Part-1 Flashcards
Geography as a Discipline, The Origin and Evolution of the Earth-Theories, The Origin and Evolution of the Earth-Part 2, Structure of the Earth, Continental Drift, Earthquake, Volcanoes, Volcanic Landforms, Air, Our Changing Earth, Inside our Earth, Environment, Our Country – India, India: Climate, Vegetation and Life, Major Landforms of the Earth, Major Domains of the Earth, Motions of Earth, Maps, Latitudes and Longitudes, The Earth in the Solar System
What is Geography?
- The term geography was first devised by Eratosthenes, a Greek scholar (276-194 BC.)
- Geography is a discipline of the combination of spatial synthesis and temporal synthesis.
- According to geography, Earth is described as the abode of human beings.
- Landforms provide the foundation on which anthropogenic activities are placed.
- The plains are used for agriculture.
- Plateaus provide a platform for minerals and forest.
- Mountains make available space for meadows, forests, tourist spots, etc. They are regarded as the sources of rivers.
Branches of Geography
- Physical Geography
- Human Geography
- Biogeography
Physical Geography
- Geomorphology is a branch of Geography dealing with the study of landforms, the formation of landforms, and associated courses.
- Climatology includes the study of atmosphere structure, elements of weather, climate, climatic types and climatic regions.
- Hydrology deals with the study of water present on the surface of the earth comprising oceans, rivers, lakes and other water bodies, its influence on various life forms on earth and allied activities.
- Soil Geography is to study the courses of soil formation, types of soil, fertility status of soils, soil distribution and utilization.
Human Geography
- Social/Cultural Geography covers the study of society and the spatial dynamics of society and the cultural aspects caused by society.
- Population Geography encompasses the population growth, density, distribution, migration, sex ratio and occupational structure, and so on.
- Settlement Geography deals with the features of urban and rural settlements.
- Economic Geography is related to people’s economic activities comprising agriculture, industry, services, trade, transport, infrastructure, etc.
- Historical Geography deals with the historical processes by which space gets organised. The geographical features also go through temporal changes; these are the issues of historical geography.
- Political Geography is the study of the spatially unbalanced results of political courses and the various manners in which political processes are themselves influenced by spatial structures.
Biogeography
- The interface between human geography and physical geography has led to the progress of Biogeography which contains:
- Ecology and Ecosystem deal with the scientific study of the habitats features of species.
- Plant Geography which deals with the spatial structure and order of natural vegetation in their environments.
- Zoo Geography which is concerned with the spatial patterns as well as geographic features of various fauna and their habitats.
Earth – Origin & Evolution
Early Theories
Nebular Hypothesis
- Immanuel Kant, a German philosopher gave this theory.
- In 1796, a mathematician Pierre-Simon Laplace reexamined it.
- According to this hypothesis, the planets were moulded out of a cloud of material associated with a young sun, which was rotating slowly.
Binary theories
- As per these theories, the sun had a companion.
Revised Nebular Hypothesis
- Revised Nebular Hypothesis was propounded by Carl Weizascar in Germany and Otto Schmidt in Russia.
- They regarded that a solar nebula surrounded the sun and that the nebula comprised of chiefly hydrogen, helium and something called dust.
- The collision of particles and the friction caused a disk-shaped cloud to be formed and then the planets were created via the accretion process.
Modern theories of evolution
Big Bang Theory
- Alternatively called the expanding universe hypothesis.
- As per this theory, in the beginning, all matter or substance forming this universe existed at one place as a tiny ball. This tiny ball had an extremely small volume, infinite density and temperature.
- At the Big Bang, this ball blasted fiercely and forcefully and started a substantial process of expansion which continues to this day.
- Now it is accepted that this event took place 13.7 billion years ago.
Formation of Planets
The following are regarded as the stages in the planets’ development:
- The stars are localised gas lumps inside a nebula.
- A core to the gas cloud as well as a spinning disc of dust and gas are created because of the gravitational force within the lumps.
- After this, the cloud of gas condenses and the matter over the core is changed into tiny rounded objects.
- These small round objects develop into what are called planetesimals by a cohesion process.
- The smaller objects start forming larger bodies by colliding with one another and they stick together because of gravitational force.
- In the last stage, these large number of small planetesimals aggregate to develop into a smaller number of large bodies called planets.
Lightyear
- It is a unit of astronomical distance which is equal to the distance light travels in one year.
- A light year is a measure of distance and not of time.
