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2. Zamboni Company - Wikipedia

   en.wikipedia.org/wiki/Zamboni_Company

   Frank J. Zamboni developed the first ice resurfacing machine in 1949, and started the Zamboni Company in 1950. Zamboni / z æ m ˈ b oʊ n i / is an internationally registered trademark . The machines are made in Paramount, California, and in Brantford, Ontario.

3. Taylor Company - Wikipedia

   en.wikipedia.org/wiki/Taylor_Company

   A mixture of chocolate and vanilla soft serve being dispensed, a flavor colloquially referred to as swirl or twist. The company was founded in 1926 by Charles Taylor, a third-generation ice cream maker from Buffalo, New York, who invented an automated countertop ice cream freezer [3] that allowed restaurants to manufacture their own ice cream from mix. [4]

4. Weichselian glaciation - Wikipedia

   en.wikipedia.org/wiki/Weichselian_glaciation

   The Fennoscandian Ice Sheet of the Weichselian glaciation most likely grew out of a mountain glaciation of small ice fields and ice caps in the Scandinavian Mountains.The initial glaciation of the Scandinavian Mountains would have been enabled by moisture coming from the Atlantic Ocean and the mountains high altitude.

5. Quaternary glaciation - Wikipedia

   en.wikipedia.org/wiki/Quaternary_glaciation

   During the Quaternary glaciation, ice sheets appeared, expanding during glacial periods and contracting during interglacial periods. Since the end of the last glacial period, only the Antarctic and Greenland ice sheets have survived, while other sheets formed during glacial periods, such as the Laurentide Ice Sheet, have completely melted.

6. Interglacial - Wikipedia

   en.wikipedia.org/wiki/Interglacial

   Shows the pattern of temperature and ice volume changes associated with recent glacials and interglacials. An interglacial period (or alternatively interglacial, interglaciation) is a geological interval of warmer global average temperature lasting thousands of years that separates consecutive glacial periods within an ice age.

7. Post-glacial rebound - Wikipedia

   en.wikipedia.org/wiki/Post-glacial_rebound

   To form the ice sheets of the last Ice Age, water from the oceans evaporated, condensed as snow and was deposited as ice in high latitudes. Thus global sea level fell during glaciation. The ice sheets at the last glacial maximum were so massive that global sea level fell by about 120 metres. Thus continental shelves were exposed and many ...