A growing glacier is one where the rate of deposition of snow at the source exceeds the rate of loss of ice at the tow. In other words, a glacier which is getting bigger/longer.
A melting glacier gets smaller, but a growing glacier gets bigger.
It's growing As of 2013, the glacier is shrinking quickly due to global warming.
When a glacier is growing, it is experiencing positive mass balance, meaning that it is accumulating more snow and ice than it is losing through melting or iceberg calving. This process leads to the glacier advancing in size and sometimes even causing the glacier's terminus to extend further down its valley.
A Glacier will advance when the snow deposited in the collection zone exceeds the rate of melting at the terminus. There will be some time delay between these events, even a steep glacier will take a few years between the events.
* Fryingpan Glacier * Nisqually Glacier * Paradise Glacier * Pyramid Glacier * Puyallup Glacier * South Tahoma Glacier * Tahoma Glacier * Success Glacier * Sarvent Glacier
It is a valley glacier
No, a glacier canyon is not a real glacier. A glacier canyon is a canyon formed by the movement of a glacier over time, carving out the landscape as it flows.
Penck Glacier (Tanzania); Pine Island Glacier, Polar Times Glacier, Priestley Glacier (Antarctica); Panchchuli Glacier, Pindari Glacier (India); Panmar Glacier, Passu Glacier (Pakistan); Pasterze Glacier (Austria); Platigliole Glacier, Praz-SecGlacier, Presena Glacier (Italy); Peyto Glacier, Pemberton Icefield (Canada); Pico de Orizaba, Popocatépetl, Glacier (Mexico); Portage Glacier, Princeton Glacier (Alaska); etc
It is apline glacier
There are quite a few glaciers to hike to in Glacier, but probably the most-visited glacier is Grinnell Glacier, located in the Many Glacier Valley.
* Franz Josef Glacier * Fox Glacier * Tasman Glacier * Hukawai Glacier * Haast Glaciers
The tip of a glacier is called the glacier terminus or glacier snout. It is the furthest point reached by the glacier as it flows downhill.