On the sensitivity of Holocene talus-derived rock glaciers to climate change in the Ben Ohau Range, New Zealand / Martin P. Kirkbride, Vanessa Brazier.

MARCXML

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008 230321s1995####xx#a##|##|b##|0||#0|eng#d
035 ## ‡aSPRI-137104
040 ## ‡aUkCU-P‡beng‡eaacr
100 1# ‡aKirkbride, Martin P.
245 10 ‡aOn the sensitivity of Holocene talus-derived rock glaciers to climate change in the Ben Ohau Range, New Zealand /‡cMartin P. Kirkbride, Vanessa Brazier.
260 ## ‡a[S.l.] :‡b[s.n.],‡c1995.
300 ## ‡ap. 353-365 :‡bill.
500 ## ‡aJournal of Quaternary Science : JQS. Vol. 10(4) :353-365 (1995).
500 ## ‡aReferences: Glen, Ice physics bibliography.
520 3# ‡aStudy of mophology and surface age leads to a conceptual model of rock glacier formation with two thresholds: presence of a cool climate and presence of sufficiently thick talus to generate adequate shear stress to induce movement. The ability of this model to explain the phenomena is discussed.
650 07 ‡a551.34 -- Geocryology. Frozen ground.‡2udc
650 07 ‡a551.343.4 -- Rock glaciers.‡2udc
650 07 ‡a01 -- Bibliographies: Glen.‡2udc
650 07 ‡aE8 -- Glaciology: frost action and permafrost.‡2local
651 #7 ‡a(931) -- New Zealand.‡2udc
700 1# ‡aBrazier, Vanessa.
773 0# ‡7nnas ‡tJournal of Quaternary Science : JQS. ‡gVol. 10(4) (1995) ‡wSPRI-78713
917 ## ‡aUnenhanced record from Muscat, imported 2019
948 3# ‡a20230321