Abstract

Anthropogenic activities have exacerbated the incidences of floods, soil and gully erosion and landslides in parts of southeastern states of Anambra and Imo, Nigeria. Intense urbanization, deforestation, agricultural, commercial/industrial activities has extensively-denudated and elluviated the total environment. The variations in climatic condition also have associated implications. The rainy season registers an average annual rainfall of 2000 mm. The Geology comprises an unstable platform of a regional escarpment/cuesta subtended by sandy, highly-fractured and faulted Nanka sands/Ameki Formation. The underlying unstable geology facilitates the development of gullies with depth ranging from 2 m to over 80 m. The calculated rate of soil removal from the gully prone areas is about 9.20 to 10.16 ton/ha/yr. The significant cuesta of the area with steep scarp slope and gentle dip slope forms both surface and groundwater divide that also facilitates gully and landslide developments. The underlying geologic sandy structure is quite porous and permeable with huge aquiferous horizons of high pore-water pressures and effective stress. The problems of laissez faire attitude and poor understanding of the destructive implications of the unstable regional geologic platform result in the failure of measures to prevent myriads of environmental destructions and economic wastes.

Highlights

  • Geological Sciences or Earth Sciences or Applied Geology is keyed towards fully-understanding the constituents and geotechnical intricacies of the earthly environment and being able to use the realized knowledge to control any arising problems and implications in anthropogenic activities

  • The escarpment consists of the steep east scarp slope and the gentle west dip slope

  • The gully problems are more on the scarp slope than on the dip slope

Read more

Summary

Introduction

Geological Sciences or Earth Sciences or Applied Geology is keyed towards fully-understanding the constituents and geotechnical intricacies of the earthly environment and being able to use the realized knowledge to control any arising problems and implications in anthropogenic activities. The gully problems are more on the scarp slope than on the dip slope. Sites at Agulu, Adazi Ani, Nanka, Oko, Ekwulobia, Uga, Umuchu etc are along the scarp slope while the dip slope hosts the gully sites of Adazi, Alor, Oraukwu, Nnobi, Abatete and Ideani. Major rivers such as Mamu, Uchu, Idemili, Odo and Orashi emanate from both the scarp and dip slopes of the escarpment. The rivers form eroding agents wreaking havoc on the unconsolidated geologic unit of the area

Objectives
Methods
Discussion
Conclusion
Full Text
Published version (Free)

Talk to us

Join us for a 30 min session where you can share your feedback and ask us any queries you have

Schedule a call