Sunday, 5 January 2014

Major Straits of the world



Name
Joins
Location
Malacca Strait
Andaman Sea & South China Sea
Indonesia - Malaysia
Palk Strait
Palk Bay & Bay of Bengal
India-Sri Lanka
Sunda Strait
Java Sea & Indian Ocean
Indonesia
Yucatan Strait
Gulf of Mexico and Carribbean Sea
Mexico-Cuba
Mesina Strait
Mediterranean Sea
Italy-Sicily
Otranto Strait
Adriatic Sea & Ionian Sea
Italy-Albania
Bab-el-Mandeb Strait
Red Sea & Gulf of Aden
Yemen-Djibouti
Cook Strait
South Pacific Ocean
New Zealand (N & S islands)
Mozambique Strait
Indian Ocean
Mozambique - Malagassy
North Channel
Irish Sea & Atlantic Ocean
Ireland-England
Taurus Strait
Arafura Sea & Gulf of Papua
Papua New Guinea - Australia
Bass strait
Tasman Sea & South Sea
Australia
Bering Strait
Bering Sea & Chuksi Sea
Alaska-Russia
Bonne-Fasio Strait
Mediterranean Sea
Corsika-Sardinia
Bosporous Strait
Black Sea and Marmara Sea
Turkey
Dardenleez Strait
Marmara Sea and Agean Sea
Turkey
Davis strait
Baffin Bay & Atlantic Ocean
Greenland-Canada
Denmark strait
North Atlantic and Arctic Ocean
Greenland-Iceland
Dover strait
English Channel & North Sea
England-France
Florida Strait
Gulf of Mexico and Atlantic Ocean
USA-Cuba
Hormuz strait
Gulf of Persia & Gulf of Oman
Oman-Iran
Hudson strait
Gulf of Hudson & Atlantic Ocean
Canada
Gibraltar Strait
Mediterranean Sea & Atlantic Ocean
Spain-Morocco
Magellan strait
Pacific and South Atlantic Ocean
Chile
Makkassar Strait
Java Sea & Celebeze Sea
Indonesia
Tsungaru Strait
Japan Sea and Pacific Ocean
Japan (Hokkaido-Honshu island)
Tatar Strait
Japan Sea & Okhotsk Sea
Russia (E Russia-Sakhalin Island)

Mountains and Plateau

Mountains are such highlands whose slopes are steep and the peaks are pointed. Generally, the mountains are more than 1000 mts high. The mountains whose height is less than 1000 mts, are called hills. The highest point of a mountain or a hill is called its peak. A mountain range is a system of mountains and hills having several ridges, peaks, summits and valleys, formed in a particular period and spread in a narrow belt.
Classification of Mountains
  • Folded Mountains: These Mountains are the results of compressive forces, triggered by the endogenetic forces. When the rocks on (he surface of the earth are folded due to the forces generated within the earth, the resultant Himalaya Ural, Rockies, Andes, Atlas etc. examples of folded mountains.
  • Block Mountains: These Mountains originate due to the forces of tension leading to the formation of rift valleys. These are also know as fault Block Mountains, as they are the result of faulting. Sierra Nevada mountain of California, USA, Vosages and Black Forest mountains of Europe.
  • Accumulated Mountains: These mountain are formed due to accumulation of lava other ejected materials in the proccess of vulcanism. Fujiyama of Japan, Cotopaxi of Equador are its examples.
  • Relict Mountains: When orginal mountains are eroded by the agents of gradation, they become relict mountains. Vindhyas, Aravallis, Satpura, Eastern Ghats, Western Ghats, Parasnath etc. are relict mountains.
Plateau
A plateau may be defined as that upland which has at least one side of very steep slope standing well above the neighbouring surface and whose upper part is extensive and almost flat.
Classification of Plateau
  1. Intermontane Plateau: These Plateaus are surrounded by hills and mountains from all sides. For Example Tibetan plateau, Columbian plateau.
  2. Piedmont Plateau: Which is surrounded by-mountain range on one side and by plain or ocean on the other side. For Example Appalachian Mountains (USA) and Patagonian plateau of South America.
  3. Dome Shaped Plateau: These Plateaus are formed when the landmass is uplifted in such a manner that the middle portion is raised and the sides are rounded. Chhotanagpur plateau of Jharkhand, Ozark Plateau (USA).
  4. Continental Plateau: These are very extensive Plateau and surrounded by oceanic coasts or plains. These are also called Shield. For Example Siberian shield.
  5. Volcanic Plateau: These Plateau are formed due to accumulation of thick layers of bassltic laves. Deccan plateau of India and Columbian plateau of USA are the best example of this type.
Plateaus
Location
Anatolia
Turkey
Meseta
Iberian Peninsula
Chiyapas
S. Mexico
Alaska / Yukon
USA
Columbian
USA
Great Basin
USA
Colorado
USA

