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Record #32983:
- #32983
Main publication details
MARC recordПеригляциал Антарктиды
| Title: | Перигляциал Антарктиды |
| Title, transliterated: | Perigli︠a︡t︠s︡ial Antarktidy / K.K. Markov. |
| Translated title: | Periglacial phenomena in Antarctica. |
| Author(s): | Markov, K. K. |
| Date: | 1959. |
| Language: | Russian. |
| In: | Informat︠s︡ionnyĭ bi︠u︡lletenʹ Sovetskoĭ antarkticheskoĭ ėkspedit︠s︡ii. (1959.), Vol. 9 (1959) |
| Abstract: | Physical and chemical weathering in Antarctica is described. Frost action, temperature variations, and wind cause desquamations, fissuring nivation cirques and terraces, structural formations, cellular weathering, eolian deposits, and stone cauldrons, while in loose deposits frost fissures, stone splitting, stone stripes and screes form, and stones are set upright. Two periglacial zones are disdtinguished: the internal zone of the cold Antarctic desert, and the cool and moist peripheral zone of the Antarctic islands (subantarctic and temperate zone). There is no vertical zonation of periglacial phenomena, those at sea level being the same as those at elevations up to 1-2 km. |
| Notes: | Informat︠s︡ionnyĭ bi︠u︡lletenʹ Sovetskoĭ antarkticheskoĭ ėkspedit︠s︡ii. Vol. 9 :9-12 incl. (1959). |
| Keywords: | 551.34 -- Geocryology. Frozen ground. 551.343 -- Periglacial processes. Thermokarst. E8 -- Glaciology: frost action and permafrost. (*7) -- Antarctic regions. |
| SPRI record no.: | 32983 |
LDR 02110naa#a2200000#a#4500 001 SPRI-32983 005 20240418094938.0 007 ta 008 240418s1959####xx####|##|###|0||#0|rus#d 035 ## ‡aSPRI-32983 040 ## ‡aUkCU-P‡beng‡eaacr 041 0# ‡arus 100 1# ‡6880-01‡aMarkov, K. K. 242 10 ‡aPeriglacial phenomena in Antarctica.‡yeng 245 10 ‡6880-02‡aPerigli︠a︡t︠s︡ial Antarktidy /‡cK.K. Markov. 260 ## ‡a[S.l.] :‡b[s.n.],‡c1959. 300 ## ‡ap. 9-12 incl. :‡btable, 2 refs. 500 ## ‡aInformat︠s︡ionnyĭ bi︠u︡lletenʹ Sovetskoĭ antarkticheskoĭ ėkspedit︠s︡ii. Vol. 9 :9-12 incl. (1959). 520 3# ‡aPhysical and chemical weathering in Antarctica is described. Frost action, temperature variations, and wind cause desquamations, fissuring nivation cirques and terraces, structural formations, cellular weathering, eolian deposits, and stone cauldrons, while in loose deposits frost fissures, stone splitting, stone stripes and screes form, and stones are set upright. Two periglacial zones are disdtinguished: the internal zone of the cold Antarctic desert, and the cool and moist peripheral zone of the Antarctic islands (subantarctic and temperate zone). There is no vertical zonation of periglacial phenomena, those at sea level being the same as those at elevations up to 1-2 km. 546 ## ‡aIn Russian. 546 ## ‡aRussian transliteration entered into original records using BGN/PCGN 1947 romanisation of Russian; Cyrillic text in MARC 880 field(s) reverse transliterated from this by automated process; BGN/PCGN 1947 text then upgraded to Library of Congress romanisation. 650 07 ‡a551.34 -- Geocryology. Frozen ground.‡2udc 650 07 ‡a551.343 -- Periglacial processes. Thermokarst.‡2udc 650 07 ‡aE8 -- Glaciology: frost action and permafrost.‡2local 651 #7 ‡a(*7) -- Antarctic regions.‡2udc 773 0# ‡6880-03‡7nnas ‡tInformat︠s︡ionnyĭ bi︠u︡lletenʹ Sovetskoĭ antarkticheskoĭ ėkspedit︠s︡ii. ‡gVol. 9 (1959) ‡wSPRI-30495 880 1# ‡6100-01/(N‡aМарков, К. К. 880 10 ‡6245-02/(N‡aПеригляциал Антарктиды /‡cК.К. Марков. 880 0# ‡6773-03/(N‡7nnas ‡tИнформационный бюллетень Советской антарктической экспедиции. ‡gVol. 9 (1959) ‡wSPRI-30495 917 ## ‡aUnenhanced record from Muscat, imported 2019 948 3# ‡a20240418