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Record #172243:
- #172243
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MARC recordHypothesis on glacial morphology on Amba Aradam mountain (northern Ethiopia) / Mario Panizza.
| Title: | Hypothesis on glacial morphology on Amba Aradam mountain (northern Ethiopia) / Mario Panizza. |
| Author(s): | Panizza, Mario. |
| Date: | 2004. |
| In: | Prace Geograficzne. (2004.), Vol. 189 (2004) |
| Abstract: | Describes geomorphologic features observed in area south-west of Makalé, in Tigray region, at altitude 2500-2780 m a.s.l. These include apparent glacial cirques, moraine, roches moutonnées, etc. Notes restriction of previous reporting of glacial landforms in Ethiopia to much higher elevations. Suggests east-west trending narrow and deep valley, sheltered from wind, could have favoured Pleistocene snow and ice presence and advocates other surveys and climate reconstruction. Proposes alternative hypothesis of "geomorphologic convergence", i.e., coincidence of features of various origins. |
| Notes: | Prace Geograficzne. Vol. 189 :283-298 (2004). Polish abstract. |
| Keywords: | 551.33 -- Glacial geology. 551.336 -- Ice ages. 551.791 -- Pleistocene. 551.331.5 -- Glacial erosion and protection. Sub-glacial topography. 551.331.54 -- Roches moutonnees. 551.331.52 -- Glaciated valleys. 551.332.52 -- Moraines, terminal and recessional. 551.4 -- Geomorphology. 551.583.3 -- Climatic changes, Quaternary. E7 -- Glaciology: glacial geology and ice ages. (6) -- Africa. (236.7) -- East African mountains. |
| SPRI record no.: | 172243 |
LDR 01807naa#a2200000#a#4500 001 SPRI-172243 005 20240416105006.0 007 ta 008 240416s2004####xx#ab#|##|###|0||#0|eng#d 035 ## ‡aSPRI-172243 040 ## ‡aUkCU-P‡beng‡eaacr 100 1# ‡aPanizza, Mario. 245 10 ‡aHypothesis on glacial morphology on Amba Aradam mountain (northern Ethiopia) /‡cMario Panizza. 260 ## ‡a[S.l.] :‡b[s.n.],‡c2004. 300 ## ‡ap. 283-298 :‡bill., map. 500 ## ‡aPrace Geograficzne. Vol. 189 :283-298 (2004). 500 ## ‡aPolish abstract. 520 3# ‡aDescribes geomorphologic features observed in area south-west of Makalé, in Tigray region, at altitude 2500-2780 m a.s.l. These include apparent glacial cirques, moraine, roches moutonnées, etc. Notes restriction of previous reporting of glacial landforms in Ethiopia to much higher elevations. Suggests east-west trending narrow and deep valley, sheltered from wind, could have favoured Pleistocene snow and ice presence and advocates other surveys and climate reconstruction. Proposes alternative hypothesis of "geomorphologic convergence", i.e., coincidence of features of various origins. 650 07 ‡a551.33 -- Glacial geology.‡2udc 650 07 ‡a551.336 -- Ice ages.‡2udc 650 07 ‡a551.791 -- Pleistocene.‡2udc 650 07 ‡a551.331.5 -- Glacial erosion and protection. Sub-glacial topography.‡2udc 650 07 ‡a551.331.54 -- Roches moutonnees.‡2udc 650 07 ‡a551.331.52 -- Glaciated valleys.‡2udc 650 07 ‡a551.332.52 -- Moraines, terminal and recessional.‡2udc 650 07 ‡a551.4 -- Geomorphology.‡2udc 650 07 ‡a551.583.3 -- Climatic changes, Quaternary.‡2udc 650 07 ‡aE7 -- Glaciology: glacial geology and ice ages.‡2local 651 #7 ‡a(6) -- Africa.‡2udc 651 #7 ‡a(236.7) -- East African mountains.‡2udc 773 0# ‡7nnas ‡tPrace Geograficzne. ‡gVol. 189 (2004) ‡wSPRI-25867 916 ## ‡a2005/06/08 -- RF 917 ## ‡aUnenhanced record from Muscat, imported 2019 948 3# ‡a20240416 ‡bRF