Any time accumulation (typically snowfall) rates are greater than melting rates, a permanent snowpack forms which then freezes further to become ice. Ice behaves in a plastic fashion which allows it to flow.
The debris left behind by a melting glacier is called "moraine." Moraines consist of a mixture of soil, rocks, and sediment that the glacier has eroded and transported. They are typically found at the edges or terminus of the glacier, forming ridges or piles that mark the glacier's former extent.
Materials bulldozed at the front of a glacier form a feature known as a moraine. Moraines are accumulations of debris, such as rocks and soil, that have been transported and deposited by the glacier as it moves. They can vary in size and shape, often creating ridges or mounds that mark the glacier's former extent. These features are important indicators of past glacial activity and landscape evolution.
* Fryingpan Glacier * Nisqually Glacier * Paradise Glacier * Pyramid Glacier * Puyallup Glacier * South Tahoma Glacier * Tahoma Glacier * Success Glacier * Sarvent Glacier
Not sure what the title of it was, but it was a stock music file that sounded similar to the techno "Mortal Kombat" theme.
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.
The Many Glacier Valley is an area within Glacier National Park. It is also known as the Swiftcurrent Valley. It was named by George Bird Grinnell, the former editor of Forest & Stream Magazine (now called Field & Stream) in order to make it sound exotic and Native American in origin. The Many Glacier area encompasses several valleys that meet together in the main Swiftcurrent Valley. There are several glaciers within the Many Glacier Area including the popular Grinnell Glacier, Swiftcurrent Glacier, and the small Gem Glacier. A popular destination in Many Glacier is the Many Glacier Hotel, a historic lodge in the park built by the Great Northern Railroad around 1916. There is also the Swiftcurrent Motor Inn and a campground. Some popular hiking destinations in the valley are Cracker Lake, Iceberg Lake, Ptarmigan Tunnel, Swiftcurrent Pass, Redrock Falls, Grinnell Lake, and Grinnell Glacier. Many Glacier is an excellent place to view grizzly bears, black bears, and moose, among the other diverse wildlife in the park.