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Geography of Vietnam
Vietnam is located in the southeastern extremity of the Indochinese peninsula
and occupies about 331,688 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 as the limit of its territorial waters, an
additional 12 nautical miles as a contiguous customs and security zone, and 200
nautical miles as an exclusive economic zone.
The boundary with Laos, settled, on an ethnic basis, between the rulers of
Vietnam and Laos in the mid-seventeenth century, 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.
Geographic coordinates: 16°00′N 108°00′E
Vietnam is located in the southeastern extremity of the Indochinese peninsula
and occupies about 331,688 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 as the limit of its territorial waters, an
additional 12 nautical miles as a contiguous customs and security zone, and 200
nautical miles as an exclusive economic zone.
The boundary with Laos, settled, on an ethnic basis, between the rulers of
Vietnam and Laos in the mid-seventeenth century, 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.
Geographic coordinates: 16°00′N 108°00′E
Physiography
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 Giai
Truong Son (Central mountains, or the Chaîne Annamitique, sometimes referred to
simply as "the Chaine."), the coastal lowlands, and the Mekong River Delta in
the south.
Red River Delta
The delta of the Red River (also known as the Sông Hồng), is a flat, triangular
region of 3,000 square kilometers, is smaller but more intensely developed and
more densely populated than the Mekong River Delta. Once an inlet of the Gulf of
Tonkin, it has been filled in by the enormous alluvial deposits of the rivers
over a period of millennia, and it advances one hundred meters into the Gulf
annually. The ancestral home of the ethnic Vietnamese, the delta accounted for
almost 70 % of the agriculture and 80 % of the industry of North Vietnam before
1975.
The Red River, rising in China's Yunnan province, is about 1,200 kilometers
long. Its two main tributaries, the Sông Lô (also called the Lo River, the
Riviere Claire, or the Clear River) and the Sông Da (also called the Black River
or Riviere Noire), contribute to its high water volume, which averages 500
million cubic meters per second, but may increase by more than 60 times at the
peak of the rainy season. The entire delta region, backed by the steep rises of
the forested highlands, is no more than three meters above sea level, and much
of it is one meter or less. The area is subject to frequent flooding; at some
places the high-water mark of floods is fourteen meters above the surrounding
countryside. For centuries flood control has been an integral part of the
delta's culture and economy. An extensive system of dikes and canals has been
built to contain the Red River and to irrigate the rich rice-growing delta.
Modeled on that of China's, this ancient system has sustained a highly
concentrated population and has made double-cropping wet-rice cultivation
possible throughout about half the region.
Highlands
The highlands and mountain plateaus in the north and northwest are inhabited
mainly by tribal minority groups. The Giai Truong Son (Annamite Range)
originates in the Tibetan and Yunnan regions of southwest China and forms
Vietnam's border with Laos and Cambodia. 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.
Central Highlands
Within the southern portion of Vietnam is a plateau known as the Central
Highlands (Tay Nguyen), approximately 51,800 square kilometers of rugged
mountain peaks, extensive forests, and rich soil. Comprising 5 relatively flat
plateaus of basalt soil spread over the provinces of Đắk Lắk (or "Dac Lac"), Gia
Lai, and Kon Tom, the highlands account for 16% of the country's arable land and
22% of its total forested land. Before 1975, North Vietnam had maintained that
the Central Highlands and the Giai Truong Son were strategic areas of paramount
importance, essential to the domination not only of South Vietnam but also of
the southern part of Indochina. Since 1975, the highlands have provided an area
in which to relocate people from the densely populated lowlands.
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 Giai Truong Son 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.
Mekong River Delta
The Mekong delta, covering about 40,000 square kilometers, is a low-level plain
not more than three meters above sea level at any point and criss-crossed by a
maze of canals and rivers. So much sediment is carried by the Mekong's various
branches and tributaries that the delta advances sixty to eighty meters into the
sea every year. An official Vietnamese source estimates the amount of sediment
deposited annually to be about 1 billion cubic meters, or nearly 13 times the
amount deposited by the Red River. About 10,000 square kilometers of the delta
are under rice cultivation, making the area one of the major rice-growing
regions of the world. The southern tip, known as the Cà Mau Peninsula, or Mui
Bai Bung, is covered by dense jungle and mangrove swamps.
The Mekong, which is 4,220 kilometers long, is one of the 12 great rivers of the
world. From its source in the Tibetan plateau, it flows through the Tibetan and
Yunnan regions of China, forms the boundary between Laos and Myanmar as well as
between Laos and Thailand, divides into two branches - the Song Hau Giang and
Song Tien Giang - below Phnom Penh, and continues through Cambodia and the
Mekong basin before draining into the South China Sea through nine mouths known
as the cuu long (nine dragons). The river is heavily silted and is navigable by
seagoing craft of shallow draft as far as Kompong Cham in Cambodia. A tributary
entering the river at Phnom Penh drains the Tonlé Sap, a shallow freshwater lake
that acts as a natural reservoir to stabilize the flow of water through the
lower Mekong. When the river is in flood stage, its silted delta outlets are
unable to carry off the high volume of water. Floodwaters back up into the Tonlé
Sap, causing the lake to inundate as much as 10,000 square kilometers. As the
flood subsides, the flow of water reverses and proceeds from the lake to the
sea. The effect is to reduce significantly the danger of devastating floods in
the Mekong delta, where the river floods the surrounding fields each year to a
level of one to two meters.
Climate
Vietnam has a tropical monsoon 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.
Annual rainfall is substantial in all regions and torrential in some, ranging
from 120 centimeters to 300 centimeters. 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
in December and January, the coolest months, to more than 37°C 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°C-28°C range. Wikipedia

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