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In case it touches the mountain relief, it sinks as far as below the level of the summits.

At the following types even the valley glacier surface–and not only the firn 60 caldron and firn basin–runs as far as kilometers- to deca-kilometers above the ELA thus contributing by primary snow precipitation to the glacier nourishing and further ice filling (Figures 2 and 3: Fm and Fs; e.g. At last, when the whole relief has been filled with ice, in the high mountains develops an ice stream network. On the high plateaus evolved a plateau glacier (Figure 1c).

In this case the dimensions of the Tibetan plateau induced an ice sheet with very flat surface inclinations.

Some have opened up healing centers, written books, facilitated retreats and workshops etc..

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