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  2. Champlain Sea - Wikipedia

    en.wikipedia.org/wiki/Champlain_Sea

    The mass of ice from the continental ice sheets had depressed the rock beneath it over millennia. At the end of the last glacial period, while the rock was still depressed, the Saint Lawrence and Ottawa River valleys, as well as modern Lake Champlain, at that time Lake Vermont, were below sea level and flooded with rising worldwide sea levels, once the ice no longer prevented the ocean from ...

  3. Blue Lake Crater - Wikipedia

    en.wikipedia.org/wiki/Blue_Lake_Crater

    The geological feature consists of three overlapping craters, which are filled by the waters of Blue Lake, [4] often called "the Crater Lake of the Central Oregon Cascades." [ 6 ] With an area of 60.4 acres (0.244 km 2 ), [ 6 ] Blue Lake has dimensions of 0.19 by 0.50 miles (0.3 by 0.8 km), [ 4 ] with a depth of more than 300 feet (90 m). [ 7 ]

  4. Mount Jefferson (Oregon) - Wikipedia

    en.wikipedia.org/wiki/Mount_Jefferson_(Oregon)

    A view of Mount Jefferson from Russell Lake in 1934. When Little Ice Age glaciers retreated during the 20th century, water filled in the spaces left behind, forming moraine-dammed lakes, [14] which are more common in the Mount Jefferson Wilderness and the nearby Three Sisters Wilderness than anywhere else in the contiguous United States. [15]

  5. Body of water - Wikipedia

    en.wikipedia.org/wiki/Body_of_water

    The process of creating an "impoundment" of water is itself called "impoundment". Ice cap: A body of frozen water less than 50,000 km 2 not constrained by topographical features (i.e., they will lie over the top of mountains) Ice field: A body of frozen water constrained by topographical features: Ice sheet: A body of frozen water more than ...

  6. Sea ice - Wikipedia

    en.wikipedia.org/wiki/Sea_ice

    Once nilas has formed, a quite different growth process occurs, in which water freezes on to the bottom of the existing ice sheet, a process called congelation growth. This growth process yields first-year ice. In rough water, fresh sea ice is formed by the cooling of the ocean as heat is lost into the atmosphere.

  7. Lake Pontchartrain - Wikipedia

    en.wikipedia.org/wiki/Lake_Pontchartrain

    Lake Pontchartrain from southbound causeway entrance Lake Pontchartrain's north shore at Fontainebleau State Park near Mandeville, Louisiana, in 2004. Lake Pontchartrain (/ ˈ p ɒ n tʃ ə t r eɪ n / PON-chə-trayn; [1] French: Lac Pontchartrain) is an estuary located in southeastern Louisiana in the United States.

  8. The only living core member of 'The Jeffersons' cast made a ...

    www.aol.com/entertainment/only-living-member...

    While Gibbs may be best known her "Jeffersons" character from 1975 to 1985 — yes, that's a decade-long run! — her career has continued to flourish with dozens of TV and film roles.

  9. Lake Michigan–Huron - Wikipedia

    en.wikipedia.org/wiki/Lake_Michigan–Huron

    Before that, Lake Chicago occupied the southern tip of the Lake Michigan basin, at the southern end of the ice sheet. Lake Algonquin and Lake Chicago both drained south into the Mississippi River watershed. [8] Around 9,500 years ago, new pathways draining the system to the east were opened by the retreat of the ice, and proglacial Lake Stanley ...