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Morocco tops the 20 million mark

A paleovalley system in the floodplain of the Mark River (Central Belgium)
Belgique ; Fluviatile ; Géographie physique ; Holocène ; Mark ; Paléo-environnement ; Paléohydrologie ; Paléovallée ; Quaternaire zones moyennes ; Sédimentation
Un programme de sondage dans la plaine d'inondation de la rivière Mark a révélé un système fluvial fossile important, encaissé dans des sables fluviatiles probablement d'âge pléniglaciaire et recouvert de matériel éolien. Les conséquences
1985

Znaky urbanistickych premien slovenskych miest. (Marks of urban transformations in Slovak towns)
1985

The Weichselian Late Glacial in a small Lowland valley (Mark river, Belgium and the Netherlands)
Belgique ; Cours d'eau ; Fluviatile ; Géographie physique ; Lit fluvial ; Mark rivière ; Paléobotanique ; Paléoclimat ; Pays-Bas ; Quaternaire ; Stratigraphie ; Tardiglaciaire ; Weichselien
La rivière Mark a établi un cours à méandres profondément entaillés au début du Tardiglaciaire par suite des changements du climat et de la couverture végétale. L'incision maximale a été atteinte entre 11 780 et 11 920 B.P. Cela a donné lieu à un
1985

Profile type maps of alluvial deposits-The case of the Mark River, Belgium in Fluvial geomorphology. In memoriam J. N. Jennings.
Belgique ; Cartographie thématique ; Fluviatile ; Géographie de l'Europe ; Holocène ; Lithologie ; Mark rivière ; Plaine alluviale ; Quaternaire zones moyennes ; Représentation cartographique ; Roche
1985

Three sections containing Late Glacial deposits (especially of Allerod Interstadial Age) are described. The stratigraphy of the Late Glacial is discussed for the area of Schleswig-Holstein. The Bolling Interstadial is well marked by a maximum
of Betula pollen (tree birches). Below this a less marked Meiendorf-Interstadial is characterized by maxima of Betula nana and Hippophae.
1985

Mark och vattenvard i sodra Afrika. (Protection des sols et de l'eau en Afrique australe)
1985

Correlation of the Rockland ash bed, a 400,000-year-old stratigraphic marker in northern California and western Nevada, and implications for Middle Pleistocene paleogeography of central California
1985

Design and conservation in the city. (Papers to mark the 75th anniversary of publication of the Town Planning Review)
1985

The analyses of position of signifiant Slovak towns and the influence of natural conditions on their development are examined on the basis of fundamental geographical data with marking areas for urbanistic development programs. (MS).
1985

Tufa activity in N. Cape S.A.

Lichenometric studies from four glaciers in Northern Iceland are used to determine the dates of their Little Ice Age maxima. In all cases these date to the last half of the nineteenth century and probably marked the maximum Neoglacial extent
1985

On the basis of biostratigraphical, magnetostratigraphical, paleoclimatological and sedimentological studies of the continuous Pliocene-Pleistocene sequences, the M/G boundary is found an important marker in North China. The evidence of mammals
1985

The change from limnic to terrestrial sedimentation is regarded as a marker of the N/Q boundary in the Carpathian basin. It is roughly synchronous with the Matuyama-Gauss paleomagnetic reversal (million years). The boundary is easy to trace
1985

The lower part of a 5. m core from Hay Lake (34 N, 109 25W) at 2780 m in east-central Arizona provides a pollen record for the middle Wisconsin. The middle Wisconsin climate is inferred to have been cooler than today and is marked by more available
1985

Patterns of glacial fluctuation are related to the general trends in climate. Between 1862 and 1888 there was locally important glacier recession. This was followed by a cooler period marked by glacier advance. A glacier stillstand is recorded
1985

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