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Mountains
& Life
'We
go over 4000 or 5000 metre mountains every week and work all year round in all
terrains and climate conditions.....with no health insurance...'
An overview of the importance of
mountains in sustainable development
Mountain ecosystems are found throughout the world,
from the equator almost to the poles, occupying approximately one-fifth of its
land surface. Beyond their common characteristics of having high relative relief
(or very marked topographic variation) and steep slopes, mountains are
remarkably diverse (Ives. Messerli and Spiess, 1997). They are found on every
continent, and at every altitude, from close to sea level to the highest place
on the earth - the summit of Mount Everest (Sagarmatha or Qomolangma) on the
border between Nepal and the Tibet Autonomous Region of China.
Half of the world's population depends on mountain water
An estimated one-tenth of the human population derive
their life-support directly from mountains. Yet, mountains are important not
only for their inhabitants, but for millions of people living in lowlands. At
the global scale, mountains' greatest value may be as sources of all the world's
major rivers, and many smaller ones (Mountain Agenda, 1998). Mountains play a
critical role in the water cycle by capturing moisture from air masses; when
this precipitation falls as snow, it is stored until it melts in the spring and
summer, providing essential water for settlements, agriculture and industries
downstream - often during the period of lowest rainfall. In semi-arid and arid
regions, over 90 percent of river flow comes from the mountains. Even in
temperate Europe, the Alps that occupy only 11 percent of the area of the Rhine
river basin supply 31 percent of the annual flow - and in summer more than 50
percent.
Mountain water is also a source of hydroelectric
power, most of which is used on the plains below. Historically, water wheels
have provided energy in mountain regions, mainly for grinding grain. In rural
Nepal there are an estimated 25 000 water wheels and over 900 micro-hydropower
turbines - a more recent technology - that provide a critical source of energy,
mainly for agroprocessing (Schweizer and Preiser, 1997). Such local renewable
energy is a vital catalyst for economic development in areas that are at the far
ends of the distribution networks for the fossil fuels on which most urban
dwellers depend. In developing countries, wood fuel is the predominant energy
source in mountain settlements, but it is also essential - whether as wood or
charcoal - to many people living in urban centres in the lowlands and on the
plains. For example, any visitor to Marrakech can observe the large piles of
fuelwood stacked outside communal bakeries, to which every household brings its
daily bread to be baked; the wood comes from the forests in the Atlas Mountains.
Mountain wood also has many other uses,
including timber and wood products both for local use and, where road, rail or
water networks permit, for export. It is significant to note, however, that,
while deforestation of the tropical rain forests remains most visible in the
global media, the highest rate of deforestation in any biome occurs in tropical
upland forests -1.1 percent per year. Rates of clearing are particularly high in
Central America, East and Central Africa, Southeast Asia and the Andes (FAO,
1993).
CENTRES OF BIODIVERSITY
Mountain ecosystems are globally important as centres
of biological diversity. The greatest diversity of vascular plant species occurs
in mountains: Costa Rica, the tropical eastern Andes, the Atlantic forest of
Brazil, the eastern Himalaya-Yunnan region, northern Borneo and Papua New Guinea
(Barthlott, Lauer and Placke, 1996). Other important centres are found in arid
subtropical mountains. Many of these areas with the greatest biological
diversity are designated as national parks or other types of protected area.
Mountains are
important centres of biodiversity: mowing mountain meadows to maintain
biodiversity, La Vanoise National Park, France
It is not only the diversity of natural mountain
species that is of value to humankind, both intrinsically and as a source of "wild
foods" such as mushrooms, game and birds, and many other non-timber forest
products. Mountains are also important as centres of crop diversity. The
maintenance and expansion of mountain populations in many parts of the world
have been made possible by the introduction of potatoes and maize from Latin
America. The original precursors of wheat came from the mountains of the Near
East. These original varieties maintain their importance in the breeding of new
varieties of major food crops. Equally, species that are not widely known but
are adaptable and nutritious - such as many of the Latin American root and tuber
crops which are the focus of research at the International Potato Center (CIP)
in Peru - may be potential major sources of food.
