By M. Koïta, H. Jourde (auth.), Nicolaos Lambrakis, George Stournaras, Konstantina Katsanou (eds.)
The booklet specializes in the administration of the aquatic setting. it's aimed toward scientists, scholars, governmental officers and experts facing groundwater and surroundings. Its major aim is to notify the reader of rules, wisdom and adventure by way of a sustainable aquatic setting. the most issues are as follows: Water our bodies and Ecosystems; weather switch and Water our bodies; Water caliber and agriculture; interplay of floor and floor waters; Karst Hydrogeology; non-stop Media Hydrogeology; Fissured Rocks Hydrogeology; Hydrochemistry; Geothermics and thermal waters; The position of water in building tasks; Hydrology
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Additional info for Advances in the Research of Aquatic Environment: Volume 2
Oladele subsurface material (Kelly 1976). The study area is situated at Gbagada, near the coastline of Lagos (Fig 1). 5x10-4. Adepelumi et al (2008) mapped the intrusion of sea water into coaster aquifer of Lagos using VES technique of Direct Current (DC) resistivity method. Longe et al. (1987) revealed multilayered aquifer system for the metropolis in their study of the hydrogeology of Lagos. The present work is concerned with groundwater exploration through delineation of aquifer geometry using Vertical Electrical Soundings (VES) results to give a tangible solution to the demand for exploitation of water resources for sustainable economic growth in the heavily populated area of Lagos.
These “pipe rocks”, common in many Cambrian and Ordovician siliciclastic successions, are also known as “Tigillites”. In the upper Dibsiyah, thickness of Skolithos pipe rocks varies between some 10 centimeters to several meters. Simple Skolithos burrows are often associated with larger burrows attributed to “Bergaueria” sp. The 24 H. Al Ajmi et al. almost “reef-like” horizons of Skolithos and/or Bergaueria are up to 13 meters thick. Most of the internal sedimentary structures have been destroyed by burrowing; however, the primary cross-bedding is often faintly visible.
Clast- and matrix-supported conglomerates and coarse conglomeratic sandstones represent the basal channel-fill facies association (Keller et al. 2011). They are interpreted as coarse glacial outwash sediment near melt water outlets. A facies association of massive to cross-bedded sandstones, arranged in clinoforms, fills up the upper part of the valleys. These sediments are interpreted as Gilberttype deltas prograding from sandur plains into the water-filled valleys during glacier retreat. Together with glacial striations, striated clasts, and similar corresponding features, these sediments indicate a glacial origin of this part of the Wajid Sandstone (Keller et al.
Advances in the Research of Aquatic Environment: Volume 2 by M. Koïta, H. Jourde (auth.), Nicolaos Lambrakis, George Stournaras, Konstantina Katsanou (eds.)