Africa - Mediterranean Vegetation

Africa

Table of Contents

Introduction
Geologic history
- General considerations
- Rock types and structural evolution
  - The Precambrian
  - The Paleozoic Era
  - The Mesozoic Era
    - Marine formations
    - Continental formations
  - The Cenozoic Era
    - Marine formations
    - Continental formations
    - Tectonic movements
    - Formation of the Red Sea
    - Volcanism and rifting
    - Pleistocene and Holocene developments
Land
- Relief
- Drainage
  - Nile basin
  - Niger basin
  - Congo basin
  - Zambezi basin
  - Orange basin
  - Chad basin
- Soils
  - Soil types
    - Desert soils
    - Chestnut-brown soils
    - Chernozem-like and black soils
    - Red tropical soils and laterites
    - Mediterranean soils
  - Soil problems
- Climate
  - Factors influencing the African climate
  - Climatic regions
- Plant life
  - Ecological relationships
  - Vegetational zones
    - Lowland rainforest
    - Eastern African forest and bush
    - Mangrove swamp
    - Broad-leaved woodland and grassland
    - Thorn woodland, grassland, and semidesert vegetation
    - Afromontane vegetation
    - Desert vegetation
    - Karoo-Namib shrubland
    - Highveld grassland
    - Mediterranean vegetation
    - Cape shrub, bush, and thicket
    - Madagascar
    - Sudd
  - Long-term changes in vegetation
    - Geologic influences
    - Climatic influences
    - Human influences
    - Conserving the vegetation
- Animal life
  - Genera and distribution
    - Mammals
    - Birds
    - Reptiles and amphibians
    - Arthropods
    - Aquatic life
    - Origin and adaption of African fauna
  - The effects of humans
  - Ecology
    - Animal life of particular interest
    - Conservation
    - Animals affecting land usage
People
- Culture areas
  - Northern Africa
  - Western Africa
  - West-central Africa
  - Eastern Africa
  - Central and Southern Africa
  - Madagascar
- Cultural patterns
  - Languages
  - Religions
  - Domestic groupings
- Demographic patterns
  - Population distribution
  - Settlement patterns
  - Migrations
Economy
- Resources
  - Mineral resources
    - Metallic deposits
    - Nonmetallic deposits
  - Water resources
    - Surface water
    - Groundwater
    - Availability for human use
  - Biological resources
    - Botanical resources
    - Animal resources
- Agriculture
  - Principal crops
    - Cereals and grains
    - Legumes and fodder
    - Tubers and root crops
    - Fruits and vegetables
    - Beverage crops
    - Fibres
    - Other cash crops
  - Livestock and fishing
- Industry
- Power
- Trade
  - Internal trade
  - External trade
    - Exports
    - Imports
- Transportation
  - Animal transport
  - Motor transport
  - Rail transport
  - Air transport
  - Navigation

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This zone is determined chiefly by its climate, which is characterized by very dry summers and mild, rainy winters, but it has long been much differentiated by its inhabitants. Large tracts have been degraded into maquis (macchie), garigue, or dry semidesert (steppe) vegetation. Maquis consists of dense scrub growths of xerophytic (drought-resistant) and sclerophyllous (leathery) shrubs and small trees, which are often fire-resistant. Garigue characteristically is found on limestone soils and has more woody growth, including evergreen and cork oaks (Quercus suber). The higher slopes of the Atlas Mountains once carried large stands of pine and cedar, but they have ...(100 of 32999 words)

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