Thursday, June 11, 2015

Waterfall

Waterfall: A flow of water over the edge of a cliff.Waterfall


There are two types of waterfall:
1.CataractsWaterfall 
2. Cascade Waterfall 
Cataracts Waterfall : Cataracts are found where there are many rapids in a large river and large volume of water flows down from this rapids.

Cascade Waterfall : Cascade waterfalls have a small volume of water. A series of  falls may form one waterfall.

Formation of Waterfall:Hard Rock covers the soft rock. Water flows on soft rock.Overtime the soft rock is eroded more and more by the force of water flowing over it. This makes a cliff which the water topples over it.At the bottom of the cliff  some water splashes onto the cliff and makes a plunge pool by a process called 'undercutting '. 


Plunge Pool:  A plunge pool is  found at the bottom of a waterfall. A large pothole is formed by the water swirling and throwing boulders and stones around in circles.There is a lot of spray in a plunge pool at the bottom of a very large waterfall.

Facts: 
# The tallest waterfall in the world is the Angel Falls. It is 979  meters high .
# The highest waterfall in Africa is the Tugela Falls in Africa  . It is 947 meters and found in South Africa . 
# Niagara Falls on the border of Canada and the USA.Niagara Falls  are the easiest waterfalls for people to reach.

Tuesday, April 28, 2015

RIVERS : Stages of a River




                                                                  RIVERS    
A river is a natural flowing water course usually freshwater, flowing towards an ocean, a lake, a sea, or another river.
River Bank: Two sides of a river called River banks.
Rivers have two banks: Right bank and Left bank.
If you stand on a river and face the way the water is flowing, the right will be on your right hand side and left bank will be on your left hand side.
River bed:
 The bottom of the river called River bed. It can be made up of stones, pebbles, boulders, rock and mud. The water flows over the river bed. Rivers bed can be seen in streams because of its shallow water. River bed of middle and lower course is not visible because of deeper water.
River Channel: The main way or the path by which river water flow is called the river channel. It can be a straight channel like a canal or a meandering channel. Channel gives the river its shape.
Courses of Rivers: Rivers have three courses:
Upper course
Middle course
 Lower course
Upper course: The upper course found in the mountains and hills where the river starts its journey. Waterfalls, rapids are found in this course. The river starts as a stream in the upper course and flows through V-shaped valleys. The river has fast flowing water in the upper course. Rivers carry lots of stones and boulders with the water to flow over. Fast flowing water and grinding stones cut down the river valley and make the river valleys deeper and steeper in upper course. Erosion occurs mostly here.
Rivers in upper course



Middle course: The middle course is where the river starts to become wider and deeper. Instead of eroding downwards river starts erode sideways. This creates a broad V-shaped valley. The river starts to meander or bend in the middle course. River flows gently here. Erosion and deposition occurs in this course.
Rivers in middle course

Lower course: Rivers flow slowly in this course. Rivers become widest here. This course is found closest to the sea where the river has its mouth. The flat area beside the river banks is known as floodplain. Floodplain is very fertile because of its alluvial soil. Farmers grow crops there. Sometimes river might also have Estuary or Delta at its mouth.
Rivers in lower course

Stages of Rivers: There are also three stages of a river’s life:
Stage 1 is a youthful river. This is the rivers upper course where the rivers have fast flowing water, rapids, stream and tributaries.
Stage 2 is the mature river. This is the river in its middle course where it has meanders and flowing gently.
Stage 3 is the river in old age. This is in lower course, where rivers flow slowly towards its mouth at the sea.
 
Features of a river
                                                                    Source:
Source is the start or beginning of a river.The source of a river usually found in hills and mountains.A river can have more than one source.Sources can be different type:
Springs:Some rivers begin where water flows out of rocks.Rain water sinks through the soil and trickles through the cracks and spaces in rocks such as chalk and limestone.These are called Permeable rocks.The water continues to do this until it reaches a rock like clay.Clay is an impermeable rock.
Rills and Streams:Lots of rain fall on mountains.Rainwater flows down slopes and quickly makes channels.At beginning channels are small . They are called They are called Rills.They join together and make bigger rills . Finally stream is formed.The streams join up  to make a river.

Lakes:The source of some rivers are Lakes. The source of river Nile is Lake Victoria in Burundi.
Melting Snow and ice:When the weather gets warmer the snow and ice melts.This forms lake in front of glaciers and rushes into channels in the V-shaped valley and eventually forms a river.
Few examples of sources of rivers:
The source of river Nile is Lake Victoria in Burundi.
The source of Missouri river is  in Rocky mountain.
The source of Amazon river is  in Andes mountains.
                                                         
                                                                 
                                                                     Stream
A stream is the same as a river. Streams usually have narrow channels and are quiet shallow. Streams are usually found in the upper courses.
                                                                    Tributary:
A tributary is a stream or a river flowing into a larger river. A river grows as more tributaries flow into it. There is no special size that a tributary has to be. Some of the World’s longest river are joined by tributaries that themselves are major rivers. Example is Missouri river a major tributary of the Mississippi river.
                                                                    Mouth:
Mouth is the place where river ends its journey.Rivers may meet the sea, a lake or a larger waterway.Most rivers flow into the sea.
Not all rivers mouth are the same.There may be an Estuary or Delta at the mouth.The River Jordan flows into the dead sea which is actually an inland lake.In desert areas some rivers simply dry up.
                                                                  Estuary:
If the river has wide mouth, it is called an Estuary.Rivers carry a lot of sediment as it travels from its source to its mouth.When the freshwater from the rivers meet the salty water from the sea , the river drops its sediment.Most is then washed away by the sea and the tides.

Monday, February 23, 2015

Ring of fire or circum-Pacific Belt

Geography ,short notes( Plate , Plate boundaries, Ring of fire, Subduction zone)Geography ,short notes( Plate , Plate boundaries, Ring of fire, Subduction zone)

Ring of fire or circum-Pacific Belt 
There are two major regions of earthquake  activity. one is Circum- Pacific belt, which encircles the Pacific ocean and other is the Alpide belt which slices through Europe and Asia.The Circum- Pacific belt or Ring of fire includes the West costs of North America and South America,Japan and the Phillipines.

Ring of fire or circum-Pacific Belt: The Pacific Ocean region has more earthquakes and volcanic activity than any other area of the world. For this reason this region has been named Ring of fire or Circum-Pacific belt. About 90% of all earthquakes and volcanic eruption occur there.





Geologists came to the conclusion in 1960's that the Earth's rigid outer layer was not a single piece, but was broken up into 12 large pieces called Plates.

Plate: The Earth's crust is broken into many pieces called Plate.
Plates are two types.

  1. Oceanic Plate
  2. Continental PlateGeography ,short notes( Plate , Plate boundaries, Ring of fire, Subduction zone)

Plate Boundaries:There are Three types of Plate boundaries:

Convergent boundaries: two plates collide together to form mountains or a Subduction zone.
Convergent Boundary

Divergent boundaries:two plates move in opposite directions as in Mid-Ocean ridge.
Divergent boundary

Transform boundaries: Two plates slide past each other as in San Andreas fault of California.
Transform boundary
 Subduction zone: When a Continental plate overrides Oceanic plate, the Oceanic Plate gets driven down and a Subduction zone forms.
 Subduction zone