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PHYSICAL CHARACTERISTICS
Location and size
Abelenkpe Zonal Council has a total land space of 385km sq and occupies about 3.0 % of the Ayawaso West Land Area. It is located on Longitude 05°35'N and on Latitude 00°06'W. It is bordered in the North by La NkwantanangMadina Municipal Assembly, North East by Adentan Municipal Assembly, East by Ledzokuku Municipal Assembly, South East by La Dade Kotopon, South with Ayawaso North Municipal Assembly, South West with Accra Metropolitan Assembly, West with Okaikwei North Municipal Assembly and in the North West by Ga East Municipal Assembly. Figure 1.2 shows the location of the Municipality in the National and Regional context.
Geological Structure
AWMA consists of mixed quartzite sands, garnet, Hornblende Gneiss. The Garnet and Hornblende Gneiss can be found around the western part of the Municipality and the mixed quartzite and sandnit can be found in the mid portion of the Municipality.
The soil in the Municipality can be divided into four main groups; drift materials resulting from deposits by windblown erosion; alluvial and marine mottled clay of comparatively recent origin derived from underlying shales; residual clay and gravels derived from Accrarian sandstone bedrock. In many low lying poorly drained areas, pockets of alluvial ‘black cotton’ sand are found. These soils have a heavy organic content; they expand and contract readily causing major problems on building foundations and footings. In some areas lateritic soils which are strongly acidic abound. These soils when saturated are compact but pose a threat to concrete foundations causing honey-combing.
Precipitation Climate and Drainage
AWMA lies in the Savanna Zone with annual average rainfall of about 800-900mm within the two rainy seasons; May-mid-July and mid-August -October. However due to recent climate variability there are sometimes variation from the major raining seasons with dry months of December experiencing rainfall. There is very little variation in temperature throughout the year. The mean monthly temperature ranges from 24.7C in August (the coolest) to 28.C in March (the hottest) with the annual coverage of 26.C. As the area is close to the equator, the daylight hours are practically uniform throughout the year. Relative humidity is generally high varying from 65% in the mid- afternoon to 95% at night.
Vegetation
There is evidence to suggest that the vegetation of the Municipality has been altered in the past century by climate and the other human factors. Much of the Municipality was believed to have been covered by dense forest of which only a few remnant trees survive. Climate change combined with rapid urbanization has imposed vegetation structures similar to those of the Southern sahael.
Abelenkpe Zonal Council has a total land space of 385km sq and occupies about 3.0 % of the Ayawaso West Land Area. It is located on Longitude 05°35'N and on Latitude 00°06'W. It is bordered in the North by La NkwantanangMadina Municipal Assembly, North East by Adentan Municipal Assembly, East by Ledzokuku Municipal Assembly, South East by La Dade Kotopon, South with Ayawaso North Municipal Assembly, South West with Accra Metropolitan Assembly, West with Okaikwei North Municipal Assembly and in the North West by Ga East Municipal Assembly. Figure 1.2 shows the location of the Municipality in the National and Regional context.
Geological Structure
AWMA consists of mixed quartzite sands, garnet, Hornblende Gneiss. The Garnet and Hornblende Gneiss can be found around the western part of the Municipality and the mixed quartzite and sandnit can be found in the mid portion of the Municipality.
The soil in the Municipality can be divided into four main groups; drift materials resulting from deposits by windblown erosion; alluvial and marine mottled clay of comparatively recent origin derived from underlying shales; residual clay and gravels derived from Accrarian sandstone bedrock. In many low lying poorly drained areas, pockets of alluvial ‘black cotton’ sand are found. These soils have a heavy organic content; they expand and contract readily causing major problems on building foundations and footings. In some areas lateritic soils which are strongly acidic abound. These soils when saturated are compact but pose a threat to concrete foundations causing honey-combing.
Precipitation Climate and Drainage
AWMA lies in the Savanna Zone with annual average rainfall of about 800-900mm within the two rainy seasons; May-mid-July and mid-August -October. However due to recent climate variability there are sometimes variation from the major raining seasons with dry months of December experiencing rainfall. There is very little variation in temperature throughout the year. The mean monthly temperature ranges from 24.7C in August (the coolest) to 28.C in March (the hottest) with the annual coverage of 26.C. As the area is close to the equator, the daylight hours are practically uniform throughout the year. Relative humidity is generally high varying from 65% in the mid- afternoon to 95% at night.
Vegetation
There is evidence to suggest that the vegetation of the Municipality has been altered in the past century by climate and the other human factors. Much of the Municipality was believed to have been covered by dense forest of which only a few remnant trees survive. Climate change combined with rapid urbanization has imposed vegetation structures similar to those of the Southern sahael.
Date Created : 11/12/2025 12:00:00 AM
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