The present study presents preliminary investigation on the physico-chemical and bacteriological parameters of surface water samples collected, during the wet and dry seasons, from streams in Orem and environs, a typical Basement terrain in southeastern Nigeria. The intension was to evaluate the suitability of the water for domestic and agricultural uses. Results generally indicate normal water temperature, especially for the tropic; pH reflecting slightly acidic conditions; low EC and water hardness which respectively qualifies the water as excellent and soft; turbidity values that points to the water as a possible sources of water-borne diseases; DO values that are reasonable, to support good fish production, throughout the year; low levels of nutrients and heavy metals that pose no detrimental effect for the aquatic ecosystem; and low Salinity and Total Dissolved Solids (TDS) that reflects water of low mineralization. The major dissolved cations points to a possible geogenic source for the major ions, while the anion levels supports agricultural and anthropogenic pollutions. Values recorded during the dry season were frequently higher than those recorded during the wet season, possibly reflecting dilution and evaporation effects during the wet and dry seasons, respectively. With minor exceptions, the levels of almost all the tested parameters were within the respective permissible limits of the Nigerian standards for drinking water quality (NSDWQ). Among the exceptions in this regards, is the unacceptable and alarmingly high volume of bacteriological inputs recorded for the waters. Clearly, this renders the water unfit for consumption and various other usage, in its present form. ' E -8°50' E of the Greenwich meridian, and latitude 5°28' N -5°33 ' N of the equator. The relief of the area can best be classified as an elevated or high land. In terms of climate, the area

Barite occurrences in the Calabar Flank, Oban massif, Mamfe Embayment and Obudu Plateau of Southeastern Nigeria have been sampled and analyzed for the purpose of assessing their chemical composition and industrial quality. Barite occurrences were observed mostly along faults and unconformities marking the boundaries between the Precambrian basement rocks of Oban and Obudu massifs and the Cretaceous sediments of the Calabar Flank and Mamfe embayment. Occurrences were also observed within the sediments. The chemical data show that BaSO 4 , SiO 2 and TiO 2 are the major chemical species of the barite. The Ba and SO 4 content vary between 53.62 -56.10 wt% and 27.57 -39.35 wt% respectively across the sampled areas. The specific gravity is 4.45 and this combined with high BaSO 4 (approximately 94 wt%) shows that the mineralization is of high industrial quality and compares favourably with the Azara barite deposits of the Benue Trough. The quality of the barite meets American Petroleum institute (API) requirements for use as drilling mud.

This research presents a review on water resources in Delta state, southern part of Nigeria, with emphasis on hydrogeochemical and microbial assessment. It also evaluate factors responsible for water contamination, and their resulting health problems within the study area. To achieve the objective of this study, related articles were downloaded from Google, published article on influence of hydrogeochemical and microbial activities on water resources, these articles were thoroughly studied. Findings from this study revealed that groundwater was more studied than surface water. It was observed that groundwater within the riverine communities are much more prone to pollution when compared to groundwater in upland area. From reviewed article, it was observed that, larger percentage of groundwater showed presence of coliform. Study from reviewed article further suggested that hydrogeochemical processes such as rock water interaction, saltwater intrusion and precipitation influences groundwater quality within the study area especially within Sombreiro-Warri Deltaic Plain Deposit.

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Different rock types from the area northeast of Obudu, southeastern Nigeria were investigated in order to place constraints on their metamorphic conditions. Detailed petrographic studies indicate four main rock groups in the studied area, namely migmatitic gneiss, migmatitic schist, granite gneiss and a minor amount of amphibolite, metagabbro and dolerite. The chemistry of minerals in these rocks is used to estimate metamorphic pressure and temperature (P-T) using appropriate geothermometers and geobarometers. The estimated temperature for migmatitic gneiss of the area is 600-625 °C and 600-650 °C for migmatitic schist; the pressure is ~ 8 kbar. For amphibolite the temperature is ~600-700 °C and pressure is 8-12 kbar. The estimated pressures and temperatures for the northeast Obudu rocks correspond to upper amphibolite to lower granulite facies metamorphism. The metamorphism occurred due to continent-continent collision during the Pan-African orogeny, most likely during the D1 deformational phase of the area. The recorded high pressures possibly resulted from crustal thickening in the area. P-T conditions for Pan-African orogeny in northeast Obudu area are in good agreement with P-T estimations for the Pan-African event in adjacent areas.