Monday, 1 April 2013

SOUTH EAST ASIA


SOUTH EAST ASIA MAP

South East Asia countries


Brunei 


Cambodia


East Timor


Indonesia


Laos


Malaysia


Burma


Philiphines


Singapore


Thailand


Vietnam

Major geographical physical regions and climate

THAILAND

Land boundaries
  •  514,000 square kilometers lie in the middle of mainland Southeast Asia. The nation's axial position influenced many aspects of Thailand's society and culture—it controls the only land route from Asia to Malaysia and Singapore
  • Border countries: Myanmar, Cambodia, Laos, Malaysia
  • ·         Land: 511,770 square kilometres (197,600 sq mi)
    ·         Water: 2,230 cubic kilometres (540 cu mi)
    Thailand uses a unit of land area called the Rai (unit), which is 1,600 square metres (0.40 acre).
    Elevation extremes
    ·         Highest point: Doi Inthanon, 2,565 metres (8,415 ft), at 18°35′32″N 98°29′12″E
    ·         Lowest point: Gulf of Thailand, 0 metres - sea level

    Provinces
    Thailand's regions are further politically divided into a total of 77 provinces,such as Ratchaburi,Petchaburi etc. plus Bangkok, which is a special administrative area. The country's provinces have the same names as their respective capitals.
    Climate
    Most of Thailand has a Tropical wet and dry or savanna climate (Aw) according to the Köppen climate classification, while the South and the eastern tip of the East have a tropical monsoon climate (Am); countrywide, temperatures normally range from an average annual high of 38 °C (100.4 °F) to a low of19 °C (66.2 °F). During the dry season, the temperature rises dramatically in the second half of March, spiking to well over 40 °C (104 °F) in some areas by mid April when the Sun passes the Zenith. Southwest monsoons that arrive between May and July (except in the South) signal the advent of the rainy season (ruedu fon), which lasts into October and the cloud covering reduces the temperature again but the high humidity is experienced as 'hot and sticky'. November and December mark the onset of the dry season and night temperatures on high ground can occasionally drop to a light frost. Temperatures begin to climb in January, and a hot sun parches the landscape. The dry season is shortest in the South because of the proximity of the sea to all parts of the Malay Peninsula. With only minor exceptions, every area of the country receives adequate rainfall, but the duration of the rainy season and the amount of rain vary substantially from region to region and with altitude. The Northeast experiences a long dry season although the dry 2007/2008 season lasted only from late November through mid March. Its red,(laterite) dense clayey soils retain water well, which limits their agricultural potential for many crops but is ideal for keeping the water in the paddy fields and local village reservoirs. The well drained, loose sandy alluvium of the Mekong flood plain is very fertile, the main crops being tomatoes on an industrial scale, tobacco, and pineapples.
    DEMOGRAPHY
    POPULATION
    Thailand population is 67, 041, 000( 67 million )
    Thailand’s population is relatively homogeneous, however, this is changing due to immigration. More than 85% speak a Tai language and share a common culture. This core population includes the central Thai (33.7% of the population, including Bangkok’s population), Northeastern Thai or Lao (34.2%), northern Thai (18.8%), andsouthern Thai (13.3%).
    ETHNIC
    Thailand's population is relatively homogeneous, however, this is changing due to immigration. Ethnic Tais make up the majority of the population with 75 percent of all inhabitants. Thai Chinese make up 14 percent with the remaining 11 percent made up of various other groups.
    The language of the central Thai population is the educational language and administrative language. Several other small Tai groups include the Shan, Lue, and Phutai.
    Malay and Yawi-speaking Muslim's language of the south comprise another significant minority group (2.3%). Other groups include the Khmer; the Mon, who are substantially assimilated with the Thai; and the Vietnamese. Smaller mountain-dwelling tribes, such as the Hmong and Mein, as well as the Karen, number about 788,024. Some 300,000 Hmong, who ironically have lived this area for more generations than the Thais themselves, are to receive citizenship by 2010.
    Thailand is also home to a significant number of registered foreigners from Asia, Europe, and North America, as well as an estimated several hundred thousand illegal immigrants, some of which are natives. Increasing numbers of migrants from Burma, Laos, and Cambodia as well as nations such as Nepal, India, along with those from the West and Japan have pushed the number of non-nationals residing in Thailand to close to 2 million in 2008, up from about 1.3 million in the year 2000. A rising awareness of minorities is slowly changing attitudes in a country where non-nationals, some having resided in what is now Thailand longer than the Thais themselves, are barred from numerous privileges ranging from healthcare, ownership of property, or schooling in their own language.
    RELIGION

