Pregled bibliografske jedinice broj: 761265
J. W. Gregory's contribution to Quaternary geology of Croatia, and some of his dilemmas solved
J. W. Gregory's contribution to Quaternary geology of Croatia, and some of his dilemmas solved // Abstracts and field guidebook / Marjanac, Ljerka (ur.).
Zagreb: Hrvatska akademija znanosti i umjetnosti (HAZU), 2015. str. 24-30 (plenarno, nije recenziran, sažetak, stručni)
CROSBI ID: 761265 Za ispravke kontaktirajte CROSBI podršku putem web obrasca
Naslov
J. W. Gregory's contribution to Quaternary geology of Croatia, and some of his dilemmas solved
Autori
Marjanac, Tihomir ; Marjanac, Ljerka
Vrsta, podvrsta i kategorija rada
Sažeci sa skupova, sažetak, stručni
Izvornik
Abstracts and field guidebook
/ Marjanac, Ljerka - Zagreb : Hrvatska akademija znanosti i umjetnosti (HAZU), 2015, 24-30
ISBN
978-953-347-021-4
Skup
4th Scientific meeting Quaternary geology in Croatia and Slovenia.
Mjesto i datum
Zagreb, Hrvatska, 25.03.2015
Vrsta sudjelovanja
Plenarno
Vrsta recenzije
Nije recenziran
Ključne riječi
Dinarides; glaciation; Dalmatia; Croatia; Montenegro
Sažetak
Gregory's research in Dalmatia, and his 1913 and 1915 publications are unduly forgotten seminal works which provide excellent historical insight into the stage of the art in the early XX century, and his claims and interpretations should be reinterpreted in the light of recent geological and geomorphological reasoning and knowledge. Gregory listed six geomorphological features which are, at higher latitudes, diagnostic of glacial origin, but admited that in Dalmatia these originated by different processes. His dilemma concerning (pseudo)glacial origin of some landforms can be solved now in the light of new evidence. Herein, we present 14 features which document glaciation of the eastern Adriatic coast ; 1) trough valleys, 2) exotic drifts, 3) striated blocks, 4) erratic blocks, 5) moraine ridges, 6) moraine hummocks, 7) kame terraces, 8) ice wedge casts, 9) lacustrine sediments with dropstones, 10) glaciotectonic features, 11) sandur, 12) moutonated rocks, 13) hanging valleys, and 14) glacioisostatic uplift. These evidence come from low altitude locations, as well as locations at the modern sea level, and some imply that the ice had to descent to even lower altitudes. The described glacial features imply that the NE Adriatic coast was affected by a strong glacial advance during Middle Pleistocene. This observation is consistent with recent knowledge on glacial history of the Mediterranean region.
Izvorni jezik
Engleski
Znanstvena područja
Geologija
POVEZANOST RADA
Projekti:
119-0000000-1164 - Impakti i prateći geološki događaji u razvoju Dinarida (Marjanac, Tihomir, MZOS ) ( CroRIS)
Ustanove:
Prirodoslovno-matematički fakultet, Zagreb