Book contents
- Frontmatter
- Contents
- Preface
- Part I The Tropical Environment
- Part II Process geomorphology in the tropics
- 5 Weathering in the tropics
- 6 Slopes: forms and processes
- 7 Rivers in the tropics
- 8 Alluvial valleys
- 9 Large rivers in the tropics
- 10 The tropical coasts
- 11 Deltas in the tropics
- 12 The arid tropics
- 13 Tropical highlands
- 14 Volcanic landforms
- 15 Tropical karst
- 16 Quaternary in the tropics
- Part III Anthropogenic changes
- References
- Index
- Plate section
13 - Tropical highlands
from Part II - Process geomorphology in the tropics
Published online by Cambridge University Press: 05 February 2012
- Frontmatter
- Contents
- Preface
- Part I The Tropical Environment
- Part II Process geomorphology in the tropics
- 5 Weathering in the tropics
- 6 Slopes: forms and processes
- 7 Rivers in the tropics
- 8 Alluvial valleys
- 9 Large rivers in the tropics
- 10 The tropical coasts
- 11 Deltas in the tropics
- 12 The arid tropics
- 13 Tropical highlands
- 14 Volcanic landforms
- 15 Tropical karst
- 16 Quaternary in the tropics
- Part III Anthropogenic changes
- References
- Index
- Plate section
Summary
Towards the north is the Himalaya, the lord of the mountains, the abode of the gods.
Kalidasa, translated from SanskritImportance of highlands
Highlands are geomorphologically important regions. A large part of a river’s discharge and nearly all of its sediment may come from mountainous areas. These elevated areas also impact on the regional climate, especially precipitation. Precipitation arrives as snow at high altitudes, even in the tropics, and as rain on the lower windward slopes. Such precipitation can be very high in a tropical storm or when winds converge near the Inter Tropical Convergence Zone (ITCZ). Highlands may therefore supply a large proportion of a river’s discharge.
- Type
- Chapter
- Information
- Tropical Geomorphology , pp. 232 - 253Publisher: Cambridge University PressPrint publication year: 2011