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  • The study of large erratic boulders casts new light on some glacial palaeogeography problems in the Apuan Alps
  • Appennino ; Erratic boulder ; Geochronology ; Glacial features ; Italy ; Palaeogeography ; Spatial distribution ; Toscana
  • Erratic boulders of glacial origin, mainly made of jasper, marble and cherty limestone, are found in the main valleys of the Apuan Alps. Such boulders are especially widespread in the north-eastern sector of the Apuan Alps, sometimes in great number
  • , and they bear witness to a 6 km long journey. The types and distribution of the erratic boulders allow one to outline the dimensions of the main glacial bodies and assess the relationships between them. Moreover, the presence of erratic boulders opens new
  • avenues of research in order to complete the description of the Apuan glaciation and its chronology by using the techniques of exposure age dating, which can be easily applied to erratic boulders. - (NFà.
  • Boulder depressions in central Sweden. Remnants of a pre-Late Weichselian landscape?
  • Drumlin ; Erratic boulder ; Glaciation ; Moraine ; Palaeogeography ; Periglacial features ; Quaternary ; Sweden
  • During geomorphological mapping of an area in central Sweden, it was found that areas of boulder depressions tended to be mutually exclusive with drumlinized and Rogen moraine areas of Late Weichselian origin. This irregular erosion pattern probably
  • reflects the fact that the Late Weichselian ice sheet was partially frozen to its bed. If the situation is the same in other parts of Fennoscandia, boulder depressions may prove to be a helpful feature when searching for warm- and cold-based areas
  • Boulder deposits from large waves during the last interglaciation on North Eleuthera Island, Bahamas
  • Aminostratigraphy ; Bahamas ; Coastal dynamics ; Coastal environment ; Erratic boulder ; Interglacial ; Mass movement ; Pleistocene ; Rainstorm ; Stratigraphy ; Tsunami ; Wave
  • This paper presents a detailed description of the boulders of north Eleuthera and demonstrates that they were deposited by waves during the Pleistocene. It describes the time and stratigraphy related to boulder emplacement, and evaluates tsunamis
  • Crystalline rocks ; Duricrust ; Erratic boulder ; Karokoram ; Moraine ; Pakistan ; Valley ; Weathering
  • This paper reports on rock temperature fluctuation in the north and south surfaces of a moraine boulder in Hunza Karakoram obtained over 2 years, and concludes that the rock surface weathering processes depend primarily on the differences
  • Downslope displacement rates of ploughing boulders in a mid-alpine environment : Finse, southern Norway
  • Erratic boulder ; Freeze-thaw cycle ; Gelifluction ; Global Positioning System ; Mountain ; Norway ; Periglacial features ; Slope dynamics ; Survey
  • Annual and seasonal displacements of ploughing boulders were investigated at Finse, by traditional surveying and differential carrier-phase global positioning system measurements. Annual displacement rates were mainly below 10mm/year
  • . There was a tendency for larger boulders to travel faster. Seasonal displacements were restricted to the annual freeze-thaw cycle. The concept of frost creep seems not applicable to the investigated ploughing borders. On the hand, due to tilting of the boulders
  • Differential rock weathering in the Valley of the Boulders, Kärkevagge, Swedish Lapland
  • Chemical erosion ; Cold area ; Differential erosion ; Erratic boulder ; Geochemistry ; Lapland ; Mineralogy ; Sweden ; Weathering
  • Geomorphological environment of boulders and grain-size analysis of gravel sheets in the Southern Börzsöny, Hungary
  • Erratic boulder ; Geomorphology ; Grain size distribution ; Gravel ; Hungary ; Komáron-Esztergom ; Lithology ; Mountain ; Slope deposit
