World Geography
The snow line on the northern side of greater Himalayas range about

4,500 to 6,000 metres
None of these
3,500 to 6,000 metres
5,500 to 6,000 metres

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World Geography
The rate of infiltration normally declines rapidly during the early part of rainstorm event and reaches a constant value after several hours of rainfall. The factors responsible for this phenomenon are I. the filling of fine soil pores with water, which reduces capillary forces II. moistened soil, clay particles to swell and reduce the size of pores III. raindrop impact breaking up with soil clumps, splashing fine particles into pores

I, III
II, III
All of these
I, II

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