geogra l5 1

• Melting due to global warming

• New sea route from Europe to Russia

• Potential petroleum reserve

• Artic ocean- global commons

• Arctic council

Arctic Ocean

• Sulphur – rarely found on land. Available in sea during marine volcanism.

Ex. Gulf of Mexico – rich source of sulphur

Resource at continental shelf

Placer depositsWave action erode the beach rocks some stable minerals freed from the rocks due to weatheringwaves shift the lighter material more rapidly than heavierconcentration of heavy minerals on shelf

Resources from continental shelf

• monazite sand (source of thorium) at Kerala coast

• Gold (Alaska)• Zircon (Brazil,

Australia)• Diamond (South

Africa)

Resources from continental shelf

• Calcium- least soluble in ocean water – Peruvian coast rich deposits of calcium and phosphate

• Fishes are rich in nitrate and phosphate, high protein, medicinal use

• Pearls

Resource at continental shelf

Continental shelf Continental slope Continental rise

Ocean- continent margin landforms

• Very steep slope• Massive landslides of

terrigenous deposits• Rivers like, Ganga,

Indus, Mississippi, Yukon and Congo have created submarine canyons

• Highest waterfall on earth – under Denmark Strait.

Continental slope

Continental shelf Continental slope Continental rise

Ocean- continent margin landforms

• Transition zone between continental block and oceanic block

Continental Rise

• They are absent near trenches, as subduction near trenches consumes the deposition of Continental rise

Continental rise

Continental shelf Continental slope Continental rise

Ocean- continent margin landforms

3 divisions:1) Ocean –

continent margin

2) MOR3) Deep

Ocean plains

Division of Ocean Bottom

• Occupies 40% of the ocean floor

• Tremendous diversity in terms of landforms

• It has deposits from continents (terrigenous), marine life (biogenous) and salts and mineral (inorganic)

Abyssal Plain

• PMN (Poly Metallic Nodules) or Manganese nodules• Concentration of

metals around a core• Depth 4000-

6000m

Resources from Abyssal plain

• First found in Kara sea, Arctic ocean

• These nodules are found in the all the oceans –economically viable -central Indian Ocean and Eastern Pacific Ocean.

Global distribution of PMN

PMN• PMN are small nodules

of metals like, Manganese, Iron, Silicon, Al, Nickel and Cobalt etc.

• some of the minerals are rare on land.

• Countries are in race to explore and extract PMN

2002- India got approval from ISA – ‘Pioneer Investor’ for 15 years

India - 1,50,000 ml ha ocean stretch in central Indian Ocean out of 10 to15 ml ha of PMN

India RV Samudra Ratnakar + equipment from S Korea

NIOT – developing tech for exploration

2011 - China acquired 10,000 ha area

2013 – UK co. in Pacific ocean

PMN

India

UN convention on Laws of the seas1983 60 countries signedcame into force in 19931) Decides the maritime

boundary2) Deep sea mining (ISA,

Kingston, Jamaica)3) Environment protection4) Dispute settlement

UNCLOS

ISA

• Decides territorial waters, contiguous zone and EEZ for coastal countries

• EEZ – special right of the state to explore minerals or produce energy from the area

UNCLOS

Mains

2014

Q. Critically evaluate the various resources of the oceans which can be harnessed to meet the resource crisis in the world (10)

UPSC

Question

4 types of Islands:1) Volcanic (plate/ hot spot)2) Continental3) Coral islands 4) Sand bar islands

Types of Islands

Island Formationcontinental Once part of

large continentvolcanic O-O plate

collision, Hot spot

coral Formed due to coral reefs

Sand-bar island Accumulation of sand near the coast

Types of Islands

Continental IslandsVolcanic islands

Types of Islands

Sand-bar islandsCoral Islands

Types of Islands

Volcanic Continental

Coral Sandbar

Japan Shri Lanka

Lakshadweep

Long Island (New York)

Philippines

Madagascar

Maldives

Kurile Vancouver

Mauritius

Aleutian Baffin Island

Bahama, Bermuda

Example of Islands

• Indicative of health of Marine ecology

• Primary food-chain

• Source of great biodiversity

Coral Reefs

• Corals = tiny fleshy sea anemones polyps. • They extract Ca from the sea water for their

skeletons to protect their bodies.• One generation die on previous generation. • Corals live symbiotic relationship with

microscopic plant – Zooxanthalae, photosynthesis capabilities.