    Theravada Buddhism is the official religion of Thailand and is officially the religion of about 97% of its people. However, the true figure lies closer to 85%, Muslims are some 10% and 5% other religions including Christianity, Hinduism, especially among immigrants. In addition to Malay and Yawi speaking Thais and other southerners who are Muslim, the Cham of Cambodia in recent years begun a large scale influx into Thailand. The government permits religious diversity, and other major religions are represented, though there is much social tension, especially in the South.Spirit worship and animism are widely practiced.
    NATURAL RESOURCES
    Natural Resources & Landforms in Thailand
    Natural Resources
     The natural resources in Thailand consists of tin, rubber, natural gas, tungsten, tantalum, timber, lead, fish, gypsum, lignite, fluorite and arable land. Thailand's is the world's largest exporter of rice. The most produced strain of rice in Thailand is jasmine rice. The rice fields in Thailand takes up a total of 9.2 million hectares.
     Volcanoes in Thailand
      The two volcanoes in Thailand, which are already extinct, are called Phanom Rung(1200 feet) and Doi Pha Khok Hin Fu(1480 feet). 
     Mountains in Thailand
    There are more than 50 mountains in Thailand, Many mountains in the country are not important because of their height, but because of their symbolic and cultural significance. Some mountains have Buddhist worship places on top, like Doi Suthep close to Chiang Mai, while others have been adopted as provincial symbol, like relatively small Khao Sam Muk in Chonburi Province.


    VIETNAM
    Vietnam is located on the eastern margin of the Indochinese peninsula and occupies about 331,211.6 square kilometers, of which about 25% was under cultivation in 1987. It borders the Gulf of Thailand, Gulf of Tonkin, and South China Sea, alongside China, Laos, and Cambodia. The S-shaped country has a north-to-south distance of 1,650 kilometers and is about 50 kilometers wide at the narrowest point. With a coastline of 3,260 kilometers, excluding islands, Vietnam claims 12 nautical miles (22.2 km; 13.8 mi) as the limit of its territorial waters, an additional 12 nautical miles (22.2 km; 13.8 mi) as a contiguous customs and security zone, and 200 nautical miles (370.4 km; 230.2 mi) as an exclusive economic zone.
    The boundary with Laos, settled, on both an ethnic and geographical basis, between the rulers of Vietnam and Laos in the mid-seventeenth century with the Annamite Range as a reference, was formally defined by a delimitation treaty signed in 1977 and ratified in 1986. The frontier with Cambodia, defined at the time of French annexation of the western part of the Mekong River Delta in 1867, remained essentially unchanged, according to Hanoi, until some unresolved border issues were finally settled in the 1982-85 period. The land and sea boundary with China, delineated under the France-China treaties of 1887 and 1895, is "the frontier line" accepted by Hanoi that China agreed in 1957- 58 to respect. However, in February 1979, following China's limited invasion of Vietnam, Hanoi complained that from 1957 onward China had provoked numerous border incidents as part of its anti-Vietnam policy and expansionist designs in Southeast Asia. Among the territorial infringements cited was the Chinese occupation in January 1974 of the Paracel Islands, claimed by both countries in a dispute left unresolved in the 1980s.
    Vietnam is a country of tropical lowlands, hills, and densely forested highlands, with level land covering no more than 20% of the area. The country is divided into the highlands and the Red River delta in the north; and the Dãy Trường Sơn (Central mountains, or the Chaîne Annamitique, sometimes referred to simply as "the Chaine."), the coastal lowlands, and the Mekong River Delta in the south.