INFLUENCE OF CHANGES IN GLOBAL SYSTEMS
The economic relationships of mountain communities are
also undergoing transformation. Even the most remote mountain community has
always been linked to regional or global markets for essential commodities such
as salt. Until quite recently, however, the economies of most mountain societies
in the developing world were largely internal, based on the complementary use of
resources in different altitudinal zones. Connections to outside economies have
been driven by a number of factors, notably increases in accessibility owing to
the construction of new road networks and the rapid expansion of air transport
since the Second World War. In Nepal, the availability of surplus military
helicopters from the former Union of Soviet Socialist Republics means that small
villages, formerly many days' walk from Kathmandu, are now accessible in an hour
or less. Similarly, small communities in the mountains of Siberia and in the
Tien Shan of Kyrgyzstan may no longer be isolated.
While the helicopters carry some local people, their
principal passengers are usually tourists from all parts of the world - the
latest followers of a trend that began in the early nineteenth century with the
discovery of the Swiss Alps by English travellers. In an increasingly urbanized
world, the importance of mountain regions as global centres of tourism continues
to grow. The reasons for travel are highly diverse. Old forms, such as
pilgrimage, still exist and have major influences on regional economies; for
example, 9.3 million pilgrims arrive each year at Hardwar-Rishikesh, the entry
point into the Garhwal Himalaya. Badrinath, one of the major sites, is visited
by about 450 000 people a year, representing a threefold increase in two decades
(Academy for Mountain Environics, 1995). The growing number of tourists
attracted by the remarkable scenery and unfamiliar cultures of Nepal has been
even greater - from 9 526 in 1964 to 293 567 in 1993. Relatively few governments
have taken the steps of the Royal Government of Bhutan or the Zuni Nation of New
Mexico to limit the number of tourists; the world's largest industry is widely
seen as a motor for economic development (Price, Moss and Williams, 1997).
Yet tourism is a fickle industry. As Nepali Sherpas
noted in the 1980s, "tourists are like so many cattle, representing highly
mobile, productive, and prestigious, but perishable, forms of wealth. Like
cattle, tourists give good milk, but only if they are well fed" (Fisher, 1990,
p. 123). A decline in the reliability of tourism had already been noted in the
Swiss Alps, where the industry is undergoing a period of reorganization. Many
people will always want to visit the mountains to test their physical endurance,
escape from the pressures of everyday life, or visit sacred sites and places of
inspiration, but the vagaries of tourism are as dynamic as the physical
environment to which long-established mountain communities have learned to adapt.
In a world increasingly influenced by global forces, highland people need to
find new ways to survive and prosper. In the new parlance, this is sustainable
development, and its fostering is vital not only to mountain people, but to the
billions living downstream or farther away but linked through the global
transportation network.
The Andes
'The longest Mountain chain
in the world'
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The Andes Mountains are
located in South America, running north to south along the western coast
of the continent. The latitude is 10° N. to 57° S. The longitude is 70°
W. to 80° E. The
Andes Mountains are the longest and one of the highest mountain ranges
in the world. They are located in South America and stretch 4,500 miles
from north to south, along the west coast of the continent.
The climate is not the
same throughout the biome because there are places nearer to the equator
than others. The Andes are separated into three natural regions: the
southern, central, and northern regions. In the northern region, it is
hotter because it is closest to the equator. There are rain forests in
this region, due to the more humid, rainy climate. In the southern
region, the mountains are nearer to the Antarctic and it is much colder.
It is not very populated in the southern area.
In the central region
of this biome, the weather is more mild because it is not near either
the equator or the cold Antarctic. The largest herb in the world, Puya
raimondii, grows in this region and can survive at high elevations up to
13,000 feet. The herb can also live for 100 years. The herb's leaves all
grow from one big stem, which allows for moisture to run down the leaves
to the base of the plant. So during times of drought, the plant can
survive.
