can you describe the place where the sheet of ice melted at?
A moraine is any glacially formed accumulation of unconsolidated glacial debris that occurs in both currently and formerly glaciated regions on Earth
Moraine
A moraine is any glacially formed accumulation of unconsolidated glacial debris (regolith and rock) that occurs in both currently and formerly glaciated regions on Earth
when did immigrants stop coming to ellis island UNANSWERABLE where is this island located? New York Harbor can you mention any geographical features of the islands? Ellis Island is in Upper New York Bay, east of Liberty State Park and north of Liberty Island. While most of the island is in Jersey City, New Jersey, a small section is an exclave of New York City. are there any military facilities? Ellis Island was also used by the military for almost 80 years. By the mid-1790s, as a result of the United States' increased military tensions with Britain and France, a U.S. congressional committee drew a map of possible locations for the First System of fortifications to protect major American urban centers such as New York Harbor. what was the state of this place before colonialization? The present-day Ellis Island was created by retreating glaciers at the end of the Wisconsin glaciation about 15,000 years ago. The island was described as a "hummock along a plain fronting the west side of the Hudson River estuary. what is this glaciation process that you just mentioned? It refers to the most recent glacial period of the North American ice sheet complex. This advance included the Cordilleran Ice Sheet, which nucleated in the northern North American Cordillera when did it happen? From approximately 75,000 to 11,000 years ago has it resulted in formation of sheets of ice? No, but  the ice sheet melted from the north at a moraine, water would begin to pond in the divide between a moraine and the ice front.
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Moraine [SEP] Introduction
A moraine is any glacially formed accumulation of unconsolidated glacial debris (regolith and rock) that occurs in both currently and formerly glaciated regions on Earth (i.e. a past glacial maximum), through geomorphological processes. Moraines are formed from debris previously carried along by a glacier, and normally consist of somewhat rounded particles ranging in size from large boulders to minute glacial flour. Lateral moraines are formed at the side of the ice flow and terminal moraines at the foot, marking the maximum advance of the glacier. Other types of moraine include ground moraines (till-covered areas with irregular topography) and medial moraines (moraines formed where two glaciers meet).