    Highlands
    The highlands and mountain plateaus in the north and northwest are inhabited mainly by tribal minority groups. The Dãy Trường Sơn (Annamite Range) originates in the Tibetan and Yunnan regions of southwest China and forms Vietnam's border with Laos. It terminates in the Mekong River Delta north of Hồ Chí Minh City (formerly Saigon).
    These central mountains, which have several high plateaus, are irregular in elevation and form. The northern section is narrow and very rugged; the country's highest peak, Fan Si Pan, rises to 3,142 meters in the extreme northwest. The southern portion has numerous spurs that divide the narrow coastal strip into a series of compartments. For centuries these topographical features not only rendered north-south communication difficult but also formed an effective natural barrier for the containment of the people living in the Mekong basin.


    Coastal lowlands
    The narrow, flat coastal lowlands extend from south of the Red River Delta to the Mekong River basin. On the landward side, the Dãy Trường Sơn rises precipitously above the coast, its spurs jutting into the sea at several places. Generally the coastal strip is fertile and rice is cultivated intensively.

    CLIMATE
    Vietnam in the northern regions have a humid subtropical climate, with humidity averaging 84% throughout the year. However, because of differences in latitude and the marked variety of topographical relief, the climate tends to vary considerably from place to place. During the winter or dry season, extending roughly from November to April, the monsoon winds usually blow from the northeast along the China coast and across the Gulf of Tonkin, picking up considerable moisture; consequently the winter season in most parts of the country is dry only by comparison with the rainy or summer season. During the southwesterly summer monsoon, occurring from May to October, the heated air of the Gobi Desert rises, far to the north, inducing moist air to flow inland from the sea and deposit heavy rainfall. The climate in the southern regions especially Ho Chi Minh City and surrounding Mekong Delta is predominantly Tropical savanna climate with high humidity and a distinct wet and dry season.
    Annual rainfall is substantial in all regions and torrential in some, ranging from 1,200 to 3,000 millimeters (47.2 to 118.1 in). Nearly 90% of the precipitation occurs during the summer. The average annual temperature is generally higher in the plains than in the mountains and plateaus. Temperatures range from a low of 5 °C (41 °F) in December and January, the coolest months, to more than 37 °C (98.6 °F) in April, the hottest month. Seasonal divisions are more clearly marked in the northern half than in the southern half of the country, where, except in some of the highlands, seasonal temperatures vary only a few degrees, usually in the 21–28 °C (69.8–82.4 °F) range.
DEMOGRAPHY

VIETNAM POPULATION

The total population in Vietnam was last recorded at 87.8 million people in 2011 from 34.7 million in 1960, changing 153 percent during the last 50 years. Population in Vietnam is reported by the the World Bank. Historically, from 1960 until 2011, Vietnam Population averaged 60.6 Million reaching an all time high of 87.8 Million in December of 2011 and a record low of 34.7 Million in December of 1960. The population of Vietnam represents 1.27 percent of the world´s total population which arguably means that one person in every 79 people on the planet is a resident of Vietnam. This page includes a chart with historical data for Vietnam Population.

ETHNICS
Vietnam has one of the most complex ethnolinguistic patterns in Asia. The Vietnamese majority was significantly Sinicized during a millennium of Chinese rule, which ended in ad 939. Indian influence is most evident among the Cham and Khmer minorities. The Cham formed the majority population in the Indianized kingdom of Champa in what is now central Vietnam from the 2nd to the late 15th century ad. Small numbers of Cham remain in the south-central coastal plain and in the Mekong delta near the Cambodian border. The Khmer (Cambodians) are scattered throughout the Mekong delta.

RELIGION
The major religious traditions in Vietnam are Buddhism (which fuses forms of Taoism and Confucianism),Vietnam religionChristianity (Catholicism and Protestantism), Islam, Caodaism and the Hoa Hao sect.

Buddhism
Buddhism was first introduced to Vietnam in the 2nd century, and reached its peak in the Ly dynasty (11th century). It was then regarded as the official religion dominating court affairs. Buddhism was preached broadly among the population and it enjoyed a profound influence on people's daily life. Its influence also left marks in various areas of traditional literature and architecture. As such, many pagodas and temples were built during this time.
Vietnam religion

At the end of the 14th century, Buddhism began to show signs of decline. The ideological influence of Buddhism, however, remained very strong in social and cultural life. Presently, over 70 percent of the population of Vietnam are either Buddhist or strongly influenced by Buddhist practices.

