DEGRADING ENVIRONMENT AND GROWING POPULATION OF THE INDIAN HIMALAYAS
|
|
|
|
|
|
Department of Geography, Government Post Graduate College, Rudrapur,
Udham Singh Nagar 263 153, Uttaranchal
INTRODUCTION
The Himalaya, lying in Indian sub-continent, constitutes one of the greatest and youngest folded mountain systems in the world rising from about 300 m to more than 8000 m above sea level. It is a mountain region of majestic grand-eur and high geographical significance. It acts as protector, regulator and creator of natural resources, climate and soil. The rapidly increasing population, settlement and development are exhibiting environmental transformation in the form of deteriorating environment, depletion of natural resources and conditions of poverty. There has been large scale deforestation, overgrazing and expansion of agriculture on forest and marginal lands, resulting in micro – climatic changes, loss of wild life, change in water level and river regions, soil erosion, flood and landslides, all of which brought about hardships increasing environmental degradation in the ecologically fragile and geologically sensitive Himalayan region. Increasing population is not sole responsible factor; while less enlightened government and non-government agencies and unawareness of the people are equally liable for this degradation process.
The Himalaya, which plays a vital role not only in Indian but also in sub-continental economy, is in the grip of environmental degradation. Aspects of population, which are highly correlated with it, are discussed here. Figures pertaining to demographic scenario are based on Census 1991 and 2001, and overview regarding the environmental stress is based on published works.
About the Himalaya
The Himalaya makes the northern boundary of India extending from eastern border of Pakistan to the western frontiers of Myanmar having a length of about 2500 km and width of about 160 to 400 km. Extending between 70047’ and 97022’ east longitudes and 21057’ and 37015’ north latitudes, the Himalaya encompasses an area of about 5,17,733 km2, i.e., 15.75% of the area of the country. Administratively, the Indian Himalaya is divided into three broad regions - the Western Himalaya, consisting the states of Jammu and Kashmir and Himachal Pradesh, includes illegally occupied areas by Pakistan and China. The Central Himalaya consists of Uttaranchal, and the Eastern Himalaya comprises the states of Sikkim, Arunachal Pradesh, Mainpur, Tripura, Mizoram, Nagaland and hill districts of Assam and West Bengal. It is worth to mention here that the Himalayan region of West Bengal Hills consists of Darjeeling district only and the Assam Hills consists of the districts of North Cachar and Karbi Anglong. About 15% area of the Uttaranchal state (partially plains of Dehradun, Pauri, Nainital and fully plains of Haridwar and Udham Singh Nagar) is below 600 meters, i.e., continuation of Indo-gengetic plain, tarai and Bhabar.
From the northern boundary of the alluvial plain to the extreme north upto the Indian boundary, the Himalaya is divided into several geo-tectonic divisions - the Outer Himalaya (Siwaliks, Duns, Dwars, Tarai and Bhabar), the Lesser Himalaya having a number of fertile river valleys, the Great Himalayas, a zone of high snow peaks, glaciers and source of several rivers, and the Trans Himalaya a region across the Himalaya (rain shadow zone). These latitudinal divisions are separated from one another by thrusts and faults such as Himalayan Frontal Fault (H.F.F) extending between the Siwaliks and the Bhabar, Main Boundary Thrust (M.B.T) lying between the Siwaliks and the Lesser Himalaya, Main Central Thrust (M.C.T.) separating the Lesser and the Great Himalaya and Trans Himadri Thrust (T.H.T) lying between the Great and the Trans Himalaya. The total population of the Indian Himalaya is 4,03,11,039 persons in 2001 accounting for about 3.92% population of the country.
Degrading environmental profile
With the alarming devastation caused by massive landslides, accelerating soil erosion, reduced soil productivity, drying up springs, frequent earthquakes and uncontrolled floods, the Himalaya is facing a number of environmental hazards, which are manifestations of ruthless deforestation, rapid growth of population, negligence of administration and unawareness of the society on environmental issues.