• Zooxanthalae provide food to corals and corals provide protection to zooxanthalae

Coral Reefs

• Need submarine shallow platform (50 meter deep)– to receive sun light

• Temperature- 25-27 degree• Warm, tropical and low latitude waters• Salinity – 33 ppt• Not at mouth of river, No turbulent water• Need circulating nutrient rich water

Condition for growth of Corals

Spatial distribution of Corals

• When corals are in stress they expel zooxanthalae – that’s why coral seem white => coral bleaching. Ultimately, without food coral die

Coral Bleaching

• Global warming => increase in sea surface temperature

• Ozone depletion => increase in solar irradiation• Ocean acidification • algal bloom• Increase sedimentation from rivers• Marine pollution – oil spill• Diseases

Reason of coral Bleaching

Distribution of Coral Bleaching

• Corals can be developed both at the margins of the continents or around islands

• 3 stages of coral formation

1) Fringing reef2) Barrier reef3) Atoll

Formation of coral reef

• Coral reef developed along margin of an island

• If Gap is created between corals and the surface of island

• Small water bodies = lagoons

Fringing reef

• Reef is not continuous but broken

• Lagoon can connect to open ocean

• Most extensive • If they are parallel to

coast -> barrier reef

Barrier reef

• The hill submerged • Only narrow ring of

coral is visible

Atoll

Fringing Reef Atolls

Great Barrier Reef, Australia

• Dangerous for marine biodiversity• Marine diversity is

the wealth of the earth• Harmful to global

environment

Marine pollution

Marine pollutionIssue effectOil spill Marine life – devoid

of sunlight and oxygen

Run-off from land Eutrophication - Algal bloom

Atmospheric input makes ocean water acidic

Dumping of toxic elements

Toxicity harms marine organism

Ballistic water issue Danger to biodiversity

• Tar balls — lumps of petroleum

• oil spillage from tankers

• The wax-like lumps are caused due to the reaction of the oil with sea water

• Sticky and greasy

Tar balls

Ocean bottom relief:1) Continental shelf2) Continental slope3) Continental rise4) Abyssal plain Types of islandsFormation of coralMarine pollution

Horizontal

•waves•currents

Vertical •tides•Up-welling

Motion of Ocean water

• Creation of waves:• wind pushes the water body • gravity pulls the crests of the waves

downward, the falling water pushes the former troughs upward.

• Actual motion of water beneath the wave is circular

Waves

Waves

• when the depth of water is less than half the wavelength of the wave, the wave breaks

Breaking up of the waves

Horizontal

•waves•currents

Vertical •tides•Up-welling

Motion of Ocean water

• Ocean currents are narrow and shallow (up to 500 meter deep), stream of water circulating along the Ocean margins

• Circumnavigate the earth

Ocean Currents

• Heat distribution – from Poles to Eq.• warm water

from equator • Cold water

from Poles

Ocean currents

Wind

Insolation

Gravity

Coriolis Force

Forces responsible for Ocean Current

• Most of the currents follow the direction of the trade winds, Westerlies and polar easterlies

Dominant force : wind

• Water expands under high temperature• Cold water near poles• Water lighter near equator, than at the poles• Cold water - heavier (denser) sinks downward• Cold water from pole flow towards equator at

subsurface level, to balance loss of water at equator

Insolation: temperature gradient

Insolation: temperature gradient

• Salinity increases density of water• Denser water sinks at depth• Less saline water move towards high saline

water on the surface• High saline water move towards less saline

water at sub-surface• Equator – rainfall –less saline water• Poles – iceberg – high saline water

Insolation: Salinity gradient

• Factor deflect the path of the currents: • Coastlines modify the path of the currents• coriolis force deflect the path

Factors modifying the ocean currents

• Due to Earth’s rotation W->E

• Deflective force- deflect the direction of currents

• Clockwise – N• Anti-clockwise -

S

Coriolis effect

Prelims 2012

Q. Consider the following factors:1. Rotation of the earth2. Air pressure and wind3. Density of ocean water4. Revolution of the earthWhich of the above factors influence ocean currents?

UPSC

oceano

Prelims 2012

a) 1 and 2b) 1,2,3c) 1 and 4d) 2,3,4

Ans. B)Rotation of the earth -> coriolis forceAir pressure and wind -> planetary windsDensity of water -> salinity

UPSC

oceano

Prelims 2002

Q. Consider the following statements:1. Ocean currents are slow-

surface movement of water in ocean

2. Ocean current assist in maintaining the earth’s heat balance

3. Ocean currents are set in motion primarily by prevailing winds

UPSC

oceano

Prelims 2002

4. Tropical currents are affected by the configuration of the oceanWhich of the statements are correct?a) 1 and 2b) 2,3 and 4c) 1,3 and 4d) 1,2,3 and 4Ans. B)