Catholicism
Catholicism was introduced to Vietnam in the 17th century. At present the most densely-populated Catholic areas are Bui Chu-Phat Diem in the northern province of Ninh Binh and Ho Nai-Bien Hoa in Dong Nai Province to the South. About 10 percent of the population are considered Catholic.
Vietnam religion

Protestantism
Protestantism was introduced to Vietnam at about the same time as Catholicism. Protestantism, however, remains an obscure religion. At present most Protestants live in the Central Highlands. There still remains a Protestant church on Hang Da Street in Hanoi. The number of Protestants living in Vietnam is estimated at 400,000.

Islam
Islamic followers in Vietnam are primarily from the Cham ethnic minority group living in the central part of the central coast. The number of Islamic followers in Vietnam totals about 50,000. 
Vietnam religion

Caodaism
Caodaism was first introduced to the country in 1926. Settlements of the Cao Dai followers in South Vietnam are located near the Church in Tay Ninh. The number of followers of this sect is estimated at 2 million.

Hoa Hao Sect
The Hoa Hao Sect was first introduced to Vietnam in 1939. More than 1 million Vietnamese are followers of this sect. Most of them live in the south-west of Vietnam.

Mother Worship (Tho Mau)
Vietnam religion
Researchers describe the Vietnamese mother-worship cult as a primitive religion. Mother, Me in the Vietnamese language, is pronounced Mau in Sino-­script. The mother worship cult might be originated from the cult of the Goddess in ancient ages. In the Middle Ages, the Mother was worshipped in temples and palaces. Due to the fact that it is a worshipping custom and not a religion, the Mother worshipping cult has not been organized as Buddhism and Catholicism have. As a result, the different affiliations of the cult have yet to be consistent and different places still have different customs.
The custom of Mother worship originated from the north. In the south, the religion has integrated the local goddesses such as Thien Y A Na (Hue) and Linh Son (Tay Ninh).

In fact, the Mother worship cult was influenced by other religions, mainly Taoism.
  • NATURAL RESOURCES
Although Vietnam is relatively rich in natural resources, the country's protracted state of war has precluded their proper exploitation. Coal reserves, located mainly in the North, have been estimated at 20 billion tons. With Soviet assistance, coal mining has been expanded somewhat. Commercially exploitable metals and minerals include iron ore, tin, copper, lead, zinc, nickel, manganese, titanium, chromite, tungsten, bauxite, apatite, graphite, mica, silica sand, and limestone. Vietnam is deficient, however, in coking coal, which, prior to the outbreak of hostilities with China in 1979, it traditionally imported from the Chinese. Gold deposits are small.
Vietnam's production of crude oil and natural gas was in very preliminary stages in the late 1980s and the amounts of commercially recoverable reserves were not available to Western analysts. With the cooperation of the Soviet Union, Vietnam began exploitation of a reported 1-billion-ton offshore oil find southeast of the Vung Tau-Con Dao Special Zone (see fig. 1). By early 1987, the Vietnamese were exporting crude oil for the first time in shipments to Japan. Production remained low, estimated at about 5,000 barrels per day, although Vietnam's minimum domestic oil requirements totaled 30,000 barrels per day. Despite optimistic plans for developing offshore fields, Vietnam was likely to remain dependent on Soviet-supplied petroleum products through the 1990s.
Vietnam's ability to exploit its resources diminished in the early 1980s, as production fell from the levels attained between 1976 and 1980. In the 1980s, the need to regulate investment and focus spending on projects with a short-term payoff pointed to continued slow development of the country's resource base, with the exception of areas targeted by the Soviet Union for economic assistance, such as oil, gas, coal, tin, and apatite.
Vietnam's fisheries are modest, even though the country's lengthy coast provides it with a disproportionately large offshore economic zone for its size. In the 1980s, Vietnam claimed a 1-million-square- kilometer offshore economic zone and an annual catch of 1.3 to 1.4 million tons. More than half the fish caught, however, were classified as being of low-quality. Schools of fish reportedly were small and widely dispersed.
As the 1990s approached,it seemed increasingly likely that Vietnam's economy would remain predominantly agricultural. This trend, however, did not necessarily limit attainable economic growth since Vietnam processed a significant amount of unused land with agricultural potential. According to Vietnamese statistics of the mid 1980s, agricultural land then in use theoretically could be expanded by more than 50 percent to occupy nearly one-third of the nation. Funds and equipment for expensive land-reclamation projects were scarce, however, and foreign economists believed that a projected increase in agricultural land use of about 20 to 25 percent was more realistic. Even if the reclaimed land were only minimally productive, an increase in land use would increase agricultural output substantially.
Both the availability of land and the density of settlement in traditional agricultural areas--about 463 persons per square kilometer in the Red River Delta and 366 persons per square kilometer in the Mekong Delta-- explained much of the government's commitment to the building of new economic zones (see Glossary) in less-settled areas. During the period from 1976 to 1980, only 1.5 million out of the 4 million persons targeted for relocation actually were moved to new economic zones. The government's Third Five-Year Plan (1981-85) called for the relocation of 2 million people by 1985, and subsequent plans projected the resettlement of as many as 10 million by 1999. By the end of 1986, however, the Vietnamese reported that fewer than 3 million people had been resettled since the program began. Slow progress in bringing new land into production, low yields on reclaimed land, and hardships endured by resettled workers-- particularly former city dwellers, many of whom chose to return home--testified to the problems inherent in the resettlement program.

