... and the Forêt de Chaux along the N060°E-trending present-day Doubs valley [ Liniger, 1967 ; Bonvalot, 1974 ; Chauve et al. , 1979 ; Petit et al. , 1996 ; Madritsch et al. , 2010a ]. This ancestor is often referred to as the Paleo-Aar-Doubs river. To the southwest, gravels of the Forêt de Chaux area show...

...Claude Grandjacquet Abstract Three principal structural elements are recognized in the Salins tectonic unit in the area west of the Loue valley, between Bolandoz and the Mouthier depression in Doubs, France--the Ornans (a slightly dislocated foreland zone), an intermediate buffer zone...

...Maurice Dreyfuss Abstract The marshes of the Drugeon valley in the Jura region, France, are peaty depressions between masses of moraine gravels. They are usually easily drained. In the case of the Champlive basin, near Baume-les-Dames, a natural underground outlet was improved. The Saone marsh...

...Fig. 6. Anticlinal foreridges of the High Jura, near Pontarlier. View from southwest, from the Doubs valley. ...

... to Callovian. Introduction The present note records the find of one species each of the brachiopodl5 genus Arceythyris from two different stratigraphic levels within the Sulcacutus Beds exposed near Kibber (32°20' : 78°04') in the Spiti valley. The stratigraphic succession exposed near Kibber along...

...°) at the site, with the largest SOC contents at the valley bottom, close to a drainage ditch. The SOC gradient is probably a legacy of decreasing water table depths toward the valley bottom. The field was under grass and clover ley (50% timothy [ Phleum pratense L.], 25% red clover [ Trifolium pratense L...

... at limb bone scaling in macropods and quadrupedal artiodactyles, Doube et al. ( 2018 ) speculated that the hopping behavior of macropods might have enhanced repair of fatigue damage by increasing bone remodeling. However, unexpectedly, they found that a femur of Macropus gianteus Shaw, 1790 , lacked...

... the trunk valleys and distinct bedrock straths at their junction with tributary valleys. This landscape has evolved as a result of fast base level changes in response to repeated glaciations during the Quaternary. As the archives related to the evolution of this transient landscape are scarce, available...

... Valley (Bagh Beds), Madhya Fossils De let Letage Albein Dec Montcley (Doubs). Pradesh and Gujarat. Pal. Indica (N.S v. 42, 106p, Mem. Soc. Geologique De France Tome Premier v, EHRENBERCC.G, .(1 840). Uber die Bildung der Kcidefelsen pp. 1-84, und des Kreidemergelsdurch UnsichtbareOrganismen. BISWASS,.K...

... \ CHWA Y 56°r F 8145 A X 'i'2'4-; 123° qR P/NE PASS 0 8 16 24 32 SCALE IN MILE S 121° I 145 FTC . 1Index map of Peace River area, British Columbia . side of the Peace River valley near Stott Creek, which were reported to contain Dielasma, Spiri,fer, Notothyri-s, Edmondia, Solemya, Schizodus...

... by Redfield (113) 1 , on pages 97 to 103 of which the possible oil-bearing regions of the country are classified as (1) the Rhine trough, (2) Jura Mountains, (3) Lower Languedoc, (4) Aquitanian basin, (5) Paris basin, and (6) Limagne valley. Redfield’s paper, like all literature on the subject, has been...

... and extraglacial features in Britain is reviewed by Hutchinson (1991 a , 1992). Of these, the following are particularly important: the periglacial solifluction of clayey materials*, periglacial and Post-glacial landslides and rockfalls, superficial valley disturbances* (including cambering and valley bulging...

... and wasps, tiger beetles, and dung beetles also are known to construct vertical burrows with some form of a terminal chamber (e.g., Evans 1963 ; Michener 1974 ; Stanley and Fagerstrom 1974 ; Ratcliffe and Fagerstrom 1980 ; Doube 1991 ; Hasiotis et al. 1993b ; Hasiotis 2002 ; Hembree et al. 2005...

... MOTICHIKlI ~\YDo 2i KAOlPANI Fig. 1. A. Exposures of Bagh Beds along the Nannada Valley B. Bagh Beds along the Gandharva Nala. BI (Borghal; 22"24',75"05') and DI (Dhantalav; 2r22', 75"05') arc the localities from where the Nodular Limestone was collected. C. Bagh Beds along the Man River Region ZI (Zirabad...

... moraines which extend down the valley significantlyfarther than the Qg4 moraines. Figure 4 shows further details which pertain to the age of the Qg4 glaciogenic sediments. Thin (<15 cm), weak A horizons and thin (<30 cm), poorly developed B k or B w horizons characterize soils developed in morainal...

... to the caveats required to study the localization of vines: I have some causes to suspect that the separation of the mountain from the vineyards that the préfect of Doubs has highlighted has no geological effects and that it only derives from the fact that the valley of the Doubs, being very deep, has...

... Hauterivian of Ukraine (Krymskaya, Simferopolskij district, Alma river, Partizany [=Sably]); Barremian of France (Doubs, Morteau); late Barremian of Poland (Malopolskie, Tarnów, Trzemesna); early Aptian of Poland (Malopolskie, Wadowice, Lanckorona, Jastrzebia); late Albian of United Kingdom (Devonshire...

... Sediments in the Southern Bight of the North Sea Geol Mijnb 1968 47 245 73 Hoyt J. H. Oostdam B. L. Smith D. D. Offshore sediments and valleys of the Orange River (South and South West Africa) Mar Geol 1969 7 69 84 Kennedy W. J. Klinger H. A major intra...

...Eva C. Herbst; Michael Doube; Timothy R. Smithson; Jennifer A. Clack; John R. Hutchinson Abstract Bone healing is an important survival mechanism, allowing vertebrates to recover from injury and disease. Here we describe newly recognized paleopathologies in the hindlimbs of the early tetrapods...