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20230307120748.0 |
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210916s1958 xxu||||| |||||||||||eng d |
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|a POSLANO DO SKCR
|b 2022-01-03
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| 040 |
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|a BOD004
|b cze
|e rda
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| 072 |
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7 |
|a 551
|x Geologie. Meteorologie. Klimatologie
|2 Konspekt
|9 7
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| 080 |
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|a (048.8)
|2 MRF
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| 080 |
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|a (739.8)
|2 MRF
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| 080 |
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|a "628.6"
|2 MRF
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| 080 |
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|a 624.131.1
|2 MRF
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| 080 |
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|a 551.1/.4
|2 MRF
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| 100 |
1 |
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|a Wahrhaftig, Clyde,
|d 1919-1994
|7 mub20201070248
|4 aut
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| 245 |
1 |
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|a Quaternary and engineering geology in the central part of the Alaska Range ;
|b Quaternary Geology of the Nenana River Valley and Adjacent parts of the Alaska Range ; Engineering Geology along part of the Alaska Rairoad /
|c by Clide Wahrhaftig and Robert F. Black
|
| 264 |
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1 |
|a Washington :
|b United States Government Printing Office,
|c 1958
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| 300 |
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|a viii, 118 stran +
|e 10 složených listů
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| 336 |
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|a text
|b txt
|2 rdacontent
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| 337 |
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|a bez média
|b n
|2 rdamedia
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| 338 |
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|a svazek
|b nc
|2 rdacarrier
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| 490 |
1 |
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|a Geological survey professional paper ;
|v 293
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| 504 |
|
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|a Obsahuje bibliografii a rejstřík
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| 650 |
0 |
7 |
|a čtvrtohory
|7 ph134738
|2 czenas
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| 650 |
0 |
7 |
|a inženýrská geologie
|7 ph121179
|2 czenas
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| 650 |
0 |
7 |
|a regionální geologie
|7 ph125075
|2 czenas
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| 650 |
0 |
9 |
|a regional geology
|2 eczenas
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| 650 |
0 |
9 |
|a Quaternary
|2 eczenas
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| 650 |
0 |
9 |
|a engineering geology
|2 eczenas
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| 651 |
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7 |
|a Aljaška
|7 ge128654
|2 czenas
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| 651 |
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9 |
|a Alaska
|2 eczenas
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| 655 |
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7 |
|a studie
|7 fd133597
|2 czenas
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| 655 |
|
9 |
|a studies
|2 eczenas
|
| 700 |
1 |
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|a Black, Robert F.
|q (Robert Foster),
|d 1918-1983
|7 mzk20181003171
|4 aut
|
| 700 |
1 |
2 |
|a Wahrhaftig, Clyde,
|d 1919-1994.
|t Quaternary and engineering geology in the central part of the Alaska Range
|
| 700 |
1 |
2 |
|a Wahrhaftig, Clyde,
|d 1919-1994.
|t Quaternary Geology of the Nenana River Valley and Adjacent parts of the Alaska Range
|
| 700 |
1 |
2 |
|a Wahrhaftig, Clyde,
|d 1919-1994.
|t Engineering Geology along part of the Alaska Rairoad
|
| 830 |
|
0 |
|a Geological survey professional paper ;
|v 293
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