Thursday, 28 March 2013

SOUTH ASIA


SOUTH ASIA MAP



List of South Asia Countries :


  • Afghanistan
  • Bangladesh
  • Bhutan
  • India
  • Myanmar
  • Maldives
  • Nepal
  • Pakistan
  • Sri Lanka



  • Geographical Physical Regions of South Asia :


    While South Asia had never been a coherent geopolitical region, it has a distinct geographical identity.The boundaries of South Asia vary based on how the region is defined. South Asia's northern, eastern, and western boundaries vary based on definitions used, while the Indian Oceanis the southern periphery. Most of this region rests on the Indian Plate and is isolated from the rest of Asia by mountain barriers.The Indian Plate includes most of South Asia, forming a land mass which extends from the Himalayas into a portion of the basin under the Indian Ocean, including parts of South China and Eastern Indonesia, as well as Kuen Lun and Karakoramranges, and extending up to but not including LadakhKohistan, the Hindu Kush range and Balochistan.It may be noted that geophysically the Yarlung Tsangpo River river in Tibet is situated at the outside of the border of the Subcontinental structure, while the Pamir Mountains in Tajikistan are situated inside that border.
    Much of the region comprises a peninsula in south-central Asia, rather resembling a diamond which is delineated by the Himalayas on the north, the Hindu Kush in the west, and the Arakanese in the east,and which extends southward into the Indian Ocean with the Arabian Sea to the southwest and the Bay of Bengal to the southeast.
    Per the UN, the wider subregion's northern frontier is the Himalayas and southerly post-Soviet states of Central Asia (TajikistanUzbekistan, andTurkmenistan, bordering northern Afghanistan and Iran), its western boundary is the westerly border of Iran (with AzerbaijanArmeniaTurkey, andIraq), and its eastern boundary is the westerly border of Burma (with India and Bangladesh).
    Most of this region is a subcontinent resting on the Indian Plate (the northerly portion of the Indo-Australian Plate) separated from the rest of the Eurasian Plate. It was once a small continent before colliding with the Eurasian Plate about 50-55 million years ago and giving birth to theHimalayan range and the Tibetan plateau. It is the peninsular region south of the Himalayas and Kuen Lun mountain ranges and east of the Indus River and the Iranian Plateau, extending southward into the Indian Ocean between the Arabian Sea (to the southwest) and the Bay of Bengal (to the southeast).
    The region is home to a variety of geographical features, such as glaciersrainforestsvalleysdeserts, and grasslands that are typical of much larger continents. It is surrounded by three water bodies — the Bay of Bengal, the Indian Ocean and the Arabian Sea. The climate of this vast region varies considerably from area to area from tropical monsoon in the south to temperate in the north. The variety is influenced by not only the altitude, but also by factors such as proximity to the sea coast and the seasonal impact of the monsoons.


    Climate of The South Asia :

    Southern parts are mostly hot in summers and receive rain during monsoon period(s). The northern belt of Indo-Gangetic plains also is hot in summer, but cooler in winter. The mountainous north is colder and receives snowfall at higher altitudes of Himalyan ranges.

