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Record #117223:

Mechanical weathering in the Antarctic: a maritime perspective / Kevin J. Hall.

Title: Mechanical weathering in the Antarctic: a maritime perspective / Kevin J. Hall.
Author(s): Hall, Kevin J.
Date: 1992.
Publisher: Chichester: John Wiley & Sons
In: Periglacial geomorphology. Proceedings of the 22nd Annual Binghamton Symposium in Geomorphology. (1992.),
Abstract: Greater availability of moisture in maritime, in contrast to continental, Antarctic has significant effect on weathering. Data are presented on processes of mechanical weathering, with emphasis on freeze-thaw, from Signy Island. Shows interrelationship of these processes and demonstrates manner in which factors controlling freeze-thaw can exert influence on other processes. Attempt is made to integrate combination of field and simulation data to deduce freeze-thaw mechansim causing rock breakdown. Shows that, compared to continent, maritime weathering rates are slow.
Notes:

In: Periglacial geomorphology. Proceedings of the 22nd Annual Binghamton Symposium in Geomorphology / John C. Dixon, Athol D. Abrahams, eds.

Keywords: 551.34 -- Geocryology. Frozen ground.
551.342 -- Frost shattering.
551.343 -- Periglacial processes. Thermokarst.
551.311.11 -- Geological phenomena caused by low temperatures.
E8 -- Glaciology: frost action and permafrost.
(*7) -- Antarctic regions.
(*725) -- South Orkney Islands.
SPRI record no.: 117223

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100 1# ‡aHall, Kevin J.
245 10 ‡aMechanical weathering in the Antarctic :‡ba maritime perspective /‡cKevin J. Hall.
260 ## ‡aChichester :‡bJohn Wiley & Sons,‡c1992.
300 ## ‡ap. 103-123 :‡bdiags., map.
500 ## ‡aIn: Periglacial geomorphology. Proceedings of the 22nd Annual Binghamton Symposium in Geomorphology / John C. Dixon, Athol D. Abrahams, eds.
520 3# ‡aGreater availability of moisture in maritime, in contrast to continental, Antarctic has significant effect on weathering. Data are presented on processes of mechanical weathering, with emphasis on freeze-thaw, from Signy Island. Shows interrelationship of these processes and demonstrates manner in which factors controlling freeze-thaw can exert influence on other processes. Attempt is made to integrate combination of field and simulation data to deduce freeze-thaw mechansim causing rock breakdown. Shows that, compared to continent, maritime weathering rates are slow.
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 ‡a551.311.11 -- Geological phenomena caused by low temperatures.‡2udc
650 07 ‡aE8 -- Glaciology: frost action and permafrost.‡2local
651 #7 ‡a(*7) -- Antarctic regions.‡2udc
651 #7 ‡a(*725) -- South Orkney Islands.‡2udc
773 0# ‡7nnam ‡aJohn C. Dixon, Athol D. Abrahams, eds. ‡tPeriglacial geomorphology. Proceedings of the 22nd Annual Binghamton Symposium in Geomorphology. ‡dChichester : John Wiley & Sons, 1992. ‡wSPRI-117218
917 ## ‡aUnenhanced record from Muscat, imported 2019
948 3# ‡a20240419