The Gateway to the Polynia: A Voyage to Spitzbergen |
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Spitzbergen - The Gateway to the Polynia - Moffen Island - Walrus - Sea Devils —
Moffen Island – New Dangers - Formation of Ice Floes 194 CHAPTER VII .
Difficulties in Narrow Waters — The Wounded Sea Bird - Nature most Desolate -
Deer ...
Spitzbergen - The Gateway to the Polynia - Moffen Island - Walrus - Sea Devils —
Moffen Island – New Dangers - Formation of Ice Floes 194 CHAPTER VII .
Difficulties in Narrow Waters — The Wounded Sea Bird - Nature most Desolate -
Deer ...
Página
Professor Nordenskiold – Boats for the Journey - Method of Travelling - Parry's
Journal - Latitude 81 ° 31'41 " N. - Meteorological Observations - Stout - built
Boats — Thickness of the Ice - Formation of Ice - Long Time getting to 83 ° —If
they ...
Professor Nordenskiold – Boats for the Journey - Method of Travelling - Parry's
Journal - Latitude 81 ° 31'41 " N. - Meteorological Observations - Stout - built
Boats — Thickness of the Ice - Formation of Ice - Long Time getting to 83 ° —If
they ...
Página 37
The climate must have been not only more equable but warmer , as is shown by
the coral banks which were formed at that time in Spitzbergen , as well as by the
enormous tree - like cryptogams , and the large - leaved ferns which Bear Island
...
The climate must have been not only more equable but warmer , as is shown by
the coral banks which were formed at that time in Spitzbergen , as well as by the
enormous tree - like cryptogams , and the large - leaved ferns which Bear Island
...
Página 42
... thickness of the ice whether the regions around the Pole are warmer than in
about 75 ° N. What are the regions of perennial ice ? for that there are such
regions seems clear from the occurrence of sea ice in sheets formed of annual
layers .
... thickness of the ice whether the regions around the Pole are warmer than in
about 75 ° N. What are the regions of perennial ice ? for that there are such
regions seems clear from the occurrence of sea ice in sheets formed of annual
layers .
Página 47
From the position in which these masses occurred , it seems probable that they
formed part of a large fall of meteoric iron during the miocene period . In 1872 the
Swedish government sent a ship out to convey these masses to Sweden .
From the position in which these masses occurred , it seems probable that they
formed part of a large fall of meteoric iron during the miocene period . In 1872 the
Swedish government sent a ship out to convey these masses to Sweden .
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advance animals appearance Arctic attempt bear boat called Captain carried cause CHAPTER clear close coast coming continued course crew danger deer difficulty direction distance drift east effect escape evidently explored fact fall feet floating force formed four gained give Greenland hands head hope Island journey kind land latitude leave less look masses means miles mountain nature northern noticed object observed once ourselves party passage passed Polar Pole present probably proved pursuit reached region remains rest rise rocks round sailed sailors schooner seal season seems seen ship shore short shot side sight snow soon Sound Spitzbergen sport Strait success surface temperature travelling turned vessel voyage warm weather whale whole wind winter
Información bibliográfica
| Título | The Gateway to the Polynia: A Voyage to Spitzbergen |
| Autor | John Campion Wells |
| Editor | H.S. King, 1873 |
| Procedencia del original | Universidad de California |
| Digitalizado | 1 Abr. 2009 |
| Largo | 355 páginas |
| Exportar cita | BiBTeX EndNote RefMan |