    As the Himalayas block the north-Asian bitter cold winds, the temperatures are considerably moderate in the plains down below. For most part, the climate of the region is called the Monsoon climate, which keeps the region humid during summer and dry during winter, and favors the cultivation of jutetearice, and various vegetables in this region.

    The Importance of Geographical Physical Regions and Climate for South Asia Tourism :

    • for the tourist attraction
    • can increase the loca ecnomies
    • can rate the tourism level
    INDIA



    demography india

    With 1,210,193,422 residents reported in the 2011 provisional census,India is the world's second-most populous country. Its population grew at 1.76% per annum during 2001–2011,down from 2.13% per annum in the previous decade (1991–2001).The human sex ratio, according to the 2011 census, is 940 females per 1,000 males.The median age was 24.9 in the 2001 census.The first post-colonial census, conducted in 1951, counted 361.1 million people.Medical advances made in the last 50 years as well as increased agricultural productivity brought about by the "Green Revolution" have caused India's population to grow rapidly.India continues to face several public health-related challenges.According to the World Health Organisation, 900,000 Indians die each year from drinking contaminated water or breathing polluted air.There are around 50 physicians per 100,000 Indians.The number of Indians living in urban areas has grown by 31.2% between 1991 and 2001.Yet, in 2001, over 70% lived in rural areas.According to the 2001 census, there are 27 million-plus cities in India;among them DelhiMumbaiKolkata,ChennaiBangaloreHyderabad and Ahmedabad are the most populous metropolitan areas. The literacy rate in 2011 was 74.04%: 65.46% among females and 82.14% among males.Kerala is the most literate state;Bihar the least.

    India is home to two major language familiesIndo-Aryan (spoken by about 74% of the population) and Dravidian (24%). Other languages spoken in India come from the Austroasiatic and Tibeto-Burman language families. India has no national language.Hindi, with the largest number of speakers, is the official language of the government.English is used extensively in business and administration and has the status of a "subsidiary official language";it is important in education, especially as a medium of higher education. Each state and union territory has one or more official languages, and the constitution recognises in particular 21 "scheduled languages". The Constitution of India recognises 212 scheduled tribal groups which together constitute about 7.5% of the country's population.The 2001 census reported that Hinduism, with over 800 million adherents (80.5% of the population), was the largest religion in India; it is followed by Islam (13.4%), Christianity (2.3%), Sikhism (1.9%), Buddhism (0.8%), Jainism (0.4%), JudaismZoroastrianism, and the Bahá'í Faith.India has the world's largest Hindu, Sikh, Jain, Zoroastrian, and Bahá'í populations, and has the third-largest Muslim population and the largest Muslim population for a non-Muslim majority country.

    Culture


    Warli tribal painting by Jivya Soma Mashe from Thane, Maharashtra
    Indian cultural history spans more than 4,500 years.During the Vedic period (c. 1700–500 BCE), the foundations of Hindu philosophymythology, and literature were laid, and many beliefs and practices which still exist today, such as dhármakármayóga, and mokṣa, were established.India is notable for its religious diversity, with Hinduism, Sikhism, Islam, Christianity, and Jainism among the nation's major religions.The predominant religion, Hinduism, has been shaped by various historical schools of thought, including those of the Upanishads,the Yoga Sutras, the Bhaktimovement,and by Buddhist philosophy.

    Art and architecture

    Much of Indian architecture, including the Taj Mahal, other works of Mughal architecture, and South Indian architecture, blends ancient local traditions with imported styles.Vernacular architecture is also highly regional in it flavours. Vastu shastra, literally "science of construction" or "architecture" and ascribed to Mamuni Mayan,explores how the laws of nature affect human dwellings; it employs precise geometry and directional alignments to reflect perceived cosmic constructs.As applied in Hindu temple architecture, it is influenced by the Shilpa Shastras, a series of foundational texts whose basic mythological form is the Vastu-Purusha mandala, a square that embodied the "absolute".The Taj Mahal, built inAgra between 1631 and 1648 by orders of Emperor Shah Jahan in memory of his wife, has been described in the UNESCO World Heritage List as "the jewel of Muslim art in India and one of the universally admired masterpieces of the world's heritage."Indo-Saracenic Revival architecture, developed by the British in the late 19th century, drew on Indo-Islamic architecture.

