CĂRȚI ÎN ENGLEZĂ ÎN LEGĂTURĂ CU «FIRN LIMIT»
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1
Geological Survey Professional Paper
Because the ice field has a low gradient, any change of the firn limit will have far-
reaching effects on the glacier's mass balance. Waitabit Ridge (PC6) Nestled in
between the Mummery and Barnard Dent Groups is Waitabil Ridge (fig. 1, PC6).
2
Geological Survey Professional Paper
... uppermost tephra layer (1) is located at the firn limit. Glaciers in the left
background are in the drainage basin of Rio Tunel. The pass through which F.
Reichert gained access to the ice field in 1916, called Paso del Viento, is clearly
visible.
Geological Survey (U.S.), 1998
3
The Changing Earth: Exploring Geology and Evolution
The elevation to which snow recedes during a wastage season is the firn limit (
Figure 14.7). You can easily identify the zones of accumulation and wastage by
noting the location of the firn limit. The firn limit on a glacier may change yearly,
but ...
James Monroe, Reed Wicander, 2014
A plane-table map (1:1200) was made of a strip 1700 feet wide and 2700 feet
long extending transversely across the glacier just below the firn limit. f. Oxygen-
Isotope Ratios. Samples of snow, firn and ice were collected at sites ranging from
...
World Data Center A., 1965
5
Physical Geology: Exploring the Earth
The elevation to which snow recedes during a wastage season is the firn limit (b
Figure 17.7). Geologists can easily identify the zones of accumulation and
wastage by noting the loca— tion of the firm limit. The firn limit on a glacier may
change ...
James Monroe, Reed Wicander, Richard Hazlett, 2006
6
Geophysics and the IGY: Proceedings of the Symposium at the ...
It is obvious then that the maximum quantity of ice to flow through any vertical
cross section is at the firn limit. Of course, the firn limit fluctuates somewhat from
year to year, but, in general, it is a very useful division of the glacier. Now to get ...
United States. National Committee for the International Geophysical Year, Hugh Odishaw, Stanley Ruttenberg, 1958
7
Living Ice: Understanding Glaciers and Glaciation
Were we to visit our glacier during summer, we would be impressed by the large
amount of meltwater associated with the ice tongue below the firn limit. This is the
melting season during which not only the last winter's snow but also some of ...
Robert Phillip Sharp, 1988
8
Glacial and Fluvial Geomorphology of Western Himalaya: ...
These variations greatly affect the movements of glaciers and oscillations of firn
limit. The low temperature and high precipitation induces change in temperature
gradient above the firn limit.'7 Due to these changes more energy would be spent
...
Syn: firn basin; neve. firn ice iced firn. firnification (firn'-i-fi-ca'-tion) The process
whereby snow is transformed into firn and then into ice in a glacier. firn limit firn
line. firn line Commonly used as a synonym for equilibrium line. This is not ...
Julia A. Jackson, James P. Mehl, Klaus K. E. Neuendorf, 2005
10
Dictionary of Geological Terms
Syn: firn basin; névé firn limit firn line. firn line The highest level on a glacier to
which the winter snow cover recedes during the summer season; the snowline.
Syn: firn limit. first arrival The first energy to arrive from a seismic source.
Robert Latimer Bates, Julia A. Jackson, 1984
