• Effects Of Global Warming

  • CHAPTER ONE -- [Total Page(s) 7]

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    • 1.6.4  Vegetation
      Abraka is located on the equatorial rainforest which is evergreen forest and consist of three canopies of trees which are, the upper layer of which is about 60m tall, middle layer which is about 40m tall and the lower layer which is about 30m in height. The three major vegetation types in Abraka includes; the tropical rainforest belt, temperate grasslands and the grassland vegetation remains one of the key important factor which affect the climate of Abraka Region. Vegetation provides lumbering, medicinal purpose of Abraka region. The high amount of rainfall in Abraka aids the cultivation of crops like cassava and maize within the region. The influence of man has reduced the forest mainly to secondary growth (deciduous vegetation) due to agricultural practices and growing of various cash and food crops. This has in turn prone the environment direct sunlight which has resulted to intensive heating of the environment causing global warning due to lack of trees to act as shade and wind break.
                The implication of these is that human activities have reduced the vegetation of Abraka to a secondary re-growth thereby exposing the environment to hazards such as intense temperature rise, flooding erosion, etc. which have in turn affected the inhabitants of Abraka through global warming effects.
      1.6.5  Geology and Soils
      Abraka is predominantly underlying sedimentary rock. Abraka lies in southern most sedimentary rock. Abraka lies in southern most sedimentary basis in Nigeria.
                Abraka soil is acidic in nature. Abraka soil varies from coarse through medium to fine grained soils. The soils of Abraka can be said to be sandy loam. The colour of the soil is greenish brown to reddish brown and then to brown. The light grayish colouration characterizes the entire sandy portion of the soil, while the reddish brown colouration depicts the presence of ion oxide in the soil. This colouration depicts the availability of mineral matters and moisture. Abraka soil is poorly structured in relation to its type in terms of grain size, pore spaces which greatly influences the rate of percolation and capillarity, aeration and the rate of evaporation.
                The implication of these is that human activities have exposed the soil to erosional activates and flooding making the soil inferity for agricultural acuities, etc. which have in turn affected the inhabitants of Abraka region who rely on farming for their source of livelihood.

  • CHAPTER ONE -- [Total Page(s) 7]

    Page 4 of 7

    Previous   1 2 3 4 5 6 7    Next