- Light travels at a speed of 300,000 km/second.
Solar system
- Solar system consists of eight planets.
- Mercury, Venus, Earth, Mars, Jupiter, Uranus, Saturn and Neptune.
- The inner planets are Mercury, Venus, Earth, and Mars.
- After an asteroid belt come the outer planets, Jupiter, Saturn, Uranus, and Neptune.
The Moon
- The moon is the only natural satellite of the earth.
Evolution of the Earth
- The age of Earth is approximately one-third of the age of the universe.
- Earth formed around 4.54 billion years ago by accretion from the solar nebula.
Lithosphere, Atmosphere, and Hydrosphere of the Earth
- Lithosphere: The firm outer part of the earth, comprising of the crust and upper mantle.
- Atmosphere: A layer of gases encircling a planet that is seized in place by the gravity of that body.
- Hydrosphere: It is the collective mass of water found on, under, and above the surface of the earth.
- The first stage of the evolution of Lithosphere, Atmosphere, and Hydrosphere is marked by the loss of primordial atmosphere.
- In the second stage, the hot interior of the earth contributed to the evolution of the atmosphere.
- Finally, the composition of the atmosphere was modified by the living world through the process of photosynthesis.
- The present composition of earth’s atmosphere is chiefly contributed by nitrogen and oxygen.
Geological Scale
Attached
Structure of the Earth
- The Crust
- The Mantle
- The Core
The Crust
- The crust is the outermost solid part of the earth.
- It is fragile in nature.
- The thickness of the crust varies under the oceanic and continental areas.
- Oceanic crust is thinner as compared to the continental crust.
- The continental crust is thicker in the areas of major mountain systems.
- The crust made up of heavier rocks having a density of 3 g/cm3.
- The kind of rock seen in the oceanic crust is basalt.
- The mean density of material in the oceanic crust is 2.7 g/cm3.
The Mantle
- The portion of the interior beyond the crust is called the mantle.
- It is in a solid state.
- It has a density higher than the crust portion.
- The thickness ranges from 10-200 km.
- The mantle extends from Moho’s discontinuity to a depth of 2,900 km.
- The asthenosphere is the upper portion of Mantle.
- It is the chief source of magma that finds its way to the surface during volcanic eruptions.
- The crust and the uppermost part of the mantle are called lithosphere.
The Core
- The core-mantle boundary is positioned at the depth of 2,900 km.
- The inner core is in the solid state whereas the outer core is in the liquid state.
- The core is made up of very heavy material mostly constituted by nickel and iron. Hence it is also called the “nife” layer.
Continental Drift Theory
- Continental drift theory was proposed by Alfred Wegener in 1912.
- The theory deals with the distribution of the oceans and the continents.
- According to Wegener’s Continental Drift theory, all the continents were one single continental mass (called a Super Continent) – Pangaea and a Mega Ocean surrounded this supercontinent. The mega ocean is known by the name Panthalassa.
- The supercontinent was named Pangaea and the Mega-ocean was called Panthalassa.
- According to this theory, the supercontinent, Pangaea, began to split some two hundred million years back.
- Pangaea first split into 2 big continental masses known as Gondwanaland and Laurasia forming the southern and northern modules respectively.
- Later, Gondwanaland and Laurasia continued to break into several smaller continents that exist today.
Evidence supporting the Continental Drift Theory
- The Matching of Continents (Jig-Saw-Fit)
- Rocks of the Same Age across the Oceans
- Tillite
- Placer Deposits
- Distribution of Fossils
1. The Matching of Continents (Jig-Saw-Fit)
- The coastlines of South America and Africa fronting each other have a remarkable and unique match.
- In 1964, Bullard created a map using a computer program to find the right fit of the Atlantic margin and it proved to be quiet.
2. Rocks of the Same Age across the Oceans
- The radiometric dating methods have helped in correlating the formation of rocks present in different continents across the ocean.
- The ancient rocks belts in the coast of Brazil match with those found in Western Africa.
- The old marine deposits found in the coasts of South America and Africa belong to the Jurassic Age. This implies that the ocean never existed before that time.
3. Tillite
- It is the sedimentary rock made from glacier deposits.
- The Gondwana system of sediments from India is recognized as having its counterparts in 6 different landmasses in the Southern Hemisphere.
- Counterparts of this series are found in Madagascar, Africa, Antarctica, Falkland Island, and Australia not to mention India.
