Les environs nord et est de Madrid. Présentation d'une carte morpho-pédologique au 1/100000 en couleurs
Carte ; Carte morpho-pédologique ; Castilla la Nueva ; Domaine méditerranéen ; Espagne ; Géographie de l'Europe ; Madrid ; Sol ; Zone subtropicale
In the vicinity of Madrid the limits of the rather simple landforms still coincide, at the scale of 1/100000, with the pedological units (13 soil groups or subgroups). The alluvial terraces and the high and wide Villafranchian levels retain old
soils more or less bleached, rubefied and encrusted after the geochimical environment characteristics and the topographical age. The geopedological map sums up the data usually given by a geomorphological map and a pedological map. It underscores
Les altérations des roches du socle armoricain: relictes morpho-climatiques de la continentalisation post-hercynienne entre Sées et Alençon, Basse-Normandie
Les altérations des roches sédimentaires et cristallines de l'Antécambrien et du Paléozoïque ont été cartographiées et classées en: typeI, altérations évoluées à siallites (illite, kaolinite) localisées sur les surfaces d'érosion (antédoggeriennes
, the AA. have accomplished a multi-criteria analysis that highlights the vulnerability to hydrogeomorphological processes of the investigated watersheds. The basic methods are the analytical and synthetic ones, based on graphical and cartographical models
. The AA. could mention the use of graphical and cartographical data representation.
[b1] Fac. of Geography, Dept. of Geomorphology, Pedology and Geomatics, Univ., Bucarest, Roumanie
the A. has tried to clarify concepts such as the state and mode of activity, dormancy, the return time and the age of a movement. The second part sets out a few principles which may be helpful in applying these cartographic concepts in maps of various scales
[b1] Centre Européen sur les Risques Géo- et Morpho-Dynamiques, Strasbourg, France
Cartographie bio-morpho-sédimentaire des estrans dans le cadre du réseau benthique (complémentarité des orthophotographies littorales et des données LIDAR)
fournies par le Lidar. Les différents thèmes cartographiés correspondent aux structures et aux faciès sédimentaires, aux formations végétales du schorre, aux herbiers de phanérogames, aux macroalgues et aux moulières. Les données altimétriques du Lidar,sont
data and field-surveyed geomorphological data. The study was carried out in a typical Mediterranean area located in southern Italy. The study area was first characterized from a lithological, pedological, land-use and morpho-topographic point of view
The pedological regionalization of the Subcarpathian depression Cracaˇu-Bistriţa
Using a taxonomy based of the pedological and geographical reality, this paper is a synthesis of the previous research of the A., seeing the soil both as a productive and a geographical component of the landscape. - (E. Rusu).
L'instabilité d'une pente ne dépend pas que des systèmes morphoclimatiques du lieu et du moment. Elle peut provenir d'un système d'évolution morpho-tectonique. Ce dernier peut se caractériser par des formes, par un système d'évolution indépendant
des processus morpho-climatiques et s'individualiser par des processus initiaux qui dépendent de la séismicité régionale.
New data on the stratigraphy and pedology of the Clovis and Plainview sites, southern High Plains
The well known Clovis and Plainview paleo-indian sites of New Mexico and Texas have yielded new data on regional late Quaternary geologic, paleoclimatic, and pedologic histories.
Polish pedological studies on Spitsbergen. A review
A review of Polish pedological studies carried out on Spitsbergen since 1957. The first part deals with the important papers going through the sections of soil science. Special attention was focused on arctic soil forming processes, physical
properties (changes in soil volume, soil movements, thermal features), chemical properties and soil biology. Another part gives the lines for future pedological studies.
Palaeoenvironmental interpretation of geomorphological and pedological studies in the rain forest core-areas of Eastern Zaire (Central Africa)
Geomorphological studies on the Late Quaternary landscape evolution in areas of eastern Zaire indicated by pedological, sedimentological, and geochemical evidence that the recent rain forest of the region within the glacial core-areas was strongly
résultat d'un niveau technique en matière d'expression cartographique. Il se compose de trois parties: I. Situation de l'Equateur dans le contexte mondial et continental. II. Géographie du pays, la plus importante où ont été cartographiés au 1:2000000 et 1
| bassins hydrographiques des provinces d'El Ojo, Loja (détermination de zones hydrologiques homogènes au 1:800000)| les provinces orientales: Rio Villano dans la province de Pastaza| reconnaissance morpho-édaphique et répartition de la population au 1
Climatic and non-climatic controls of aridity : the case of the northern Negev of Israel in Arid and semi-arid environments. Geomorphological and pedological aspects.
Influence of eolian sedimentation on soil formation in Egypt and Canary Island deserts in Arid and semi-arid environments. Geomorphological and pedological aspects.