... groundwater flow through Late Wisconsinan till near Toronto, Ontario . Canadian Geotechnical Journal 33 : 538 – 555 . Godin L. Brown R.L. Dreimanis A. Atkinson G.M. Armstrong D.K. 2002 . Analysis and reinterpretation of deformation features in the Rouge River valley...

... to the northeast (i.e., Boyce and Eyles 2000 ) is different from the process that formed the drumlins in the Rouge River valley, as indicated by the type and orientation of structures at site A (i.e., Zelčs 1987 ). Eyles and Mohajer ( 2003 ) complain that we have not mentioned the Mackinaw interstadial...

...Laurent Godin; Richard L. Brown; Aleksis Dreimanis; Gail M. Atkinson; Derek K. Armstrong Abstract Geometry and timing of deformation affecting Ordovician bedrock and overlying Pleistocene sediments in the Rouge River valley near Scarborough, Ontario, are analysed to evaluate whether...

...RICHARD JOEL RUSSELL Abstract Five Pleistocene glaciations lowered seal levels sufficiently to rejuvenate the Mississippi River system, enabling it to cut valley systems in Louisiana to depths of 100 to over 300 feet. Rising seas of waning glaciation permitted alluvial drowning of these valley...

... in the Rouge River valley, Scarborough, Ontario.” Canadian Journal of Earth Sciences , 40 : 1299 – 1301 . doi: 10.1139/e03-036 . Eyles , N. , Clark , B.M. , Kaye , B.G. , Howard , K.W.F. , and Eyles , C. 1985 . The application of basin analysis techniques to glaciated terrains...

... as surface valleys yield relief of 25–50 m. Low-relief clay and sand plains, incised by modern rivers, have 10–25 m of relief. Gently dipping Paleozoic carbonate and shale beds influence regional groundwater flow and storage beneath thin to thick (10–200 m), carbonate-rich, glacial sediment. Sediment...

... significant constituents of flood plains, nor are they the most important elements in a stream’ load. The burden added to the Mississippi River as the result of bank caving alone, in the course of its alluvial valley below Cairo, has been estimated at about four times the total sedimentary discharge...

..., and their likely impact during erosion and aggradation episodes in the Lower and Middle Mississippi River Valley. Nineteen new Pleistocene optically stimulated luminescence (OSL) values postdate marine isotope stage (MIS) 7 ( Table 1 ). Originating in only 15 drill holes, widely scattered across a very large two...

... of coarse sand and gravel deposited by braided rivers in the Rhine–Meuse paleo-valley. Relative sea-level rise after the Last Glacial Maximum resulted in onlap, and the boundary between Holocene aggradation and incision, i.e., the inland limit of Holocene onlap (see Fig. 2 ), shifted upstream ( Pons 1957...

...…. Following a simple, richly personal service, the U.S. Marine Corps paid the veteran final respect, standing at attention through the haunting playing of taps, carefully folding the flag from his coffin and presenting it to his widow. ’ Laurie Smith Anderson, Journalist, The Advocate, Baton Rouge, December...

...Arthur C. Trowbridge ABSTRACT The delta of Mississippi River seems not to extend much, if any, above Baton Rouge and not to be as old as the Pliocene Citronelle formation. Its coarsest sediments are fine sands with very fine sand, coarse and fine silt, and clay admixtures. Its finest sediments...

...J. F. Dormaar; L. E. Lutwick Abstract Vertical sections of paleosols along the Upper North Saskatchewan River valley show horizons that have distinct brown to reddish-brown colors. Based on such criteria as time for water droplet penetration, magnetic susceptibility, and crystallization of Fe...

.... The regressive erosion is estimated to be of 2.5 m/yr for the Abu Madi valley. K=50. Q Abu Madi =5Q intermediate river =25Q small river .
 F ig . 4. – Profils en long du Nil avant (croix noires) et après (carrées rouges pour les plus petites vallées, croix bleues pour les vallées de taille intermédiaire...

... locations in this region. ORCS—river control structure; SRR—South of the Red River; BL_BR—Baton Rouge sample from Blum and Pecha (2014) . North America has undergone significant climate changes since the Last Glacial Maximum (LGM: ~20 ka) ( Aharon et al., 2012 ; Jackson et al., 2000 ; Quirk et al...

...RICHARD JOEL RUSSELL Abstract Lower Mississippi Valley loess resembles in all essential respects that of the Rhine Valley and other parts of Europe. Its field relationships preclude the possibility of eolian, lacustrine, fluvial, or other direct sedimentary origin. Typical loess grades upslope...

... Societies , 45 , 449 – 455 . Morgan , J. P. ( 1961 ). Genesis and paleontology of the Mississippi River mudlumps: Louisiana Geological Survey, Baton Rouge . Geological Bulletin , 35 . Mozley , P. S. , and Goodwin , L. B. ( 1995 ). Patterns of cementation along a Cenozoic normal...

... and central Europe. The community occupied piedmont-valley-flat red beds within the molasse facies of Variscan uplands. Des traces fossiles de vertébrés sont signalées pour la première fois dans les couches rouges gisant prés du sommet de la séquence mégacyclique II, à Prim Point, dans le sud-ouest de...

... Rouge, a drop of 30 feet in 90 miles. The Red River has built a “cone” of sediments into the valley of the Mississippi in the middle of this stretch, and the natural levees of the river have a relief of 10 feet or more, so that only a general average slope can be given. Sicily Island terrace...

... nodules, and greater kaolinite contents than comparable Holocene flood-plain soils. The primary influence on regional water- table lowering in the southern Lower Mississippi Valley was relative sea-level fall. Mississippi River flood-plain lowering adjacent to the Avoyelles Prairie most likely occurred...