lateral erosion makes rivers wider leading to the meandering of mature rivers.

1.3.4 Define the term Delta. (P.32) Delta is a low lying area at mouth of river Deltas are formed by deposition of silt Deposition occurs because river slows as it enters ocean or lake

1. 3. 5. Distinguish among the terms arcuate * 1.3.5 Distinguish among the terms arcuate delta, digitate delta and estuarine delta. (P. 32) Arcuate Delta is named from the curved shape of a bow. Fan shaped Example Nile Delta p. 32

Digitate Delta Digitate Delta is a delta with long fingers of sediment reaching into the sea Example Mississippi

Estuarine Delta p. 32 Estuarine Delta is formed when river runs into bay or estuary Tidal mud flats form which can be seen at low tide Sediment deposited from river outflow and from tidal inflow

Delta Similarities & Differences Arcuate & digitate both flow into open ocean All three allow river water to flow out All have channels or distributaries cut into them by the river Differences Estuarine empties into a bay whereas other 2 empty into open water Three different shapes

Video http://www.youtube.com/watch?v=tGHAO15hROs

1. 3. 3. Examine evidence to determine the life cycle stage of a river 1.3.3 Examine evidence to determine the life cycle stage of a river. (P. 28 questions #5 & 6) Evidence to look for Slope of the river Relief of the banks Width of the valley Meandering Size of flood plain Rapids or water falls

What stage is this river in? Young Water falls & rapids Steep slope

What stage is this river? Early maturity Some meandering However still some relief Associated with mountain

What are the Stages in a River Cycle? Youth Rapid water movement Rapids & water falls High relief on banks

What kind of Delta?

What kind of Delta?

What Kind of Delta?

How are Deltas Formed Deltas are formed from the deposition of the sediment carried by the river as the flow leaves the mouth of the river in smaller channels called distributaries. Over long periods of time, this deposition builds the characteristic geographic pattern of a river delta.

Conditions Required to Form a Delta 1. The river must carry a large amount of sediments. 2. The waves or current along the coast must NOT be strong enough to remove the sediments deposited by the river, at least not faster than the river can deposit them. 3. The slope of the sea floor or lake at the river mouth must be gentle or flat. Deltas often change in size based on ocean and river currents

How Deltas are Formed http://www.youtube.com/watch?v=adHiQ6Dn8DI