 | Henry Woodward - Electronic journals - 1869 - 646 pages
...the Gulf-stream. The total quantity of water conveyed by this stream is probably equal to that ot H stream 50 miles broad and 1000 feet deep, flowing at the rate of four miles an hour. And the mean temperature of the entire mass of moving waters is not under 65° at the moment of leaving... | |
 | Geological Society of Glasgow - 1867 - 348 pages
...viz., the Gulf-stream. The total quantity of water conveyed by this stream is probably equal to that of a stream 50 miles broad and 1000 feet deep, flowing at the rate of 4 miles an hour. And the mean temperature of the entire mass of moving water is not under 65° at the... | |
 | Henry Woodward - Electronic journals - 1869 - 664 pages
...the Gulf-stream. The total quantity of water conveyed by this stream is probably equal to tlial of A stream 50 miles broad and 1000 feet deep, flowing at the rate of four miles an hour. And the mean temperature of the entire mass of moving waters is not under 65° at the moment of leaving... | |
 | James Samuelson, Henry Lawson, William Sweetland Dallas - Science - 1869 - 506 pages
...water, he says, conveyed by this stream is probably equal to that of a stream 50 miles broad and 1,000 feet deep, flowing at the rate of four miles an hour. And the mean temperature of the entire mass of moving waters is not under 65° at the moment of leaving... | |
 | John Holmes Agnew, Walter Hilliard Bidwell - 1869 - 998 pages
...quantity of water, ha says, conveyed by this stream is probably equal to a stream 50 miles broad and 1,000 feet deep, flowing at the rate of four miles an hour. And the mean temperature of the entire mass of moving waters is not under 65° at the moment of leaving... | |
 | Geology - 1870 - 500 pages
...the conclusion that the total quantity of water conveyed by the stream is probably equal to that of a stream 50 miles broad and 1000 feet deep,* flowing...the entire mass of moving water is not under 65° at the moment of leaving the Gulf. I think we are warranted to conclude that the stream, before it... | |
 | Physics - 1870 - 1136 pages
...water conveyed by the stream is probably equal to that of a stream 50 miles broad and 1000 feet deepf, flowing at the rate of four miles an hour, and that...the entire mass of moving water is not under 65° at the moment of leaving the Gulf. I think we are warranted to conclude that the stream, before it... | |
 | E.R. KNORR - 1871 - 408 pages
...quantity of water conveyed by the stream is probably equal to that of a stream 50 miles broad and 1,000 feet deep, flowing at the rate of four miles an hour,...the entire mass of moving water is not under 65° at the moment of leaving the Gulf. I think we are warranted to conclude that the stream, before it... | |
 | David Thomas Ansted - Physical geography - 1871 - 582 pages
...the published sections made by the United States coast survey, the Gulf stream is equal to a river 50 miles broad and 1000 feet deep, flowing at the rate of four miles an hour, with a mean temperature not under 65° on leaving the Gulf. This estimate is much lower than... | |
 | Royal Geographical Society (Great Britain) - Electronic journals - 1871 - 456 pages
...the conclusion that the total quantity of water conveyed by the Stream is probably equal to that of a stream 50 miles broad and 1000 feet deep, flowing at the rate of 4 miles an hour ; and that the mean temperature of the entire mass of moving water is not under 65°... | |
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... the mean temperature of the entire mass of moving water is not under 65° at the moment of leaving the Gulf. 
