INTRODUCTION

Sikkim is a very small hilly State in the Eastern Himalayas with a geographical area of 7096 sq. km. extending approximately 114 km from North to South and 64 km. from East to West. It is surrounded by the Tibetan plateau in the North, the Chumbi valley of Tibet and the Kingdom of Bhutan in the east. It is bounded by the Darjeeling district of West Bengal in the South and the kingdom of Nepal in the west. The state is divided into the four administrative districts i.e. East, West, North and South. The State being a part of the inner ranges of the Himalayas has no open valleys or plains. But varied elevations ranging from 300 to 8353m. above mean sea level consisting of lower hills, middle and higher hills, alpine zones and snow bound land. The highest elevation being the top of the mountain Kanchendzonga itself. Sikkim Himalayas show tremendous biological diversity. More than 5000 species of Angiosperms are found in the State, which is nearly 1/3 of total species of Angiosperms found in the country. There are 4000 species of flowering plants, 300 species of Ferns and its allies, 450-500 species of Orchids, 40 species of Rhododendron, 8 species of tree ferns, 11 species of Oaks, 30-40 species of Primulas, 26 species of Bamboos, 144 species of Mammals, 500-600 species of birds, over 400 species of Butterflies and Moths and many species of reptiles etc. are found in the state.

Latitude 26º 4’ and 28º 7’48” North

Longitude 86º’ and 88º 55’25” East

TOPOGRAPHY

             The mountains terrain of Sikkim consist of a tangled series of interlacing ridges, rising one above the other, from south to the foot of the high peaks, which mark the abode of snow in the North. The total area can be divided into nine (9) unequal parts as follows:

 1.         Summits and ridges

 2.         Escarpments

 3.         Very steep slopes (>50%)

 4.         Steep slopes (>30-50%)

 5.         Moderately steep slopes (15-30%)

 6.         Narrow valleys (<30%)

 7.         Cliffs and precipitous slopes

 8.         Zones of glacial drifts/marine/boulders.

 9.         Perpetual snow

             Considering the degree of slopes, vegetation and geology, the above can be further regrouped into five broad physiographic divisions.

 summits and ridges, side slopes of hills, valleys, rock cliffs and, glacial zone

 CLIMATE 

The climate of the State has been roughly divided into the Sub-Tropical, Temperate and Alpine zones. For most of the year, the Climate is cold and humid and rainfall occurs in each month. The area experiences heavy rainfall due to its proximity to the Bay of Bengal. The rainfall in South District is comparatively less than in other Districts. The general trend of decrease in temperature with in increase in altitude holds good everywhere. Pre-monsoon rain occurs in April- May and Monsoon (South-West) operates normally from the month of May continuing up to early October.

 TEMPERATURE

             The mean temperature in the lower altitudinal zones varies between 4.5º C to 19.5º C whereas at higher altitudinal zones it varies from 1,5º C to 9.5º C. Temperature varies with altitude and slope. The maximum temperature is recorded usually during July-August and minimum during December-January. Fog is a common feature in the month of May to September. Biting cold is experienced at high altitude places in the winter months and snowfall is also not uncommon during this period.

 RAINFALL

             An examination of available rainfall data shows that the mean annual rainfall is minimum at Thangu (82mm) in North Sikkim and maximum at Gangtok (3494 mm) in east Sikkim. An isohyetal analysis of this data reveals that there are two maximum rainfall areas (i) South-East quadrant, including Mangan, Singhik, Dikchu, Gangtok and Rongli (ii) South-west quadant, including hilly. In between these two regions, there is a low rainfall region (e.g., Namchi), Rainfall in this area is about half of that in the former areas. There is an area in northwest Sikkim which gets little rainfall (even less than 4.9mm). This area is mainly snow-covered mountains, Rainfall is heavy and well distributed during the months of May to early October. July is the wettest month in most places. The intensity of rainfall during southwest monsoon season decreases from South to north, while the distribution of winter rainfall is  in the opposite order. The highest annual rainfall for individual stations may exceed 5000mm. and average number of rainy days (days with rain of 2.5 mm or more) range from 100 at Thangu to 185 at Gangtok.

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