Ocean Currents

When ocean water moves in a fixed direction within a fixed limit (of area) with very high velocity, it is called current. The velocity of a current is more than that of drift. | Ocean currents can be divided into two type warm currents and cold currents. The currents flowing from the equator to the poles are warm and those flowing from poles to the equator are cold.
Due to Coriolis force, the Ocean currents in the Northern Hemisphere deflect towards their right and those in the Southern Hemisphere, towards their left. The only exception of this rule of the flow of ocean is found in the Indian Ocean, where the direction of current flow changes with the change in the direction monsoon wind flow.
Ocean currents influence the climate of bordering coastal regions. They affect temperature, humidity and precipitation.
Coral Reefs
Coral reefs are the regions of very high bio-diversity. These are formed due to accumulation and solidification of skeletons of lime secreting organism known as coral polyps. They are dominating rocks. Coral reefs are of three types :
  1. Fringing Reef: Coral reefs developed along the coasts are called fringing reefs. Examples: Gulf of Mannar (india), Southern Florida (USA) etc.
  2. Barrier Reef : The coral reefs qf the coastal platforms are called "barrier reefs". There is extensive but shallow lagoon between the coastal land and the reef. Great Barrier Reef, located parallel to the east coast of Australia, is the largest of all the barrier reefs of the world.
  3. Coral Ring or Atoll : A ring of narrow growing corals of horse-shoe shape is called atoll. It is generally found around an island or in elliptical form on a submarine platform. Examples : Fiji Atoll, Funfutti Atoll etc.
Tides
Rise and fall of the ocean water level due to the gravitational forces of the Sun and the Moon are referred to as Tides. The waves generated by tide-are called Tidal Waves. The hight of the tides at different places varies a lot due to several factors such as - depth of water, the coastal features and openness or closeness of the sea. Though the Sun is far bigger than the moon yet, the gravitational force of the Moon is double than that of the sun. This is due to the fact that the Sun is at a greater distance than the Moon, from the Earth.
Every place, along the coast, experiences tide and ebbs twice in 24 hours. When the Sun, the Earth and the Moon are aligned in a straight line this position is referred to as SYZYGY. The combined forces of the Sun and the Moon result into High or Spring Tides. High tides are experienced on the full moon and the new moon.
Unlike this, when the Sun, the Earth and the Moon are aligned in a right angle position, the gravitational forces of the Sun and the Moon work against each other, when Neap or Low Tides are experienced. The part of the Earth facing the Moon , experiences a tide due to the gravitational pull of the Moon, but, at the same time the part of the Earth on the Opposite side also experidences a tide. This is due to the strong centrifugal force to balance the rotation of the earth.

Wednesday, 18 December 2013

Free Download YOJANA Magazine Archives: Any language, Any Issue, Any Month, Any Year

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Tuesday, 17 December 2013

SSC COMBINED HIGHER SECONDARY 10+2 (2013) LEVEL EXAM, OFFICIAL ANSWER KEY

Combined Higher Secondary (10+2) Level Exam, 2013- keys used
by the Commission for the different question paper/Test Forms Booklets
CLICK HERE TO VIEW WRITE UP-http://ssc.nic.in/whats%20new%20html/latest_news/chsl%20answer%20key2013.pdf

CLICK HERE TO VIEW KEY 20.10.2011-http://ssc.nic.in/whats%20new%20html/latest_news/KEY201013.pdf

CLICK HERE TO VIEW KEY 27.10.2013-http://ssc.nic.in/whats%20new%20html/latest_news/KEY271013.pdf

CLICK HERE TO VIEW KEY 10.11.2013 -http://ssc.nic.in/whats%20new%20html/latest_news/KEY101113.pdf

Various Buildings

Adoble
A house made from sun-dried bricks of clay and straw - usually built in warm, dry climates like the south western U.S.
Apartment
A set of rooms in a building which usually contains other similar sets of rooms.
Barracks
A building or set of buildings used to house soldiers.
Boardinghouse
A house in which rooms are rented and meals are served in a common dining room.
Bungalow
A small house with a low,wide roof and a porch. It is usually one story high.
Chalet
A mountain house with a wide,overhanging roof and posts and beams. The style originated in Switzerland.
Chateau
A home for nuns.
Cottage
A small country home or summer house used for vacations.
Duplex Apartment
An apartment with two floors of living space.
Duplex House
A house divided into two living units.
Estate
A large country house with seperate buildings on a large tract of land.
Farmhouse
Thie dwelling for people who live and work on a farm raising animals or crops.
Flat
An apartment on one floor of a building.
Geodesic Dome
A large, flat-bottom boat used as a home.
Hogan
A building made of logs and mud, used by the Navaho Indians.
Igloo
A house built by Eskimos of blocks of ice. The name means "hot house".
Jacal
A thatched hut made of intertwined branches and mud, built in Mexico.
Konah
A large home in Turkey.
Lodge
A house usually located in a remote place and used for hunting or skiing.
Loft
An apartment in a warehouse or business building.
Log Cabin
A small house made of unhewn timber.
Manse
In Scotland, a house in which a minister lives.
Mobile Home
A trailor used as a permanent home and made without a permanent foundation.
Nissen Hut
A premade shelter with a semicircular arching roof of corrugated iron, and containing a cement floor.
Octagon House
A house with eight sides.
Palace
A large, grand building in which royally live.
Penthouse
A large apartment located at the top of building.
Quonest Hut
A premade, portable circular hut made of metal and used by the U.S. Army.
Rectory
The house in which a Roman Catholic priest or Episcopal cergyman lives.
Shanty
A shack.
Sod House
A house made of bricks of sod, which is earth with grass and its roots. In the 19th century, these were built on the American prairie where there were no trees. Just grassy land.
Studio Apartment
A one-room apartment with a kitchen and bathroom.
Tent
A portable house made of skins, Canvas, or nylon.
Tepee, Tipi
A cone-shaped portable home made of buffalo skins and tree saplings, used by the American Indians of the Great Plains.
Tenement`
A rundown, low-rent apartment building.
Underground House
An earth shelter built below the ground. The earth keeps the house warm in the winter and cool in the summer.
Villa
A large country or resort home.
Wigwarm
A hut with a frame made of poles and covered iwht bark,rush mats, or hides, used by American Indians.
Yurt
A circular, portable, hut used as a home by asian shepherds. It is similar to the American wigwarm.
Zareba
An African fort made of thorny bushes.

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All the Best