Nepal
Saturday, October 2, 2010
INTRODUCTION.
Tuesday, September 28, 2010
DESERTED AREA OF NEPAL.
This area is situated in the north of the Great Himalayans which consist of Kanjiroba , Dhaulagiri , Annapurna Ι, ΙΙ, ΙΙΙ & ΙV , Lamjung, Himalchuli and Manaslu Himals. It comprises the area of Dolpa , Mustang Manang and even the upper part ot the Budi Gandaki river of the Gorkha district . In a simple word , it can be said that this area is the post –Himalayan one . as the Great Himalayas are situated on the south of this area , in the form of an obstacle to the flow of the monsoon from the south –east , this area is more or less completely rain –shaded and gets very little amount of precipitation. Because most of the monsoon precipitates to the south of the Himalayas , only the escaped- away part precipitates through some passes there. That is why, the rainfall in this part is corporately very low. For instance, Jomsom,the gateway of the Mustang district, though situated nearly on the border of the Himalayas and the deserted land of Mustang, still has and annual rainfall of about 324.2mm.which is , compared to other places in the southern part of the Great Himalayas, quite low . Jajarkot, situated on the south of Mt. Dhaulagiri , has an annual rainfall of about 1888.2mm. where as Jomsom has only 324.2mm. the further interior parts , Mustang, Manang and some parts of Dolpa, have still lower precipitation.
Suffering from this complete rain-shadow and very speedy winds of desiccating nature, the vegetation, here , is a sot of dry alpine deserted type. Nowhere are found trees , there are only shrubs and scrubs found as greeneries . It is otherwise a naked land suffering from very bad erosion problems . there are two types of erosion in this area. One is the splash erosion cased by the splashing effect of the rain drops on the naked ground, and the other is the wind erosion caused by strong winds blowing continuously for 14-15 hour every day. The latter is splashes down . the greenery of this deserted land contains mostly the Caragana species, Berberis angulasa, Sophora moorcraftiane. Egeardiana and Artemisia species .this desertded land possesses alpine type of climate the alpine here is further grouped into Humid alpine and Arid alpine . Humid alpine consists of more or less a luzruntly developed vegetation. In this the ground is covered with different types of grasses , herbs , shrubs and scrubs such as Juniperus squamata , Rhododendron setosum which are found near Jomsom and neighboring areas but it is replaced by the Caragana in the further north. But the arid alpine consists of a very poor flora. In this area no Rhododendron and Juniperus are found . it there is any vegetation , that is Caragana, which is also in a position to be vanished . So in this deserted land , due to the creation of more open land by the clearance of the existing vegetation by the local people, the environment has become too hot and too cold. and transition from the humid zone that is Rhododendron and Juniperus type , to the arid alpine zone that is Caragana type is more or less continuous .Beyond the arid alpine zone , that is beyond the limit of vascular plants , there is another alpine zone called Alpine Barren which is just below the permanent snow line . It contains mostly rocks, boulders and sands stretching towards the snow line.
The Desert and Semi-Desert Region .
Though there are found many different types of deposits like gold copper, mica, iron,lead, cobalt, ickle, zinc in different areas of the country, yet there are only few minerals like iron in Phulchouki to the south of Kathmandu valley , zinc and lead oxide at the foot of the Ganesh Himal in Rasuwa district, magnasite in the Sindhu Palchok disdtrict , sulphate in the Jhapa district, and mica in Haibung, which lies in Sindhu Palchok district. As to the gasoline resources, there had been a preliminary survey through FAO and a report was prepared too. The report shows the possibility of petroleum being available in many places, but due to some reasons the feasibility survey could not be carried out. Nepal is also home of wide variety of wild animals and birds . In the Himalayas there are very few wild animals and birds but in the Sub-Himalayan region there are found many varieties of wild animals like barking deer, musk deer, sambar (Cervus unifolor), wild sheep and goats (local name jharal and Ghoral repectively), leopards , panthers , different varieties of bears. Jackals, wild dogs, red pandas , foxes, and reptiles like snakes, wild lizards, otters, pangolins, etc. and birds like pheasants, doves, vultures and other common birds . among pheasants hanfay , monal, and kalige are famous. Danfay is the national bird. In the Mahabharat region all the wild animals and birds found in the Sub-Himalayan region are abailable , except panda, ghoral , jharal , musk deer, danfay and munal.
The Himalayan Region .