    geography

    India comprises the bulk of the Indian subcontinent and lies atop the minor Indian tectonic plate, which in turn belongs to the Indo-Australian Plate.India's defining geological processes commenced 75 million years ago when the Indian subcontinent, then part of the southern supercontinentGondwana, began a north-eastward drift across the then-unformed Indian Ocean that lasted fifty million years.The subcontinent's subsequent collision with, and subduction under, the Eurasian Plate bore aloft the planet's highest mountains, the Himalayas. They abut India in the north and thenorth-east.In the former seabed immediately south of the emerging Himalayas, plate movement created a vast trough that has gradually filled with river-borne sediment;it now forms the Indo-Gangetic Plain.To the west lies the Thar Desert, which is cut off by the Aravalli Range.
    The original Indian plate survives as peninsular India, which is the oldest and geologically most stable part of India; it extends as far north as the Satpuraand Vindhya ranges in central India. These parallel chains run from the Arabian Sea coast in Gujarat in the west to the coal-rich Chota Nagpur Plateauin Jharkhand in the east.To the south, the remaining peninsular landmass, the Deccan Plateau, is flanked on the west and east by coastal ranges known as the Western and Eastern Ghats;the plateau contains the nation's oldest rock formations, some of them over one billion years old. Constituted in such fashion, India lies to the north of the equator between 6° 44' and 35° 30' north latitude and 68° 7' and 97° 25' east longitude.


    India's coastline measures 7,517 kilometres (4,700 mi) in length; of this distance, 5,423 kilometres (3,400 mi) belong to peninsular India and 2,094 kilometres (1,300 mi) to the Andaman, Nicobar, and Lakshadweep island chains.According to the Indian naval hydrographic charts, the mainland coastline consists of the following: 43% sandy beaches; 11% rocky shores, including cliffs; and 46% mudflats or marshy shores.
    Major Himalayan-origin rivers that substantially flow through India include the Ganges and the Brahmaputra, both of which drain into the Bay of Bengal.Important tributaries of the Ganges include the Yamuna and the Kosi; the latter's extremely low gradient often leads to severe floods and course changes.[119]Major peninsular rivers, whose steeper gradients prevent their waters from flooding, include the Godavari, the Mahanadi, the Kaveri, and the Krishna, which also drain into the Bay of Bengal;and the Narmada and the Tapti, which drain into the Arabian Sea.Coastal features include the marshy Rann of Kutch of western India and the alluvial Sundarbans delta of eastern India; the latter is shared with Bangladesh.India has two archipelagos: the Lakshadweep, coral atolls off India's south-western coast; and the Andaman and Nicobar Islands, a volcanic chain in the Andaman Sea.
    The Indian climate is strongly influenced by the Himalayas and the Thar Desert, both of which drive the economically and culturally pivotal summer and wintermonsoons.The Himalayas prevent cold Central Asian katabatic winds from blowing in, keeping the bulk of the Indian subcontinent warmer than most locations at similar latitudes. The Thar Desert plays a crucial role in attracting the moisture-laden south-west summer monsoon winds that, between June and October, provide the majority of India's rainfall.Four major climatic groupings predominate in India: tropical wettropical drysubtropical humid, and montane

    natural resources india

    India's major mineral resources include Coal (fourth-largest reserves in the world), Iron ore, ManganeseMicaBauxiteTitanium ore, ChromiteNatural gasDiamondsPetroleumLimestone andThorium (world's largest along Tamil Nadus shores). India's oil reserves, found in Bombay High off the coast of MaharashtraGujaratRajasthan and in eastern Assam meet 25% of the country's demand.

