Nature, Volume 32Sir Norman Lockyer Macmillan Journals Limited, 1885 |
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Página 179
... Lake , and the present configuration be caused by subsequent erosion . It should be stated that the out- let of this lake does not now follow the course of the ice- stream towards the Balsfjord - which might have been reasonably assumed ...
... Lake , and the present configuration be caused by subsequent erosion . It should be stated that the out- let of this lake does not now follow the course of the ice- stream towards the Balsfjord - which might have been reasonably assumed ...
Página 236
... lake , and could be seen running past the jetty at the rate of about two miles per hour . But it did not stop when the old level was reached , the momentum carried it beyond that point , and raised the water up at the south end of the lake ...
... lake , and could be seen running past the jetty at the rate of about two miles per hour . But it did not stop when the old level was reached , the momentum carried it beyond that point , and raised the water up at the south end of the lake ...
Página 237
... lake lost 6 feet ; and again , from May , 1878 , to February , 1885 , say seven years , the lake again lost 6 feet by evaporation , and this of course in addition to all the rain which fell during that period . Taking the records at ...
... lake lost 6 feet ; and again , from May , 1878 , to February , 1885 , say seven years , the lake again lost 6 feet by evaporation , and this of course in addition to all the rain which fell during that period . Taking the records at ...
Índice
Auroral Zone ElevenYear Meridional Oscillation of the Bath Natural History and Antiquarian Field Club | 12 |
Prof Auwers Calculations of Longitude of Places bination of the Ordnance and Admiralty Surveys E | 101 |
Earthquakes in 11 85 460 Industrial Education in Behrens Dr W J Guide for the Microscopical Investiga | 193 |
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