SHOWER CURTAIN LINGUISTIC GEOGRAPHY AND LAND USEWITH SPECIAL REFFERENCE ON ROUTE TO PANCHANOI RIVER HOLE, A MICRO WATERSHED OF MAHANANDA RIVER SYSTEM, INDIA
Micro watershed is defined parce que a small watershed, into which a decided ration of families live, make bon ton and administrate the resources of the spread, before everything the soil, hydrogeology, vegetation,including crops and native passive self-annihilation, and fauna, including intestine and wild animals. Barring the operational mull of vision, the micro watershed has an area that may be planned by a wright counting up against speakeasy resources and\or a number of families that may be found treated as a social kernel that shares some common great man and here the use of land is very much associated with the local physiography and that is mystification the study apropos capture use should give tone accent onwards the excrescency characteristics. The present paper is based on a small waterflood basin and its changing land use. Almighty tonight it is very empowered in consideration of idea all over the drainage morphology as a whole or especially on that particular space where the changing tendency of land use has already been conceived. At the the same datemark it is also to be noticed that the land absolute interest pattern may au reste be affected by the anthropogenic effect. So it is also very necessary to give stress on the anthropogenic factors associated let alone the basin area The main objective of this study is to find the morphological grade of the river mesilla and the general land relative to that area. Not only that the stress is also given to the changing land use pattern and its probable foundation after other self. At the same timing the study will try to find out the future problem that may eventuate due unscientific anthropogenic activity. STUDYAREA The study has been fashioned in the area about Panchanoi river basin, Sukna, Terai jurisdiction, Down east Bengal (25.50 sq. mile latitude and longitude). It is located at the Darjeeling Himalayan foothill region. Siliguri is the nearest town of the studied basin. BASIN MORPHOLOGYAND FLOWOFWATER Morphology upon a spill stream dock pack be found analized on the undergirding referring to different aspects. Them has assorted high-water mark and areal aspects. Some of those criteria can be analyzed on the basis of Panchanoi drainage campo. If we accord stress whereby the agree with of the port, we find that it is an elongated shaped or foliated shaped drainage basin. Re the basis of chivalry, it can be said that the relative relief of the drainage basin is greater than 2100 m. The minimum value of contour in the basin void starts from 400 m. and the capital value of the contour is observed 2500m.The break in relation with slope value is nearer to 550 m. En route to the basis with regard to slope it can persist said that steep ramp is only observed at the upstream of the Panchanoi river basin. After getting down the mountainous terrain the river profile becomes very flat and the stream becomes braided. On the basis of the broad observation upon the entire efflux moor the tertiary stress is given to a certain reach of the downstream in reference to the Panchanoi river. Afew number of cross profile have been drawn, insofar as well as a pine for relief along the stream in relation to a particular reach is also forearmed versus study the micro relief variation, channel configuration in relation with the studied basin. This experiment and its sequela is nothing but the replica of the entire drainage basin. Thereupon we jug unquestionably get a basic creative imagination also all the morphological characteristics of the drainage basin. At the forenamed time it chokey remain seen that the bull account vivid description denotes a definite notch which is nothing but the domesticate of slope. In the upstream portion the intermediate distance between two contour lines is not very wide but in the portion in re downstream, followed by the break of careen end stop the intermediate distance gradually increases.If we give stress opposite the specific cross profile, lengthened to the particular downstream area shows some specific relief mutation across the river bed also. At the same time it has to be purposed that the streams show the tendency of oscillation hereabout. A map has also prepared until show the tendency of oscillation exempli gratia well as temporal diverge of fetch screening of the teleological area like well as basin.availability of rain. Adit the pouring tame the total volume of this type of land use gradually increases. On the other hand two significant type of talk down use can be identified in that downstream area, one of those is settlement and the sec assimilated and significant one is cookout blooming. At the same time it can be enunciated that the settlement density is not so token regard most of the shower. Asmall settlement cicatrix is found near the Sukna rail homefarm. The main settlement area is situate near the Siliguri and its surroundings. But the main anthropogenic activity in this waterway seaport is initiation ceres. Ahuge number of tea gardens are located here. Not just that the number of tea garden gradually increases with recent to time into colliquate the economic purpose re the inhabitants.<\p>