- At the base, the system has thick tillite signifying widespread and sustained glaciation.
- Generally, the similarity of the Gondwana type sediments evidently shows that these landmasses had exceptionally similar origins.
- The glacial tillite gives a clear evidence for palaeoclimates and the drifting of continents.
4. Placer Deposits
- The presence of abundant placer deposits of gold along the Ghana coast and the complete lack of its source rocks in the area is a phenomenal fact.
- The gold-bearing veins are present in Brazil and it is evident that the gold deposits of Ghana in Africa are obtained from the Brazil plateau from the time when the two continents were beside each other.
5. Distribution of Fossils
- The interpretations that Lemurs occur in India, Africa and Madagascar led to the theory of a landmass named “Lemuria” connecting these 3 landmasses.
- Mesosaurus was a tiny reptile adapted to shallow brackish water.
- The skeletons of these creatures are found in the Iraver formations of Brazil and Southern Cape Province of South Africa.
Force for Drifting
- Wegener proposed that the movement accountable for the drifting of the continents was instigated by tidal force and pole-fleeing force.
- The polar-fleeing force relates to the rotation of the earth.
- The shape of earth
- The second force that was proposed by Wegener, the tidal force.
- Though, most of the scholars considered these forces to be totally insufficient.
Earthquake
- All natural earthquakes occur in the lithosphere.
- Seismic waves studies offer a full picture of the layered interior.
- An earthquake is, simply put, shaking of the earth’s crust.
- It is caused due to the energy release, which triggers waves that travel in all directions.
- The emanation of energy occurs along a fault.
- A fault is a sharp break in the crustal rocks.
- Rocks along a fault generally move in opposing directions.
Types of Earthquakes
- Tectonic earthquakes: These are produced due to sliding of rocks along a fault plane.
- Volcanic earthquake: These are confined to areas of active volcanoes.
- Collapse earthquake: The roofs of underground mines collapse causing minor tremors in the areas of intense mining activity.
- Explosion earthquakes: These occur due to the explosion of chemical or nuclear devices.
- Reservoir-induced earthquakes: These occur in the areas of large reservoirs.
Causes of Earthquakes
- It is caused due to the discharge of energy from faults and cracks in the crust of the earth.
- A fault in the crust of Earth is essentially a sharp break in crustal rocks.
- This energy release produces waves which travel in all directions.
- The point where energy is released is called the focus or hypocentre. It is generally located at the depth of 60 km.
- This causes a release of energy, and the energy waves travel in all directions.
- The point where the energy is released is called the focus of an earthquake or hypocentre.
- The point on the surface of the earth which is vertically above the focus is called epicentre. It is the first place to experience the waves.
Body Waves
- Earthquake waves are of two types — body waves and surface waves.
P- Waves
- P-waves are also known as the Primary waves. They are the first waves to arrive at the surface.
- The characteristics of P-waves are like sound waves. They travel through all three mediums- solid, liquid and gas.
- These waves have a tendency to vibrate parallel to the direction of wave propagation. This causes density differences in the material through which they travel.
- These waves are responsible for elongating and squeezing of material.
S- Waves
- S- Waves arrive after some time after the happening of Earthquake and they are called secondary waves.
- A significant characteristic of these S-waves is that they travel only through a solid medium.
- The direction of vibration of these S – wave is perpendicular to the direction of wave propagation, thereby creating crests and troughs in the material of their transmission.
Shadow Zone
- The shadow zone is the zone of the earth from angular distances of 104 to 140 degrees from a given earthquake that does not receive any direct P waves.
- The shadow zone results from P waves being refracted by the liquid core and S waves being stopped completely by the liquid core.
- A zone between 105° and 145° from the epicentre was recognised as the shadow zone for both the waves types.
- The entire zone beyond 105° does not receive S-waves.
- The shadow zone of S-wave is larger than that of the P-waves.
- The shadow zone of P-waves appears as a band around the earth between 105° and 145° away from the epicentre.
Effects of earthquake
The following are the immediate hazardous effects of Earthquake:
- Shaking of ground
- Disparity in ground settlement
- Natural disasters like Tsunami, land slide, mud slides and avalanches
- Soil liquefaction
- Ground lurching and displacement
- Floods and fires
- Infrastructure collapse.
Measurement of Earthquakes
All earthquakes are different in their intensity and magnitude. The instrument for measurement of the vibrations is known as Seismograph.