UPSC

oceano

Ocean currents of the world

North Atlantic Ocean Currents

• Meeting of gulf stream and Labrador current at new found land• fishing ground =

grand banks• Foggy area –

dangerous for shipping

New found land

• warming effects to Western Europe• ports of

Norway Narvik, Hammerfest operating in winter- at same latitude ports in Russia freeze during winter

North Atlantic drift

cold currentPasses near canary islandsdesiccating effect to Sahara desert

Canary current

• Gyre of north equatorial current, gulf stream and canary current

• Water confined –calm and motionless

• HP zone – high salinity

• ‘Sargassum’- sea weed –obstruct navigation

• Devoid of nutrients – poor marine life

Sargasso sea

South Atlantic Ocean Currents

• Meeting of warm Brazilian and cold Falkland current• Important

fishing ground

Bahia Blanca

• Cold current• Desiccating effect

to Namib desert

Benguela current

North Pacific Ocean Currents

• cold Californian current• Chilling effect on

western coast of N. America

• Drying effect to Mojave desert, Sonoran desert in California

Desiccating effect of cold current

Meeting of cold-warm current near Japan

• Meeting of warm Kuroshio and cold Oyashio current near southern Japan

• Rich fishing ground• Foggy area

South Pacific Ocean Currents

• Cold Peru/Humboldt current – desiccating effect to Atacama dessert

• Peruvian coast – upwelling – rich fishing ground

Upwelling on Peruvian coast

North Indian Ocean Currents

• In summer: wind and current flow towards India – Arabia to India

• In winter: wind + current flow towards Arabia - sea vessel from India to Arabia

• Important for sea-trade, cultural interaction

Navigation in Indian Ocean

South Indian Ocean Currents

Prelims 1997

Q. Which one the following factor is responsible for the change in regular direction of the ocean currents in the Indian ocean?a) Indian ocean is half an oceanb) Indian ocean has monsoon

driftc) Indian ocean is a land-locked

oceand) Indian ocean has greater

variation in salinityAns. B)

UPSC

oceano

Prelims 2013

Q. The most important fishing ground of the world are found in the regions where:a) Warm and cold

atmospheric currents meetb) Rivers drain out large

amount of fresh water into sea

c) Warm and cold oceanic currents meet

UPSC

oceano

Prelims 2013

d) Continental shelf is inundating

Ans. C) 1) New found land2) Bahia Blanca3) Japanese coast

UPSC

oceano

Horizontal

•waves•currents

Vertical •Up-welling•tides

Motion of Ocean water

• The wind exerts stress on the ocean surface proportional to the square of the wind speed and in the direction of the wind.

• This motion extends to a depth of ~ 100 m

Ekman layer

• Wind force balanced by coriolis force and friction

• Water defect 45 deg under coriolis force

• Depth – wind force reduce- deflect away from wind direction

Ekman spiral

Ekman spiral 90 deg = Ekman transport• Deflect Right in N.

hemi• Deflect Left in S.

hemi• Due to coriolis

force

Ekman Transport

• When Ekman transport induce divergence at the coast

• divergence draws water from below to the surface

Up-welling

Ekman transportPeruvian coast

Ekman transport in southern hemisphere

Up-welling • cool and nutrient

rich water come at the surface• Phytoplankton

reproduce rapidly in this condition – zooplankton -> nekton

• Cold current • Humboldt current

= Peruvian coast• Gulf of Guinea,

Iberian coast• Up-welling – rich

nutrients => fishing

Up-welling regions

• When Ekman transport induce convergence at the coast

• convergence forces surface water downward

Down-welling

• Descending water -warm water - saline • push down at

the bottom

Down-welling

Horizontal

•waves•currents

Vertical •Up-welling•tides

Motion of Ocean water

• Rise and fall of sea water due to gravitation forces of sun and moon is called tides• Gravitational +

centrifugal forces

Ocean tide

• If moon stationary – every place on earth experience 2 HT and 2 LT in 24 hours

Ocean tides

• But moon also revolves around earth in 27.5 days

• So, same location comes under moon not exactly after 24 hours but 24.52 min

• So, diurnal frequency of HT and LT is 12.26 min

Ocean tides

• Difference between High tide and Low Tide

• Depends upon:1) Depth of ocean

water2) Configuration

of coastline3) Openness and

closeness of the sea

Tidal range

World: Bay FundyIndia: Gulf of Khambhat

Highest tidal range

• The time between the high tide and low tide, when the water level is falling, is called the ebb.

