𝔖 Bobbio Scriptorium
✦   LIBER   ✦

MORPHOLOGY AND DEVELOPMENT OF SELECTED BADLANDS IN SOUTHEAST SPAIN: IMPLICATIONS OF CLIMATIC CHANGE

✍ Scribed by CALVO-CASES, A.; HARVEY, A. M.


Publisher
John Wiley and Sons
Year
1996
Tongue
English
Weight
685 KB
Volume
21
Category
Article
ISSN
0360-1269

No coin nor oath required. For personal study only.

✦ Synopsis


Four areas were selected to represent a range of processes characteristic of badland surfaces in southeast Spain: Petrer and Monnegre in Alicante, Vera and Tabernas in Almeria. At Petrer, rilling and swelling processes produce a deeply cracked surface drained by a finely textured network of shallow rills. At Monnegre, piping and rilling are differentially developed on slopes ultimately controlled by basal incision. At Vera, aspect-controlled lichen and vegetation cover produce a sequence of badland development within which the relative importance of piping, mass movement and rilling varies through the sequence. At Tabernas, simple overland flow is the dominant process, but aspect influences rill network density and badland evolution.

The factors controlling badland development can be grouped into those related to gross morphology, to surface cover and runoff generation, and to material properties. These factors are effective over varying timescales, implying that morphological response times differ among the selected badlands.


πŸ“œ SIMILAR VOLUMES


THE ROLE OF ALLUVIAL FANS IN THE MOUNTAI
✍ HARVEY, A. M. πŸ“‚ Article πŸ“… 1996 πŸ› John Wiley and Sons 🌐 English βš– 820 KB

The mountain fluvial systems of southeast Spain involve sediment supply from steep mountain slopes into headwater channels. Alluvial fans often occur where these headwater channels emerge from the mountain areas, and may influence the connectivity of the sediment transport system from the mountain s

A synopsis of climatic and vegetational
✍ Lawrence R. Heaney πŸ“‚ Article πŸ“… 1991 πŸ› Springer 🌐 English βš– 786 KB

Tropical rain forest in Southeast Asia has developed within an extensive archipelago during the past 65 million years or more. During the Miocene (beginning 25 million years BP), rain forest extended much further north (to southern China and Japan); since that time it has contracted. During the Plei

Gully-head morphology and implications f
✍ Wijdenes, Dirk J. Oostwoud; Poesen, Jean; Vandekerckhove, Liesbeth; Nachtergaele πŸ“‚ Article πŸ“… 1999 πŸ› John Wiley and Sons 🌐 English βš– 819 KB

In this paper we examine whether gully-head morphology can be used as an indicator for gully development and, hence, for sediment production. A survey was conducted at five hillslopes in the Sierra de Gata where different types of channel heads occur close to each other. The survey included measurem