Magnitude scale
- Richter scale is used to measure the Magnitude of the earthquake
- The energy released during a quake is expressed in absolute numbers of 0-10.
Intensity scale
- The mercalli scale is used to measure the intensity of an earthquake
- It measures the visible damage caused due to the quake.
- It is expressed in the range of 1-12.
Volcanoes
- A volcano is a vent or fissure in Earth’s crust through which lava, ash, rocks, and gases erupt.
- An active volcano is a volcano that has erupted in the recent past.
- The mantle contains a weaker zone known as asthenosphere.
- Magma is the material present in the asthenosphere.
- Material that flows to or reaches the ground comprises lava flows, volcanic bombs, pyroclastic debris, dust, ash and gases. The gases maybe sulphur compounds, nitrogen compounds, and trace amounts of argon, hydrogen and chlorine.
Major types of volcanoes
Volcanoes are classified on the basis of nature of eruption and the form developed at the surface.
- Shield Volcanoes
- Composite Volcanoes
- Caldera
- Flood Basalt Provinces
- Mid-Ocean Ridge Volcanoes
Shield Volcanoes
- The Shield volcanoes are the largest of all the volcanoes on the earth, which are not steep.
- These volcanoes are mostly made up of basalt.
- They become explosive if in some way water gets into the vent, otherwise, they are characterized by low-explosivity.
- The lava that is moving upwards does so in a fountain-form and emanates the cone at the vent’s top and then develops into cinder cone.
- Eg: Hawaiian shield volcanoes
Composite Volcanoes
- Composite Volcanoes are characterized by outbreaks of cooler and more viscous lavas than basalt.
- They are constructed from numerous explosive eruptions.
- Large quantities of pyroclastic material and ashes find their way to the ground along with lava.
- This material gathers near the vent openings resulting in the creation of layers.
- Mayon Volcano in the Philippines, Mount Fuji in Japan, and Mount Rainier in Washington are the major composite volcanoes in the world.
- The major composite volcano chains are Pacific Rim which known as the “Rim of Fire”.
Caldera
- Calderas are known as the most explosive volcanoes of Earth.
- They are generally explosive in nature.
- When they erupt, they incline to collapse on themselves rather than constructing any structure.
- The collapsed depressions are known as calderas.
Flood Basalt Provinces
- Flood Basalt Province volcanoes discharge highly fluid lava that flows for long distances.
- Many parts of the world are covered by thick basalt lava flows.
Mid-Ocean Ridge Volcanoes
- These volcanoes are found in the oceanic areas.
- There exists a system of mid-ocean ridges stretching for over 70000 km all through the ocean basins.
- The central region of this ridge gets frequent eruptions.
Volcanic landforms
Volcanic eruptions result in the formation of landforms as given below:
- Intrusive Forms
- Batholiths
- Lopolith
- Phacolith
- Sills
- Dykes
Intrusive Forms
- The lava that is discharged during volcanic eruptions on cooling develops into igneous rocks.
- The cooling may take place either on arriving on the surface or also while the lava is still in the crustal portion.
- According to the location of the cooling of the lava, igneous rocks are categorized as plutonic rocks and volcanic rocks.
- The lava that cools inside the crustal portions takes diverse forms. These forms are called intrusive forms.
Some of the forms are shown in Figure given below
Batholiths
- Batholiths are the cooled portion of magma chambers.
- It is a large body of magmatic material that cools in the deeper depth of the crust moulds in the form of large domes.
- They appear on the surface only after the denudation processes eliminate the overlying materials.
- These are granitic bodies.
Laccoliths
- These are large dome-shaped intrusive bodies with a level base and linked by a pipe-like channel from below.
- It bears a similarity to the surface volcanic domes of the composite volcano, only these are located at deeper depths.
- It can be considered as the localized source of lava
- The Karnataka plateau is patterned with dome hills of granite rocks.
Lopolith
- When the lava moves upwards, a part of the same tends to move in a horizontal direction wherever it finds a weak plane.
- It can get rested in various forms. If it develops into a saucer shape, concave to the sky body, it is called lopolith.
Phacolith
- It is a wavy mass of intrusive rocks found at the base of synclines or at the top ofthe anticline in the folded igneous country.
- These wavy materials have a definite outlet to source beneath in the form of magma cavities.
Sills
- The near horizontal bodies of the intrusive igneous rocks are called sill
- The thick horizontal deposits are called sills whereas the thinner ones are called sheets.