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Portail d'information géographique

Résultats de la recherche (10 résultats)

Soils of the central North Downs: their distribution, derivation and geomorphological significance

Soils of the central North Downs: their distribution, derivation and geomorphological significance
Présentation des résultats d'une étude systématique des sols dans la région centrale des North Downs. Détermination de l'origine de l'alluvionnement par une analyse des caractères granulométriques et des minéraux lourds, de 114 prélèvements de sol
1995

Sedimentation in ice-dammed glacial lake Assiniboine, Saskatchewan, and catastrophic drainage down the Assiniboine valley

Sedimentation in ice-dammed glacial lake Assiniboine, Saskatchewan, and catastrophic drainage down the Assiniboine valley
1995

Nonlinear responses of soil erosion to climate change: a modelling study on the UK South Downs

Nonlinear responses of soil erosion to climate change: a modelling study on the UK South Downs
1995

Particle size-pediment slope relations: some findings from Saudi Arabia

of pedisediments were obtained and the moments used for pair-wise comparisons with down pediments changes in pediment slope. It is shown that simple comparisons of standardised regression coefficients are misleading and a formal test is introduced.
1995

Infrastructure policy in the Randstad Holland: struggle between accessibility and sustainability

. In these plans environmental and economic interests are at odds with each other. The implementation of infrastructure policy is complicated and slowed down. A more balanced infrastructure policy is advocated.
1995

Journey to asylum: a medical-geographical idea in historical context

originated, was debated and was seen to break down. The paper examines contexts in nineteenth-century England, associated with the territorial structure of the public county asylum system.
1995

Estimating the probability of river channel adjustment

DOWNS, P.W.
1995

Older industrialized regions

DOWNING, A.
1995

Anfang und Umbau des Gewässernetzes zwischen Wupper und Sieg (Oberbergisches Land, rechtsrheinisches Schiefergebirge)

and meandring rivers. During the uplift of the Rhenish Massif these rivers in its meandring manner were leaded down to the Variscan body, and directed toward the Rhine main river. The change from the system of flushing areas to linear erosion by river drainage
1995

An interdisciplinary approach to evaluation of potential instability in alluvial channels

DOWNS, P.W.
1995