    PAKISTAN




    climate

    Pakistan covers an area of 796,095 km2 (307,374 sq mi), approximately equal to the combined land areas of France and the United Kingdom. It is the36th largest nation by total area, although this ranking varies depending on how the disputed territory of Kashmir is counted. Pakistan has a 1,046 km (650 mi) coastline along the Arabian Sea and the Gulf of Oman in the south and land borders of 6,774 km (4,209 mi) in total: 2,430 km (1,510 mi) with Afghanistan, 523 km (325 mi) with China, 2,912 km (1,809 mi) with India and 909 km (565 mi) with Iran. It shares a marine border with Oman,and is separated from Tajikistan by the cold, narrow Wakhan Corridor.Pakistan occupies a geopolitically important location at the crossroads of South Asia, the Middle East and Central Asia.
    Geologically, Pakistan overlaps the Indian tectonic plate in its Sindh and Punjab provinces; Balochistan and most of Khyber Pakhtunkhwa are within theEurasian plate, mainly on the Iranian plateau. Gilgit–Baltistan and Azad Kashmir lie along the edge of the Indian plate and hence are prone to violent earthquakes. Ranging from the coastal areas of the south to the glaciated mountains of the north, Pakistan's landscapes vary from plains to deserts, forests, hills and plateaus.




    Pakistan is divided into three major geographic areas: the northern highlands, the Indus River plain and the Balochistan Plateau. The northern highlands contain the KarakoramHindu Kush and Pamir mountain ranges (see mountains of Pakistan), which contain some of the world's highest peaks, including five of the fourteen eight-thousanders (mountain peaks over 8,000 metres or 26,250 feet), which attract adventurers and mountaineers from all over the world, notably K2 (8,611 m or 28,251 ft) and Nanga Parbat (8,126 m or 26,660 ft).The Balochistan Plateau lies in the west and the Thar Desert in the east. The 1,609 km (1,000 mi) Indus River and its tributaries flow through the country from the Kashmir region to the Arabian Sea. There is an expanse of alluvial plains along it in Punjab and Sindh.
    The climate varies from tropical to temperate, with arid conditions in the coastal south. There is a monsoon season with frequent flooding due to heavy rainfall, and a dry season with significantly less rainfall or none at all. There are four distinct seasons: a cool, dry winter from December through February; a hot, dry spring from March through May; the summer rainy season, or southwest monsoon period, from June through September; and the retreating monsoon period of October and November.Rainfall varies greatly from year to year, and patterns of alternate flooding and drought are common.


    natural resources

    land, extensive natural gas reserves, limited petroleum, poor quality coal, iron ore, copper, salt, limestone

    domography


    With 180.1 million residents reported in 2012, Pakistan is the sixth most populated country in the world, behind Brazil and ahead of Bangladesh. Its 2.03% population growth rate is the highest among the SAARC countries and gives an annual increase of 3.6 million. The population is projected to reach 210.13 million by 2020 and to double by 2045. In 1947, Pakistan had a population of 32.5 million.From 1990 to 2009 it increased by 57.2%. By 2030 it is expected to surpass Indonesia as the largest Muslim-majority country in the world.Pakistan is a 'young' nation, with a median age of about 22 and 104 million people under 30 in 2010. Pakistan's fertility rate stands at 3.07, higher than its neighbours India(2.57) and Iran(1.73). Around 35% of the people are under 15
    The majority of southern Pakistan's population lives along the Indus River. Karachi is its most populous city.In the northern half of the country, most of the population lives in an arc formed by the cities of LahoreFaisalabadRawalpindiIslamabadGujranwalaSialkotGujrat,JhelumSargodhaSheikhupuraNowsheraMardan and Peshawar. During 1990–2008, city dwellers made up 36% of Pakistan's population, making it the most urbanised nation in South Asia.Furthermore, 50% of Pakistanis live in towns of 5,000 people or more.
    Expenditure on health was 2.6% of GDP in 2009.Life expectancy at birth was 65.4 years for females and 63.6 years for males in 2010. The private sector accounts for about 80% of outpatient visits. Approximately 19% of the population and 30% of children under five are malnourished. Mortality of the under-fives was 87 per 1,000 live births in 2009.About 20% of the population live below the international poverty line of US$1.25 a day.
    More than sixty languages are spoken in Pakistan, including a number of provincial languages. Urdu, the lingua franca and a symbol of Muslim identity and national unity, is the national language and is understood by over 75% of Pakistanis. English is the official language of Pakistan, used in official business, government, and legal contracts the local dialect is known as Pakistani EnglishPunjabi is the most common native language in Punjab and has many native speakers. Saraiki is mainly spoken in South PunjabPashto is the provincial language of Khyber Pakhtunkhwa, Sindhi is the provincial language of Sindh, and Balochi is dominant in Balochistan