It includes mostly the rocky, barren and permanently snow-covered land, This is a tree-less part of the country where there are some bushy and scrabby type of vegetation in the depressions. As the higher mountains , that is , the Himalayas , really start from the altitude of 4015m. above the sea level , the tree-limit of this country , apparently there is ho human settlement . In this part there are some wild animals and so-called Yeti, the wild man, whose existence is yet controversial . The Himalayan region is full of snow-clad Dhaulagiri lying to the north of the sub-Himalayan region.
The Sub-Himalayan Region.
It covers T. Hagen’s Midland and inner Himalayan . It lies between the Mhabharat in the south and the Himalayas in the north. This broad belt also spreads continuously all through the length of the country. The climate and the soil of this belt is quite suitable to the human settlement. The people have been living in this belt since antiquity . that’s why, there is a thick population in this belt. Thick population causes extensive agricultural practices, which in turn, devastate forests.
this is a traditional zone of Nepalese settlement. So , this region has more agricultural and les forest land, especially in the east.May be due to the influence of Darjeeling, Kurseong and Kalimpong of India, the capital of Nepal in nearer to the east and the industrial centre of the country is also located in the east , the population is also excessively thick in the east, considering the acreage of country. There should be about two third of the total population in the west, but nearly half of the total population if found in the east including Kathmandu valley, ,though it covers only about one third of the total area. The soil of this region covers more than half of the soil found in the international soil classification chart .the main deposited soils are soil, loam, sandy loam, clay , sandy clay, sandy clay loam, loamy sand ,glay , glayees sand and sand. Among the soils found in this region there is peculiar type of silt found in the valleys, especially in the Kthamandu valley. It is a kind of black soil, a sort of completely decomposed humus , a pure loam, which is quite fertile and quite lustrous too. The people of the Kathmandu valley use it for plastering their house walls as well. And there is another kind of black soil which seems like coal and the local name is “Matti Koila” meaning clay-coat. It is not coal . the people of Kathmandu valley use this soil in kitchens and also in brick factories to bake the bricks. This soil geves very gook calorie of heat with the combination of the paddy husks and the mustard cake made from seeds after the oil has been pressed out. this Matti Koila is nothing a half decomposed pith or humus. It gives a good service when there is no supply of coal from outside . compared to the rocks of China , Russia , Alps . Etc, the rocks of this region are quite young as is evident from the fresh boulders and pebbles found in the fringes of the rivers . the main rocks found here are quartz, quartzite , granite, gneiss, micaschist, slates, phyllite, limestone , talc stones , soapstone , rock-salt and sandstone. In this belt there are less forest lands and more agricultural lands , except in far-west, especially in Jumla and Humla districts , where some virgin forests are still found.
Mahabharat Region.
It is situated in between the Sub-Himalayan region, T. Hagen’s Miklands, and Siwaliks, spreading in the form of continuous belt right from the east to western border of the country.Its maximum height is about 2901 meters above the sea level , which possesses by Thulo Pakho (Nagidanda) situated just south of the Kathmandu valley below Phulchouki danda. The writer observed that this is the only Danda which contains the Tingray Sallow(Tsuga dumosa) among the Mahabharat hills, because this range contains a bit mature soils and rocks as compared to the Siwaliks. Bhabar and Terai areas. The soil of this range is mainly loam, sandy loam, sandy clay loam, clay, sandy clay, loamy sand and sand. As to rocks, it covers almost all varieties like quartzite, granite, micaschist, limestone including marble , soap-stone , slate, phyllite, talc stones and sandstone. The soil possesses less porosity within it and, therefore , conserves more percentage of water than Siwalik. So, the fertility is also good. That is why, the pressure of cultivation is high here.
The Siwalik Region
It is called “Churay Range ” in the east and central Nepal , and in the west,”Someshore Range ”. It is also a sort of debris of Mahabharat range carried by the rivers in the past and deposited in the form of small hills lying in between the Mahabharat and Bhabar zones. The average height of these hills is about 1000 meters in the east and central part, and in the west it exceeds even 1500 meters above the sea level. It comprises almost dry hills , consisting of mainly big boulders, gravels and conglomerates with sandy clay loam, loamy sand and sandy soil. These hills are found a bit scattered in some places, forming valleys with Mahabharat range, such as Rapti Dun, Dang, Deokhuri and Durkhet valleys, which are situated in between the Mahabharat range and the Siwalik range. But in some places it seems to have vanished with no apparent shape seen outwardly. It remains in the form of fringes of the Mhabharat itself . In some places, specially to the east of Kali Gandaki river and to the south of the Deukhuri valley, the arms of the Siwaliks extended up to the border of Nepal and India . Because of the great6 porosity in the soil, there is always scarcity of water, and due to that the soil is less fertile, which discourages the cultivation and encourages the forest production, but the trees in the forest of this range are not of high quality.
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