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Character and origin of deep arenaceous weathering mantles on the Bega batholith, southeastern Australia
Arène granitique ; Australie ; Batholite ; Bega ; Cristallin ; Granite ; Géographie physique ; Géomorphologie climatique ; Minéralogie ; Météorisation ; New South Wales ; Socle
Les manteaux d'altération arénacés dans le massif granitique de Bega, SE australien, ressemblent à ceux que décrit Millot en Europe. Il s'agit d'une altération hydrothermale de la roche-mère et de la dégradation chimique des biotites et des

Geomorphic responses of lower Bega River to catchment disturbance, 1851-1926
Prior to significant European settlement of the area in the 1850s, lower Bega River on the South Coast of NSW had a narrow, relatively deep channel lined by river oaks. By 1926 the channel had widened extensively (up to 340%) and shallowed
on the morphology and behaviour of Bega River.

The relationship between soils and vegetation ? Beggar's Bush Forest Reserve, Grahamstown

Weathering or hydrothermal alteration?

Altération hydrothermale ; Arénisation ; Australie ; Bega ; Cristallin ; Dartmoor ; England ; Granite ; Géographie physique ; Hydrothermal ; Météorisation ; Royaume-Uni
Bega (Australie) et du Dartmoor sont considérées comme résultat de la météorisation en profondeur.

Géostratégie de l'Atlantique Sud.

Revanchist urbanism heads south : the regulation of indigenous beggars and street vendors in Ecuador

La puissance maritime soviétique.

In this paper, a generic procedure to measure river recovery is developed and applied in Bega catchment, on the south coast of New South Wales (NSW), Australia. The approach is based on analysis of geomorphic units and ergodic reasoning. Historical
data and field analyses are used to identify stages of river evolution throughout Bega catchment. From this, stages of river condition and pathways of adjustment are assessed for 3 river styles at different positions within the catchment. The geomorphic

Variability in sediment delivery and storage along river courses in Bega catchment, NSW, Australia : implications for geomorphic river recovery

Une forme particulière de charisme. A propos du bégaiement charismatique. Qui est Adam Michnik ?

Antecedent landscape controls on river character, behaviour and evolution at the base of the escarpment in Bega catchment, South Coast, New South Wales, Australia
Présentation des 3 types de morphologie fluviale observés à la base de l'escarpement dans le bassin versant de la Bega, Nouvelle-Galles-du-Sud. Chaque site possède des caractères distincts, à savoir un système de creusement et remblaiement, une

In this study, a detailed investigation of the soils formed on Wallagaraugh Adamellite (a component of the Bega Batholith) of the southeastern lowlands of Australia has been used to produce a hybrid soil-landscape model for this granitoid parent

This paper reports the sedimentary and thermoluminescence evidence from barrier beaches dating from the Last Interglacial at Middle Lagoon (also known as Tanja Lagoon) and Gillards Beach, 4-6 km north of the mouth of the Bega River, on the far south

This paper describes the nature of valley fill deposits at the base of the escarpement in part of Bega catchment. Extensive valley fills, up to 12 m deep but no greater than 300 m wide, have formed in the upper reaches of Wolumla Creek, a north

of soil production rates with increasing soil thickness across the passive margin exposed in the Bega Valley, south-eastern Australia, and found remarkable similarities in rates. Quantifying such rates and processes help determine spatial variations

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