agents of gradation

39

Upload: sen

Post on 15-Jan-2016

521 views

Category:

Documents


29 download

DESCRIPTION

Agents of gradation. Introduction. Gradation changes surface features of the land. It involves erosion, transportation and deposition . It involves process like degradation, aggradations and weathering. Work of river Or Running water. Introduction. - PowerPoint PPT Presentation

TRANSCRIPT

Page 1: Agents of gradation
Page 2: Agents of gradation
Page 3: Agents of gradation

• Gradation changes surface features of the land.

• It involves erosion, transportation and deposition.

• It involves process like degradation, aggradations and weathering.

Page 4: Agents of gradation
Page 5: Agents of gradation

• Rivers originate from hills or Rivers originate from hills or mountains.mountains.

• They have different amount of water They have different amount of water In different seasons.In different seasons.

• Some rivers water through out the Some rivers water through out the year and some don’t.year and some don’t.

Page 6: Agents of gradation

• They are known as perennial and non-They are known as perennial and non-perennial rivers.perennial rivers.

• They are the most powerful agent of They are the most powerful agent of gradation.gradation.

• The work of the running water is also The work of the running water is also called as fluvial process.called as fluvial process.

Page 7: Agents of gradation

RiversRivers

Page 8: Agents of gradation
Page 9: Agents of gradation

First stageFirst stage

• In the first stage the river has it maximum speed so most of the erosion is done in this course. It forms rapids, waterfalls, gorges, canyon, V-shaped valley and erodes it bed during the upper course.

• In the upper course of a river valley the land is highest, steepest and most exposed

Page 10: Agents of gradation

WaterfallsWaterfalls

• Waterfalls occur where the bed of a river becomes suddenly steepened.

• Waterfalls are caused by differences in rock hardness.

• E.g.., Niagara falls, the great kaietur falls.

Page 11: Agents of gradation

waterfallswaterfalls

Page 12: Agents of gradation

The Niagara Falls are

voluminous waterfalls

on the Niagara River,

straddling the international

border between the

Canadian province of

Ontario and the U.S.

state of New York.

Niagara falls Niagara falls

Page 13: Agents of gradation

Victoria fallsVictoria falls

The Victoria Falls or Mosi-oa-Tunya (the Smoke that Thunders) is a waterfall located in southern Africa on the Zambezi River between the countries of Zambia and Zimbabwe.

Page 14: Agents of gradation

RapidsRapids

Page 15: Agents of gradation

Some examples for RapidsSome examples for Rapids

Page 16: Agents of gradation

CanyonsCanyons

• Where a river derives its water from snow-melt mountains and flows through arid areas and is able to maintain its erosive power ,canyons are formed.

• E.g., grand canyon ,Rhine George etc.

Page 17: Agents of gradation

GorgesGorges

Page 18: Agents of gradation

GorgesGorges

• Some valleys have very steep sides and are both narrow and deep. These are called gorges.

• Some valleys have very steep sides and are both narrow and deep. These are called gorges.

Page 19: Agents of gradation

Swan gorgesSwan gorges

Page 20: Agents of gradation

Interlocking spursInterlocking spurs

• An interlocking spur is a natural geographical feature which occurs in a river's upper course, where upward erosion is the dominant force in determining the river's course.

Page 21: Agents of gradation

Interlocking spursInterlocking spurs

Page 22: Agents of gradation

Second stageSecond stage

• In the middle course the river's speed becomes slow that it was in the upper course. The river deposits, erodes all the material along its way.

• The main features formed by the river in its middle course are meanders, oxbow lake and flood plain.

Page 23: Agents of gradation

MeandersMeanders

• Meander is a loop-like bent in a river. As a river nears the sea it winds up, forming regular horseshoe shape bends, these bends are called Meanders

Page 24: Agents of gradation

MeandersMeanders

Page 25: Agents of gradation

Flood plainsFlood plains

• Flood plain is a broad flat river valley in the lower reaches of a river.

• A river often flows over wide plains of sediments or alluvium. This alluvium is washed down the hills and spread out over the valley floor in times of flood

Page 26: Agents of gradation

Flood plainsFlood plains

Page 27: Agents of gradation

Ox-bow lakeOx-bow lake

• Oxbow lake is a crescent - shaped lake on a river floodplain. As the river wears away on the outside bend of the meander, the neck of the meander gets continually narrower.

Page 28: Agents of gradation

Ox-bow lakeOx-bow lake

Page 29: Agents of gradation

Third stageThird stage

• In the lower course of a river, the valley floor is extremely gently sloped. The river spreads over a large and its speed becomes very slow. Hence the river is not able to carry the sediments with it

• In this course the river generally deposits and very less erosion and transportation work takes place.

• The main features made by the river in its lower course are distributaries, delta and estuaries.

Page 30: Agents of gradation

DistributariesDistributaries

Page 31: Agents of gradation

DistributariesDistributaries

• By the huge amount of deposition taking place the river channel get obstructed resulting to the formation of distributaries. The distributaries branches off from the main river take the water away from the river.

Page 32: Agents of gradation

DistributariesDistributaries

Page 33: Agents of gradation

DeltaDelta

• A delta is a landform that is created at the mouth of a river where that river flows into an ocean, sea, estuary, lake, reservoir, flat arid area, or another river.

Page 34: Agents of gradation

DeltaDelta

Page 35: Agents of gradation

Nile deltaNile delta

Page 36: Agents of gradation

EstuariesEstuaries

Page 37: Agents of gradation

EstuaryEstuary

• An estuary is a semi-enclosed coastal body of water with one or more rivers or streams flowing into it, and with a free connection to the open sea.

• E.g., Klamath river

Page 38: Agents of gradation

EstuariesEstuaries

Page 39: Agents of gradation