Geography Flashcards
3 layers of Earth?
Crust, Mantle and Core
Describe Crust
Outermost solid part of the earth.
Brittle in nature
Oceanic crust is thinner than continental crust
Continental crust is thicker in Himalayan regions approx 70km thick
Continental crust is Made up of heavier rocks like granite
Oceanic crust is made up of basalt
Describe Mantle
Portion of interior below the crust.
Mohorovicic or Moho discontinuity separates the crust above from the mantle below.
Crust and upper part of mantle is called lithosphere. Its thickness ranges from 10-200km.
The upper portion of mantle is called asthenosphere and is the main source of magma.
Its density is higher than crust.
Mantle is in solid state.
Mantle is made up of silicate minerals rich in iron and magnesium.
Asthenosphere
Upper portion of the mantle
It is plastic or soft layer
Lithosphere
Crust + Cooler brittle upper part of the mantle
Composition of Mantle
Silicate minerals rich in iron and magnesium
Describe core
Outer core is in liquid state while inner core is in solid state.
Composed of NIFE layer
Weichert-Gutenberg discontinuity located at a depth of 2900 km is a core-mantle boundary. There is a sudden change of density here from 5.5g/cm3 of mantle to 10g/cm3
Weichert-Gutenberg discontinuity
Weichert-Gutenberg discontinuity located at a depth of 2900 km is a core-mantle boundary. There is a sudden change of density here from 5.5g/cm3 of mantle to 10g/cm3
Moho’s discontinuity
Between crust and mantle
Lithospheric plates
Because the asthenosphere is soft and plastic, the rigid lithosphere can easily move over it.
The lithospheric shell is divided into large pieces called lithospheric plates. A single plate can be as large as a continent and can move independently of the plates that surround it.
There are 7 major and 20 minor types of lithospheric plates
First order relief features
Continents and oceans
Who gave continental drift theory?
Alfred Wegener
Pangea
All the continents forming single continental mass is called pangea
Panthalassa
Mega-ocean surrounding pangea
Wegener’s continental drift theory?
According to Wegener, all the continents formed a single continental mass called Pangea surrounded by a mega ocean called Panthalassa. Around 20mya in the jurassic period, the super continent, Pangea began to split. pangea first broke into two large continental masses as Laurasia and Gondwanaland forming the northern and southern components respectively which continued to break into various smaller continents that exist today.
He proposed that continents are floating and constantly drifting on the Earth’s surface
His hypotheses later became the basis for plate tectonics
Evidences of existence of Pangaea?
- Jig-Saw-Fit (The Matching of Continents)- The shorelines of Africa and South America facing each other have a remarkable and unmistakable shore line.
- Radiometric dating shows that age of rocks of both the costs of Atlantic are identical. This suggests that the ocean did not exist prior to jurassic age
- Palaeoclimatic evidence- The evidences of carboniferous glaciations in the form Tillite rocks are found in Brazil, Falkland, S.Africa, Madagascar, India and Antarctica shows that these landmasses once had the same climate which was possible only if they were contiguous.
- paleontological evidence- the distribution of Glossopteris flora too matches with the above contiguous areas of Gondwana land
Tillite?
It is the sedimentary rock formed out of deposits of glaciers.
Composition of Earth’s interior?
SIAL, SIMA, and NIFE
SIAL is composed of granite and dominated by Silical and Aluminium. It floats over SIMA which is denser (3) and has Silica and Magnesium.
NIFE is composed of nickel and Iron and is found in Core
7 major lithospheric plates
Eurasian African Indo-Australian pacific north american South American Antarctic
Important minor plates
Cocos Nazca Arabian Philippines Caroline Fuji etc
Plate tectonics
Science of lithospheric plate motions is called plate tectonics.
It is not the continent that moved as believed by Wegener but plates of which continents are part
Plate margins
All tectonic activities occur along plate margins
Three types of Plate margins are:
1. Constructive margin or Divergent plate margins or Accreting plate boundaries
- Destructive plate margins or Convergent plates or Consuming plate boundaries
- Conservative plate margins or Transform Plate movements
Example of divergence on continent
East africa rift valley
Example of divergence in ocean
Atlantic ocean floor formed as the continent that included South America and Africa broke up and moved apart 2-5cm per year over millions of year