Many of the plants
which grow in the Andes Mountains are small in size to conserve energy.
Their leaves can be stiff and strong to protect them from frost and cold
weather if they are high in the mountains.
The Andes Mountains
supply many birds with homes like the Flamingo, Andean Flicker, the
Condor, and the Hillstar Hummingbird. Types of land animals include the
Mountain Lion, the Red Perll, and Llamas to name a few. The Spectacled
Bear also lives in this biome. The Giant Toad and Andean Iguana are some
examples of reptiles. This iguana is one of the few lizards found in
that cold climate.
The Andes Mountains
are hurt by humans because they cut down trees which shelter many unique
Andean animals. Man also mines for gold, silver, and copper which then
erodes the soil and hurts the plants of the Andes.
by Alan W. 2002 |
| Ancient fossils
of marine animals lie buried in the icy
peaks of the
Himalayas, the highest mountain
system in the world. During the Paleozoic and Mesozoic eras (570
million to 65 million years ago) the rocks that form the
Himalayas were being laid down as
sediment on the floor of an ancient sea. |
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Today, more than 30 Himalayan peaks rise to heights of
7,620 metres (25,000 feet) or more. One of these peaks,
Mount Everest, is the world’s highest mountain, at 8,848 metres (29,028
feet). This ancient marine sediment was thrust upwards when
India, then an island,
moved north and collided with the Asian continent.
The principal phase of uplift began 65 million years ago and is still continuing,
though uplift rates have been waning for the past 12 million years.
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Geologists recognize that
movements in the earth’s crust,
such as those that formed the Himalayas, have created most of
the major mountain belts in the world. According to the theory
of plate tectonics, the earth’s crust is made up of about a
dozen large rigid plates that
move a few centimeters per year independently. |
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| The tallest and most
spectacular mountains form along convergent plate boundaries, where the
adjacent plates are moving towards one another. |
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Uplift
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collision between plates triggers deformation and
thickening of the crust, which in turn leads to crustal
uplift and mountain formation. A common process produced
by horizontal compression is the deformation of layers
into folds or wrinkles.
The Himalayas, for example,
rose as a result of the compression and deformation that
accompanied the collision of the
Indo-Australian Plate with the
Eurasian Plate.
Compression generated by the collision of the
African Plate and the
Eurasian Plate formed Europe’s
Alps and the Jura
Mountains. |
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Some mountain belts, such
as the Andes in
South America,
result from the convergence of a continental
plate and an oceanic
plate. In these cases, the heavier oceanic plate
is subducted, or forced under, the continental
plate and partially melts, generating new
magma. This
magma solidifies as light, relatively buoyant
rock beneath the mountains and helps cause
uplift. Similarly, most of North America’s
Rocky Mountains
were formed in response to the subduction of
oceanic plates beneath the plate margin of
western North America.
This kind of mountain building is often called
orogeny.
Local uplift can also
result from continental extension or rifting,
the process that eventually breaks continents up
into two or more pieces. Usually, rifting within
continents is confined to long, narrow zones
bounded by normal
faults with a central downdropped block
and uplifted sides. The
Great Rift Valley of eastern
Africa is a famous
example of a continental rift.
Basin and
mountain structures such as those of
Nevada in the
United States and
the Mexican state of
Sonora are also due to crustal extension
and normal faulting, but over a broad area
rather than confined to a narrow
rift valley.
Crustal extension also occurs in the oceanic
realm. In fact, the mid-oceanic rift system,
which is almost entirely under water, is the
longest continuous mountain belt on the earth,
extending into all the major oceans.
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IN THE
NEXT 20 YEARS THERE WILL BE NO GLACIERS
LEFT IN MOST OF THE ANDEAN MOUNTAINS
(GLOBAL WARMING).
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THE GUIDES,
2007 |
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