Browsing Faculty of Science & Technology (FST) by Title
Now showing items 1858-1877 of 4028
-
Geology and obsidian sources around Naivasha area, Kenya.
(School of Biological Sciences, University of Nairobi, 1994)The study examines in detail an area between Mount Longonot in the east tthrough Lake Naivasha Basin to Mount Eburru in the west. The result is a model of major occurrences of obsidian quarry sources that may have been ... -
The Geology And Palaeogeomorphology Of The Northeast Winam Gulf
(Department of Geology, 1981)A survey of the geology, tectonics -and structural setting of an area of about 880 square kilometres in the northeast portion of the Nyanza rift valley is presented as primary data in understanding the palaeolandscape ... -
The geology of Ishiara area
(Department of Geology, University of Nairobi, 1981) -
Geology of the Ishiara area, Embu/Meru districts, Kenya.
(University of Nairobi.Department of Geology, 1988) -
The geology of the Kavirondian group of sediments
(University of Nairobi, 1991)The Kavirondian sediments form the Kavirondian Group and are exposed both in Kakamega and South Nyanza Districts in western Kenya. This lithological Group forms one of the three stratigraphical Groups which constitute ... -
The geology of the massive sulphide mineralization of the wire hills area, Kenya
(University of NairobiFaculty of Science, 1989)A study of Lhe Wire hills area and i Is relaliwiship to the massive sulphide deposit associated with iL is presenLed. The geology of the through dacites to Lop. Cherts and with these rocks. The study of drill coxes has ... -
The geology of the southern part of Homa mountain carbonatitic complex Western Kenya,with particular reference to the petrology of the alkaline silicate ,metasomatic and melilite bearing suites
(University of NairobiCollege of Biological and Physical Sciences, 1968-03) -
Geology, geochemistry and economic potential of the bingo carbonatite and its associated Laterites in Beni territory, North Kivu, democratic republic of Congo (DRC)
(University of Nairobi, 2018)The Bingo carbonatite complex and its surrounding geologic formations which are located in Beni, North Kivu in the Eastern part of the Democratic Republic of Congo, occur along the Western branch of the East African Rift ... -
Geomagnetic Micropulsations Observed at Kampala
(University of NairobiSchool of mathematics,, 1968)Geomagnetic micropulsations of the types Pc3, Pc4 and Pi have been observed at Makerere. The diurnal variations at: occurrence and period of these pulsations, for the year 1966, have been examined, and a brief polarization ... -
Geometry and lithology of the subsurface responsible for collapsing of boreholes in Olobanita well-field, Kenya- Rift
(University of NairobiGeology, 2011)This project describes the analysis carried out in the Olobanita well-field, Nakuru county, Kenya, using geophysical surveys and geologic logs with an aim of investigating the geometry and lithology responsible for ... -
Geometry of Elliptic Curves and Elliptic Integrals
(University of Nairobi, 2019) -
The Geometry, Hydro-geochemistry and Vulnerability of Aquifers to Pollution in Urban and Rural Settings- a Case Study of Kisumu and Mt. Elgon Aquifers
(University of Nairobi, 2021)Kenya is one of the countries in sub-Saharan Africa considered to have water scarcity, and the national per capita water is below 1,000 cubic meters. The estimated per capita by the Kenya government in 2005 was about 647 ... -
Geomorphology and sedimentology of the implications to coastal zone management Mombasa - Diani area
(Department of Geology, University of Nairobi, 1992)The overall objective of this thesis was to identify coastal zone management problems within Mombasa— Diani area. The study of sedimentological processes and geomorphic features have been used to solve these problems. Other ... -
Geophysical and hydrogeological investigations for groundwater in the lake Kenyatta settlement scheme, Lamu district, coast province, Kenya.
(Department of Geology, University of Nairobi, 1993)This thesis presents results of geophysical and hydrogeological investigations for groundwater' in the Lake Kenyatta settlement scheme: Lamu District, Coast Province: Kenya. During the Pleistocene; the area was a beach ... -
Geophysical characterization of the lithology and structure of the Olobanita Well Field, Lower Lake Baringo Basin, Kenya Rift: Implication on Groundwater occurrence
(University of NairobiGeology, 2010)The task of the research project is the use of geophysical technologies for the characterization of the lithology and structure beneath the Olobanita well field, and determine their implications on the groundwater drilling ... -
Geophysical mapping of buried river channels and other shallow structures recharging major aquifers in the lake Nakuru basin, Kenya rift: case study from Kabatini aquifer.
(University of NairobiGeology, 2010)The project covered the geophysical mapping of buried river channels and other shallow structures recharging major aquifers in the upper Nakuru basin of Kenya rift and in particular the Kabatini area. The project aimed ... -
Geophysical mapping of geological structures as potential Site for gold mineralization at golden pride nzega greenstone Belt tabora south of lake victoria tanzania
(University of Nairobi, 2013)The study area is located southeast of Lake Victoria in Nzega greenstone belt Tanzania. It represents inferred late Archean orogenic gold deposits and is hosted in intensely deformed metasedimentary rocks. Nzega greenstone ... -
Geophysical mapping of shallow structures controlling geothermal reservoir recharge in Eburru geothermal field, Kenya Rift
(University of Nairobi, 2016-11)Eburru Geothermal Field, herein referred to as the study area, that lies in the Kenya rift has been geophysically investigated. The aim of the research was to delineate shallow geological structures beneath Eburru geothermal ... -
Geophysical mapping of structures in Anza Basin, Northern Kenya
(University of NairobiGeology, 2012)The study area is located at the Anza basin. It lies between latitudes of 380 05/ E& 380 25/ E and longitudes of 20 00/ N & 20 21/ N and covered an area of 1,687.5 km2. The area is important due to its thick sedimentary ...