... sediment-bearing ice low in solutes (e.g., Fe and Cl; Raiswell et al., 2008 ). In addition, two new samples were collected from sediment-rich (SV1) and sediment-poor (SV2) basal ice in Monaco Glacier (Svalbard, 79°30′N, 12°40′E), and three new samples (IS2B, IS3B, and IS3T) were collected from water...

...}\ +\ 4SO^{2{-}}_{4}\ +\ 8H^{+}\] \end{document} Sediment samples were collected from icebergs in the Southern Ocean and subglacial ice (both sediment-rich and sediment-poor) from Taylor and Canada Glaciers (Antarctica) and the Monaco Glacier (Svalbard) (see Raiswell et al . (2008 ) for further...

... in the School of Environmental Sciences, at the University of East Anglia. These colleagues and myself are about to carry out dye-tracing experiments on glaciers in the Swiss Alps. The graduate students are diluting the rhodamine dye and getting ready to inject the dye into a crevasse. We intend to collect...

... submerged off the coast of southern Brazil, because Permian glaciers came from there. Willis and Schuchert agreed that bathymetric data should be used to determine where the land bridges might have been. The job of placing the bridges went to Willis. He explained in his paper that in 1920 he had...

... (La Brasque Farm) but its stratigraphic position remains unclear. Further, Saint Martin and Saint Martin (2018) described micro-inclusion in amber grains from the nearby Mazaugues area (Glacières de Pivaut). Therefore, a start has been made on examining localities of the Sainte-Baume Massif...

..., the first ascent of Mont Blanc in August 1787, and to him we owe the usage of the terms ‘glacier’, ‘seracs’ and ‘moraines’, and, a good deal of understanding of glaciers. His published writings on the Alps: “ Voyages dans les Alpes ” (four volumes in 1779, 1786, 1796, 1796) however, were subsequently mined...

... and forest fringes better than native species ( Rojas et al. 2011 ), as they can thrive in resource-poor habitats ( Monaco et al. 2005 ; Funk & Vitousek 2007 ). In this type of forest the main arboreal components are Neolamarckia chinensis (Roxb.) Bosser, Aphanamixis polystachya (Wall...

... ; Malloy and Hurley, 1970 ; Emery and Uchupi, 1972 ; Pinet and Popenoe, 1982 ). MU-B sediments south of Jordan Knoll are probably distal equivalents of the lower Eocene Monacos and Biejos Groups of northern Cuba. These rocks are typically flysch/olistostromes composed of coarse carbonate breccias...

... during the Holocene . Paleoclimate Research; Paläklimaforshung n o spec 25 .  Aloïsi JC , Monaco A , Pauc H. 1975 a. Mécanismes de la formation des prodeltas dans le Golfe du Lion. Exemple de l'embouchure de l'Aude (Languedoc) . Bulletin de l'Institut de Géologie du...

... in a complex geologic area: A case study from Mt. Etna volcano (southern Italy) , Nat. Hazards 86 , no.  2 , 385 – 399 . Panzera F. Lombardo G. Monaco C. , and Di Stefano A. 2015 . Seismic site effects observed on sediments and basaltic lavas outcropping in a test site of Catania...

.... 2002 Effects of volcanic eruptions on the CO 2 content of the atmosphere and the oceans: the 1996 eruption and flood within Vatnajökull Glacier, Iceland. Chemical Geology 190 181 205 10.1016/S0009-2541(02)00116-X Glass L.M. Phillips D. 2006 The Kalkarindji continental flood...

.... O'Cofaigh (eds.), Glacier-influenced Sedimentation on High-latitude Continental Margins . Geological Society of London, special publication , 203 . Boury-Esnault , N. , and J. Vacelet . 1994 . Preliminary studies on the organization and development of a hexactinellid sponge from...

... , Sherman glacier rock avalanche, Alaska, USA, in B. Voight, ed., Rockslides and avalanches, 1 : New York , American Elsevier Publishing Co. , p. 197 – 256 . Mellor , M. , 1978 , Dynamics of snow avalanches, in B. Voigt, ed., Rockslides and avalanches, 1 : New York , American Elsevier...

... 208 0 2 Fort Sumter National Monument South Carolina 95 59 2 Gateway National Recreation Area New Jersey/New York 10,767 7,099 232 George Washington Birthplace National Monument Virginia 268 9 8 Glacier Bay National Park and Preserve Alaska 2,455,134 242,249 1,897...

...) and Mt. Emilius (ME) and Glacier Rafray (GR) Nappes; f, Gneiss Minuti Complex (GMC) of the Sesia Zone and Arolla Series (AS) of Dent Blanche Nappe; g, Second Dioritic-Kinzigitic Zone (II DK) of the Sesia Zone and Valpelline Series (VS) of the Dent Blanche Nappe; h, Post-Alpine intrusions of Traversella...

.... La Brasque 43°19’24.9"N, 5°42’23.2"E MNHN-PC    12b. Dowtown 43°21’06.2"N, 5°51’15.8"E PC 13. Mazaugues Santonian    13a. Equireuil Quarry 43°21’39.6"N, 5°57’23.8"E MNHN-PC    13b. Glacières de Pivaut 43°21’12.5"N, 5°51’14.2"E MNHN-PC The amber samples were observed...

... to the Late Permian ( Veevers and Powell, 1987 ; Crowell, 1999 ; Isbell et al., 2003 ). Glaciers achieved their maximum paleolatitudinal range between the middle Stephanian (ca. 305 Ma ago) and near the end of the Sakmarian (ca. 284 Ma ago) ( Isbell et al., 2003 ). Three episodes of major ignimbrite...

.... Formation model via organic matrices (Lizard Island, Great Barrier Reef, Australia) , in Allemand , D. , and Cuif , J.-P. , eds., Biomineralization 93: Proceedings of the 7th International Symposium on Biomineralization : Institut Océanographique, Monaco, Bulletin , Numero Special 14 ( 2...

... and animal husbandry. The relief was formed by the glacier lobe of the Late Weichselian Glaciation; glacial and glaciolacustrine sediments dominate, and, to less extent, glaciofluvial sediments ( Guobytė 2002 ). The glaciolacustrine plain (20–25 m a.s.l.) consisting of fine grained and clayey sand...

... to the sedimentary supply of local rivers, for instance due to a decrease in precipitation. Potential correlation can be attempted with advance phases of Andean glaciers: the age gap between ca. 5.3 and 4.4 kyr cal BP overlaps to the ages suggested by P orter (2000) for the onset of Neoglaciation in southern...