The National Geographic Magazine, Volume 3National Geographic Society, 1892 - Geography Indexes kept up to date with supplements. |
From inside the book
Results 6-10 of 41
Page 34
... determined upon extending their influence on the north- ern and western coasts , and the Portuguese , English , Germans , and Italians are pronounced in their efforts on the eastern coast , while the English are careful , too , of their ...
... determined upon extending their influence on the north- ern and western coasts , and the Portuguese , English , Germans , and Italians are pronounced in their efforts on the eastern coast , while the English are careful , too , of their ...
Page 40
... determination of the geo- graphical position and elevation of Mount St. Elias and many neighboring peaks . Mount St. Elias is indicated to be not so high by some 4,000 feet as the heretofore accepted elevation , 19,500 feet . The ...
... determination of the geo- graphical position and elevation of Mount St. Elias and many neighboring peaks . Mount St. Elias is indicated to be not so high by some 4,000 feet as the heretofore accepted elevation , 19,500 feet . The ...
Page 42
... determine the exact meaning of the various technical terms employed by the various writers . Whether from looseness of verbiage originally or from the not infrequent habit of disputants when worsted to change their ground by claiming to ...
... determine the exact meaning of the various technical terms employed by the various writers . Whether from looseness of verbiage originally or from the not infrequent habit of disputants when worsted to change their ground by claiming to ...
Page 43
... determine the initial formation and subsequent maintenance and progress of the cyclone . Some real progress in charting lines of equal density seems to have been made by M. Nils Ekholm following Professor Abbe's system of “ isostaths ...
... determine the initial formation and subsequent maintenance and progress of the cyclone . Some real progress in charting lines of equal density seems to have been made by M. Nils Ekholm following Professor Abbe's system of “ isostaths ...
Page 44
... determination is this , that it is a measure of mass only . The density of two masses of air is determined to be the same ; but as the density may result from two entirely different causes , their physical relations cannot be fully ...
... determination is this , that it is a measure of mass only . The density of two masses of air is determined to be the same ; but as the density may result from two entirely different causes , their physical relations cannot be fully ...
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Common terms and phrases
Agassiz glacier Alaska Amazon appears avalanches base beneath Bering Bering island Bering's Blossom island border camp canoe carts chart Coast and Geodetic crest crevasses débris dense Disenchantment bay eastern elevation Elias range Elias region expedition exploration feet flows formed Geodetic Survey GEOG Geological Survey glacial Haenke island height Hitchcock range ice-streams Icy bay indicated Kamshatka Kerr l'Isle l'Isle's lake land longitude lower Lucia glacier Malaspina glacier margin Marvine glacier melting miles moraines Mount Augusta Mount Cook Mount Owen Mount St NATIONAL GEOGRAPHIC National Geographic Society névé night observations peaks Pinnacle system plateau Port Mulgrave portion reached ridge river rocks route rugged Russian sandstone Seward glacier shale shore side slope snow snow-fields southern southward steep stones storm stream Street summit surface tent terrace tion topographic tunnel valley vegetation voyage western westward Yakutat bay Yakutat system