The Geology of Southern Akor and Its Environment

 

Table Of Contents


Chapter ONE

INTRODUCTION

  • 1.1Introduction
  • 1.2Background of Study
  • 1.3Problem Statement
  • 1.4Objectives of the Study
  • 1.5Limitations of the Study
  • 1.6Scope of the Study
  • 1.7Significance of the Study
  • 1.8Structure of the Research
  • 1.9Definition of Terms

Chapter TWO

LITERATURE REVIEW

  • 2.1Overview of Geology
  • 2.2Historical Perspective
  • 2.3Geological Formations in Southern Akor
  • 2.4Environmental Factors Affecting Geology
  • 2.5Geology and Natural Resources
  • 2.6Impact of Human Activities on Geology
  • 2.7Geology and Climate Change
  • 2.8Geology and Biodiversity
  • 2.9Technological Advances in Geology
  • 2.10Future Trends in Geology

Chapter THREE

RESEARCH METHODOLOGY

  • 3.1Research Methodology Overview
  • 3.2Data Collection Methods
  • 3.3Sampling Techniques
  • 3.4Data Analysis Procedures
  • 3.5Research Design
  • 3.6Research Instruments
  • 3.7Ethical Considerations
  • 3.8Validity and Reliability

Chapter FOUR

DATA PRESENTATION AND ANALYSIS

  • 4.1Geological Survey Findings
  • 4.2Environmental Impact Analysis
  • 4.3Comparison with Previous Studies
  • 4.4Statistical Analysis of Data
  • 4.5Interpretation of Results
  • 4.6Discussion of Findings
  • 4.7Implications for Geology
  • 4.8Recommendations for Future Research

Chapter FIVE

SUMMARY, CONCLUSION AND RECOMMENDATIONS

  • 5.1Summary of Findings
  • 5.2Conclusions
  • 5.3Contributions to the Field
  • 5.4Practical Applications
  • 5.5Limitations of the Study
  • 5.6Recommendations for Future Studies
  • 5.7Conclusion

Project Abstract

The study area is located within latitude 050 271 4611N and longitude 0080 431 46E, and the elevation of the place is 156m. The major rock types encountered in the area include gneisses, quartzite, amphibolites and marbles. These are intruded by pegmatite, quartz vein and aplite. The latest metamorphic episode occurred during the Pan-African Orogeny (600 ± 15ma) and the deformation left a structural trend of NS and NE-SW on the rocks. The occurrence of NW-SE structural trend are also shown on some rocks indicating that the Pan-African event did not completely alter earlier structural imprints. The study area is highly forested, undulating in slope and is a characteristic of a tropical rain forest in the area.

Project Overview

IntroductionThe geology of southern Akor and its environs lies within the Oban Massif, a component of the crystalline basement of Nigeria. The Nigeria crystalline basement in turn forms a part of the African crystalline basement and covers over 50% of the total land surface of Nigeria . The rock assemblages encountered and identified consists of mainly schists, gneisses, Amphibolite, Charnockite, Marble and Quartzites and pegmatite, Quartz vein and Aplite emerging as Igneous intrusive rocks. The area mapped and studied (Akor) is predominated by intrusive rocks and these rocks are very well exposed where the topographyis slopy along streams and river channels.
Ekwueme et al (1992) proposed that charnockite rock’s occur in both the eastern and western Oban Massif. The rocks occur as large coarse-grained, rounded and, massive bodies deformed together with the bounded gneisses. Ekwueme (1992) has shown that the diorities and charnockite are similar in composition and that the former may be retrogressive product of the latter.The occurrences of weathering and tectonic activities were observed to have greatly affected the exposed outcrop and such effects from wet season had deformed these outcrops to boulders with reference to their shapes and sizes.1.1 Location and accessibilityThe area is located in the Eastern part of Akamkpa local Government area of theCross River State of Nigeria. It covers an estimated area of about 85sq.KM and constitutes part of the Oban Massif of the South-eastern Nigeria. The map area is largely made up of Ntebachot Akor. New Ntebeji and Ayip Eku all located in Akamkpa Local Government area of Cross River state.About 90 percent of the area is inaccessible due to thick vegetation, steep valleys and hilly terrains. The only access road across the area is the Calabar-Ekang Road while hunters tracks provide minimal access into the area.

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