  • similarity between the samples collected from the occurrences. In the environment of both locations some boulders are found composed of quartzite. In the opinion of the author these boulders were very probably transported by floating frozen ice floes. - (AM)
  • Antarctica ; Erratic boulder ; Geochronology ; Glacial features ; Kame ; Moraine ; Palaeo-environment ; Periglacial features ; Quaternary
  • The glacial geology was investigated with the purpose of studying the genesis and chronology of the glacigenic deposits in the Tumbledown Cliffs area on the west coast of James Ross Island. Erratics are evidence of an earlier, more widespread
  • Biostratigraphy ; Chalk ; England ; Erratic boulder ; Foraminifera ; Glaciation ; Moraine ; Palaeogeography ; Palaeontology ; Pleistocene ; United Kingdom
  • sheets. This technique involves extracting foraminifera from Chalk erratics and till matrix obtained from stratigraphically controlled till sections and comparing their micropaleontologywith that of Upper Cretaceous Chalk bedrock. The revised ice-flow
  • Cosmogenic Be 10 and Al 26 exposure ages of tors and erratics, Cairngorm Mountains, Scotland : timescales for the development of a classic landscape of selective linear glacial erosion
  • Earth surface processes ; Erosion rate ; Erratic boulder ; Glacial erosion ; Glacial features ; Isotope dating ; Model ; Scotland ; United Kingdom ; Weathering
  • Carrying capacity ; Catastrophe ; Coastal environment ; Erratic boulder ; Flood ; Grain size distribution ; Heavy rain ; Mudflow ; Valley ; Venezuela
  • ) affected by debris flows, and discuss the grain-size distribution with regard to the buoyancy and competence of the debris flows for boulder transport.
  • Aminostratigraphy ; Bahamas ; Climatic variation ; Coastal dynamics ; Coastal environment ; Coastal geomorphology ; Erratic boulder ; Interglacial ; Rainstorm ; Sea level ; Stratigraphy
  • On low-lying areas of the Bahamas, extensive V-shaped storm-beach ridges (chevrons in this paper) were emplaced by similar, high-energy events. The origin of these storm ridges, associated run-up features, and boulder deposits, plus the implications
  • Australia ; Coastal geomorphology ; Erratic boulder ; Fracture ; Inselberg ; Slope ; Soil erosion ; South Australia ; Weathering
  • Flared slopes are smooth concavities caused by subsurfacemoisture-generated weathering in the scarp-foot zone of hillslopes or boulders. They are well represented in granitic terrains but also developed in other massive materials such as limestone
  • The results of an almost 100 years lasting research on fossiliferous sedimentary and cristalline erratic boulders at the marginal zone of the Scandinavian glaciation with the boulder association of various basal tills, of the reconstructed ice
  • Aeolian features ; Erratic boulder ; Micromorphology ; Periglacial features ; Shoreline ; Snow ; Sweden ; Weathering
  • Cold area ; Dating ; Erratic boulder ; Glacial features ; Greenland ; Lichenometry ; Moraine
  • Deglaciation ; Erratic boulder ; Geomorphology ; Glacial deposit ; Glacial erosion ; Glaciation ; Glacier ; Mountain ; Thermokarst
  • Windpolished boulders as indicators of a Late Weichselian wind regime in Denmark in relation to neighbouring areas
  • Aeolian features ; Denmark ; Erratic boulder ; Ice sheet ; Palaeo-environment ; Quaternary ; Spatial variation ; Wind ; Wind erosion
  • Frost heave and thaw consolidation of ploughing boulders in a Mid-Alpine environment, Finse, Southern Notway
  • Cold area ; Erratic boulder ; Freezing ; Heat transfer ; Norway ; Statistical analysis ; Thawing ; Vertical movement
  • Les cordons de blocs frangeants (boulder barricades). Mise au point avec exemples du Québec
  • Canada ; Coastal dynamics ; Coastal environment ; Cold area ; Erratic boulder ; Estuary ; Floating ice processes ; Foreshore ; Palaeo-environment ; Quebec ; Saint-Laurent ; Sand bar