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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...'

Mountains: globally important ecosystems

 

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'

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

 

Facts about Mountains
 

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.

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.

Formation of Mountains
 

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. 

The tallest and most spectacular mountains form along convergent plate boundaries, where the adjacent plates are moving towards one another.
 
Uplift
 

A 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.

 

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.

 

 

IN THE NEXT 20 YEARS THERE WILL BE NO GLACIERS LEFT IN MOST OF THE ANDEAN MOUNTAINS (GLOBAL WARMING).

 

THE GUIDES, 2007