• The time between the low tide and high tide, when the tide is rising, is called the flow or flood

Ebb – Flood/Flow

• Moon’s orbit around the earth –elliptical

• Perigee tides – higher than apogee tides

Apogee and Perigee tides

Syzygy positions• the sun, the

moon and the earth are in a straight line (Syzygy)

• occur twice a month

• Conjuction – New moon

• opposition – full moon

Quadrature positionsun and moon are at right angles to each other (Quadrature)The forces of the sun and moon – counteract7/8 D of every fortnight

- Spring , neap = High tideSpring – highest HTNeap – Lowest HT- there is a 7 Days interval between the spring tides and neap tides.

Spring – Neap Tide

Spring tide

• HT higher than usual• LT lower than usual• Syzygy position• Gravitational force

from both sun and moon together

• HT lower than usual• LT higher than usual• Quadrature position• Gravitational force

of sun and moon counter-act

Neap tide

comparison

Prelims

2001

A) During the neap tides, high tide is lower and low tide is higher than usual

R) The neap tide, unlike spring tide, occurs on new moon instead of full moon.

Ans. A true, R is incorrect

UPSC

Question

• When the tide is channelled between islands or into bays and estuaries

• Coastward = flood current

• Seaward = ebb current• Reversing tidal currents

great velocity

Tidal currents

• when seawater enters into mouths of low lying rivers during HT

• Narrow opening – gentle gradient of river basin

• Obstructed by river water – so steep wall of tidal bore

Tidal bores

Prelims

2004

Q. Which of the following statement is NOT correct?a) Gulf with narrow fronts and

wider rears experience high tide

b) Tidal currents take place when a gulf is connected with open sea by narrow channel

c) Tidal bore occurs when a tide enters the narrow shallow estuary of river

UPSC

Question

If a mouth of a river is low-lying and submerged under sea-waterRiver deposit create long-narrow delta = estuary deltas Ex. Deltas of Tapi, Narmada

Estuary

Prelims

2004

d) The tidal nature of the mouth of river Hooghly is of the crucial importance to Kolkata port Ans. D)Tidal bores at Hooghly are constraints for shipping at port- Rushing current imbalance the docking ships

UPSC

Question

Hooghly -Distributary of Ganga• Kolkata on left bank

of Hooghly• Tidal bores in

Kolkata port

Hooghly river

• Tidal height important for Harbours with shallow ‘bars’ at the entrance, which prevent ships and boats from entering into the harbour.• Tides are also helpful in desilting the sediments and in

removing polluted water from river estuaries. • Tidal energy to generate electrical power

Importance of Tide

Prelims 2000

Q. Consider the following statements:1) Tides are great help

in navigation and fishing

2) High tide enable big ships to enter or leave the harbour safely

3) Tide prevents siltation of harbor

4) Kandla and diamond harbor are tidal ports

UPSC

Question

Prelims2000

a) 1 and 4b) 2,3 and 4c) 1,2 and 3d) 1,2,3 and 4

Statement 1 is wrong. Tide not helpful in navigation

Ans. B)

UPSC

Question

Kandla portDiamond harbour

Tidal ports

Tidal ports• Feed by sea water during

high tide• Located on coast• Ex. Kandla

• Feed by rivers• Relatively in-land • Ex. Kolkata port

Non-tidal ports

Ports

port facts

Kandla First port developed after independence

JNPT To decongest Mumbai port

Murmagao, KN Known for iron ore export

New Manglore port Export iron ore from Kudremukh mine in KN

Kochi At the entrance of a lagoon

Tuticorin port Also Handles cargo of Shri Lanka and Maldives

Chennai Oldest artificial port

vishakhapatnam Deepest landlocked port, export iron ore

Kolkata port Riverine port

Haldia To decongest Kolkata port

Paradip port, Odisha Initially to export iron ore

12 major ports of India

Motion of ocean waterHorizontal – wave, current

Vertical – tide

• Power is harnessed taking advantage of difference of level between HT and LT

• A dam is constructed to clock receding water during LT

• Water is released from dam – turbine - electricity

Tidal energy

• La Rance, France• Scotland, UK• potential of 8000MW in

India• Gulf of Cambay, gulf of

Kutch, Sundarban (WB)• 50 MW plant in gulf of

Kutch 2012

Tidal energy in world

• Turbines are placed on ocean floor

• Turbine are run by fast moving ocean currents

• Fastest ocean currents: gulf stream off East USA

Tidal stream energy

Horizontal

•waves•currents

Vertical •tides•Up-welling

Motion of Ocean water

Motion of ocean waterHorizontal – wave, current

Vertical – tide, upwelling –down welling

Tidal energy