The Himalayan rivers are eroding catchment areas at the mean rate of 0.1 cm per year, i.e., 100 cm in 1000 years, which is five times faster than it was in recent geological past (Menard,1963). The Ganga alone at Kolkata carries annually 411 m.t. of sediments (324 m.t. in suspended state and 83 m.t. as dissolved chemical load), implying erosion in the catchments at a rate of 549 t/km2/yr (Abbas and Subramanian, 1984). The construction of 44000 km road in the Himalaya generates about 2640m3 of debris (Valdiya, 1985). About 39% of the road bed is affected by rockfall and 38% by slamping, i.e., about 24 debris chutes/km2 (Haigh et al., 1989). At the average rate of 550 m3/km/year the total landslide debris on Himalayan roads would be of the order of 24 m.m3 annually (Valdiya, 1987). Haigh (1984) discovered 72 landslides larger than 10 m3 and total landslides sediment yield of 1105 m3/km along 66km reach of Mussoorie-Tehri road in 1978. It is well known that the whole Himalaya is dissected by various faults and thrusts. These areas are vulnerable for landslides, slumping, mass wasting, etc. Similar micro studies have been conducted by several other geologists and geographers in the Himalaya.
The Himalaya also suffers from overgrazing problem. For instance, this incidence in Uttaranchal Himalaya is 2.4 to 4.5 times higher than the carrying capacity of forest (Singh and Saxena, 1980). The annual depletion of forest is amounting to 3.76 million m3 per year, i.e., at the rate of 5.8% per year (Shah, 1985). An interpretation of land imagery indicates that only 28.7% of Indian Central Himalaya is now forested and only 4.4% of the area has a forest with greater than 60% crown density (Singh et al., 1984). Maximum land degradation occurs in the civil forest areas because of uncontrolled and unscientific anthropogenic activities. The degradation of forest has accelerated soil erosion and tragic landslides in an unprecedented manner (Bahuguna, 1981) and floods in the adjoining plains (Reiger, 1981; Ashish, 1983). It is estimated that out of the total net sown area of 7.32 x 105 ha, about 6.40 x105 ha of agricultural land suffers from severe erosion problem (Shah, 1982). The land used for agriculture is gradually being lost (Reiger, 1981). It is predicted that at the rate of 3.9 quintals per capita consumption, the carrying capacity of forest will overreach by 2031 AD (Shah, 1982). There is a perceptible decrease in spring discharge and seepage in more than 40% of the villages in Gaula catchment of Kumaun Himalaya. The extent of this decrease is between 25% and 73% in the past 5 to 50 years (Valdiya and Bartarya, 1991). The water discharge of the river Dabka in Kumaun Himalaya has decreased by 39.45% during the period of 1976-80. If this decrease continues for next 15 years, many such streams would be dry except in the monsoon seasons (Pant and Jalal, 1992). Evergrowing of population is leading to more farming and the cultivated area and the cattle population is increasing at the rate of 1.5% and 0.18% per year, respectively (Shah, 1982).
The carrying capacity of the Himalaya is decreasing day by day due to the heavy pressure of both human and livestock population. A large number of youths from the central Himalaya are migrating to other more developed parts of the country (Pant, 1992 and 1994).
A majority of the rural people does not get sufficient nutrition in their diet; consequently they suffer from nutrition deficiency related diseases (Pant 1994, 1996 and 1998). The largest number of epicenters is located in the Himalayan belt where the strongest seismicity is attributed to the movements along the MBT and MCT (Valdiya, 1992). The Himalaya falls under the 4th and 5th maximum intensity earthquake prone zone. The change in micro climate is also noticed in the Himalaya. The glaciers are receding very rapidly. A number of vegetational and wild animal species are in the endangered stage. Environmental hazards are not merely natural disasters but the result of increasing human activities and less visionary or plannings of the development agencies.
Demographic profile