Scott Polar Research InstituteSPRI library catalogue
Search the catalogue
Browse recordsView a record
Please note: You are viewing the legacy database of the Scott Polar Research Institute Library catalogue. It is no longer being updated, so does not reliably reflect our current library holdings.
Please search for material in iDiscover for up-to-date information about the library collection.
Record #110905:
- #110905
Main publication details
MARC recordCryoplanation surfaces in the central Andes at latitude 35° S / Santiago A. Grosso, Arturo E. Corte.
| Title: | Cryoplanation surfaces in the central Andes at latitude 35° S / Santiago A. Grosso, Arturo E. Corte. |
| Author(s): | Grosso, Santiago A. Corte, Arturo E. |
| Date: | 1991. |
| In: | Permafrost and Periglacial Processes. (1991.), Vol. 2(1) (1991) |
| Abstract: | General survey. Most terraces occur in areas with mean annual air temperatures <-1°C. Largest on sedimentary rocks where m.a.a.t. are near 0°C; possibly inactive now and were formed during colder episode. Thought to be result of frost shattering, frost heave and gelifluction of frost-susceptible (porous) rocks in climate with numerous freeze-thaw cycles. |
| Notes: | Permafrost and Periglacial Processes. Vol. 2(1) :49-58 (1991). |
| Keywords: | 551.34 -- Geocryology. Frozen ground. 551.342 -- Frost shattering. 551.343 -- Periglacial processes. Thermokarst. E8 -- Glaciology: frost action and permafrost. (82) -- Argentina. (83) -- Chile. (238.1) -- Andes. |
| SPRI record no.: | 110905 |
LDR 01323naa#a2200000#a#4500 001 SPRI-110905 005 20230324083012.0 007 ta 008 230324s1991####xx#ab#|##|###|0||#0|eng#d 035 ## ‡aSPRI-110905 040 ## ‡aUkCU-P‡beng‡eaacr 100 1# ‡aGrosso, Santiago A. 245 10 ‡aCryoplanation surfaces in the central Andes at latitude 35° S /‡cSantiago A. Grosso, Arturo E. Corte. 260 ## ‡a[S.l.] :‡b[s.n.],‡c1991. 300 ## ‡ap. 49-58 :‡bill., diags., tables, map. 500 ## ‡aPermafrost and Periglacial Processes. Vol. 2(1) :49-58 (1991). 520 3# ‡aGeneral survey. Most terraces occur in areas with mean annual air temperatures <-1°C. Largest on sedimentary rocks where m.a.a.t. are near 0°C; possibly inactive now and were formed during colder episode. Thought to be result of frost shattering, frost heave and gelifluction of frost-susceptible (porous) rocks in climate with numerous freeze-thaw cycles. 650 07 ‡a551.34 -- Geocryology. Frozen ground.‡2udc 650 07 ‡a551.342 -- Frost shattering.‡2udc 650 07 ‡a551.343 -- Periglacial processes. Thermokarst.‡2udc 650 07 ‡aE8 -- Glaciology: frost action and permafrost.‡2local 651 #7 ‡a(82) -- Argentina.‡2udc 651 #7 ‡a(83) -- Chile.‡2udc 651 #7 ‡a(238.1) -- Andes.‡2udc 700 1# ‡aCorte, Arturo E. 773 0# ‡7nnas ‡tPermafrost and Periglacial Processes. ‡gVol. 2(1) (1991) ‡wSPRI-102743 917 ## ‡aUnenhanced record from Muscat, imported 2019 948 3# ‡a20230324