Fiatal lepusztulasi szintek, jelenkori geomorfologiai folyamatok a Pannonhalmi-dombsagon. (Young erosional surfaces and recent geomorphic processes in the Pannonhalma Hills)
The occurrence of young erosional surfaces, the major features of drainage changes in the Pleistocene, the formation of derasion valleys and landslides and the types and distribution of recent geomorphic processes are studied. (DLO).
Beispiele für jungholozäne Bodenerosion und Bodenbildung im Untereichfeld und Randgebieten. (Examples of young Holocene soil erosion and pedogenesis in Southern Lower Saxonia)
Ukazanija za mladi naprecni razmestvanija na blokove v Trako-Mizijskata kolizionna zona na Balkanite Evidence for young transverse block faults in the Thracian-Moesian collision zone on the Balkan peninsula
The main watershed in Bulgaria follows the Diagonal Swell, the young geological structure having affected the geodynamic processes during the neotectonic period. - (SBV)
1974 ; DOCUMENTATION ; ECONOMIE RURALE ; GEOGRAPHIE HISTORIQUE ; GEOGRAPHIE REGIONALE ; Géographie de l'Europe ; MIDLANDS, OUEST ; MINE ; PAYSAGE ; PERCEPTION DE L'ESPACE ; ROYAUME-UNI ; SIECLE XX ; STAFFORDSHIRE, SUD ; TOPONYMIE ; WALES ; YOUNG (F
L'APPORT DU NOUVELLISTE A LA SCIENCE GEOGRAPHIQUE NE SE LIMITE PAS AU PITTORESQUE ET AU PSYCHOLOGIQUE. DANS LA CARACTERISATION D'UNE REGION, COMME LA BLACK COUNTRY DU PAYS DE GALLES, CHOISIE PAR FRANCIS BRETT YOUNG AU DEBUT DE CE SIECLE POUR CADRE
Zur Feinstratigraphie und Paläopedologie des Jungpleistozäns nach Untersuchungen an südniedersächsischen und nordhessischen Lossprofilen. (Fine stratigraphy and palaeopedology of the younger Pleistocene in accordance to investigations of loess
Geological and palynological investigations of two main dune systems west of Nieuwpoort. The Old Dune system is believed to be older than 4300 B.P. The Young Dune area has a complex history: older dunes (2800-900 B.P.) underneath the Young Dune
Yellow-legged herring gulls prey on the Greater Flamingo breeding colony in the Camargue (southern France), taking both eggs and chicks. They kill young chicks in their nest and flightless young forming large aggregates (crèches). Flamingos are very
Selected loess profiles in Poland, Hungary and Slovakia have been analyzed. Interpretations and parallelizations by distinguished authors are compared. The stratigraphic units of old interglacial soil, old loess, young interglacial soil and young
Een eeuwen jong podzolprofiel op de Schaijksche Heide palynologisch bekeken. (A centuries young section of podzolised soil from the Schaijksche Heide (The Netherlands), a palynological interpretation)
Bükk Mts can be classified as young formation of Alpine structural features and shows the pecularities of denuded plateaus and block-mountains composed by sedimentary, igneous and eruptive rocks and ophiolites. (CK).
In the young loess series of Basaharc type locality two stratotype paleosols occur ( Basaharc Double = BD1, BD2, and Basaharc A complexes) representing two marker horizons in the lower and middle part of young loess in Hungary. The Basaharc Double
of dendrochronology appeared to be 13,6 mm per year. Uneroded talus age corresponds to the age of its base and that of the scree slope. Eroded talus are younger than their base and far younger than the scree slope.
Precise hints about the moulding of the mountain and the Thuringian Basin as a result of younger, tertiary quaternary movements of the crust after an old young mesozoïque/old-tertiary pediplanation with inselbergs of subtropical-tropical type could
Young ecotone ecosystems differ from the original ones by their dynamicity, heterogeneity of successions and banded structure. The main factors of ecotones change on the site level of natural systems organization are humidity and salinity of soils
. For ecotones of land-system level they are : edapholithologic, geomorphologic and hydrogeologic peculiarities of the region, its economic development, intensity and character of initial vegetation. It is advisable to create a classification of young ecotone