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2. Pfister (firm) - Wikipedia

   en.wikipedia.org/wiki/Pfister_(firm)

   Pfister, called Price Pfister until 2010, is an American manufacturer of bathroom and lavatory faucets, shower systems, showerheads and accessories, kitchen faucets and other plumbing fixtures. Emil Price and William Pfister founded the company in 1910. Today, Pfister is owned by Assa Abloy.

3. USS Glacier (AGB-4) - Wikipedia

   en.wikipedia.org/wiki/USS_Glacier_(AGB-4)

   USS Glacier (AGB-4) (later USCGC Glacier (WAG/WAGB-4)) was a U.S. Navy, then U.S. Coast Guard icebreaker which served in the first through fifteenth Operation Deep Freeze expeditions. Glacier was the first icebreaker to make her way through the frozen Bellingshausen Sea , and most of the topography in the area is named for her crew members.

4. Glacier National Park (U.S.) - Wikipedia

   en.wikipedia.org/wiki/Glacier_National_Park_(U.S.)

   Glacier National Park is a national park of the United States located in northwestern Montana, on the Canada–United States border.The park encompasses more than 1 million acres (4,100 km 2) and includes parts of two mountain ranges (sub-ranges of the Rocky Mountains), more than 130 named lakes, more than 1,000 different species of plants, and hundreds of species of animals.

5. Glacier Bancorp - Wikipedia

   en.wikipedia.org/wiki/Glacier_Bancorp

   Glacier Bancorp Inc. was established in 1990 as the parent company of First Federal. First Federal was then renamed to Glacier Bank in 1992. [4] On February 25, 2013, Glacier Bancorp, Inc. acquired Wyoming-based First State Bank, which held $281 million in assets as of December 31st, 2012. [1] [5]

6. Lambert Glacier - Wikipedia

   en.wikipedia.org/wiki/Lambert_Glacier

   An icefall feeding into the Lambert Glacier, Antarctica Lambert Glacier is a major glacier in East Antarctica.At about 80 km (50 mi) wide, over 400 km (250 mi) long, and about 2,500 m (8,200 ft) deep, it is the world's largest glacier.

7. Plucking (glaciation) - Wikipedia

   en.wikipedia.org/wiki/Plucking_(glaciation)

   Plucking is increased where there are preexisting fractures in a rock bed. As the glacier slides down a mountain, energy from friction, pressure or geothermal heat causes glacial meltwater to infiltrate the spaces between rocks. [4] This process, known as frost wedging, puts stress on the rock structure as water expands when it freezes.