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تعداد نتایج: 214

Kenya: A Natural Outlook

Geo-Environmental Resources and Hazards

Publisher: Newnes, 2013-10-22
Pages: 403
Language: en
ISBN_13:9780444595478
ISBN_10:0444595473
Subject: Technology & Engineering

Kenya: A Natural Outlook

Chapter 12. Vegetation

جزئیات و درخواست

By Andreas B. Brink, Catherine Bodart, Graeme Buchanan, Marco Clerici, François Donnay
Publisher: Elsevier Inc. Chapters, 2013-10-22
Pages: 40
Language: en
ISBN_13:9780128083901
ISBN_10:0128083905
Subject: Science

Kenya: A Natural Outlook

Chapter 14. The Importance of Fire Ecology in Protected Area...

جزئیات و درخواست

By Ilaria Palumbo
Publisher: Elsevier Inc. Chapters, 2013-10-22
Pages: 18
Language: en
ISBN_13:9780128083925
ISBN_10:0128083921
Subject: Science

Kenya: A Natural Outlook

Chapter 17. The Management of Wildlife and Fisheries Resourc...

جزئیات و درخواست

By Mordecai O. Ogada, Dorothy Wanja Nyingi
Publisher: Elsevier Inc. Chapters, 2013-10-22
Pages: 25
Language: en
ISBN_13:9780128083956
ISBN_10:0128083956
Subject: Science

Kenya: A Natural Outlook

Chapter 1. General Geology of Kenya

جزئیات و درخواست

By Norbert Opiyo Akech, Christine A. Omuombo, Moses Masibo
Publisher: Elsevier Inc. Chapters, 2013-10-22
Pages: 16
Language: en
ISBN_13:9780128083796
ISBN_10:0128083794
Subject: Science

Kenya: A Natural Outlook

Chapter 20. Overview of Landslide Occurrences in Kenya: Caus...

جزئیات و درخواست

By Charles Maina-Gichaba, Enoch K. Kipseba, Moses Masibo
Publisher: Elsevier Inc. Chapters, 2013-10-22
Pages: 30
Language: en
ISBN_13:9780128083987
ISBN_10:0128083980
Subject: Science

Kenya: A Natural Outlook

Chapter 16. Freshwater Ecology of Kenyan Highlands and Lowla...

جزئیات و درخواست

By Dorothy Wanja Nyingi, Nathan Gichuki, Mordecai O. Ogada
Publisher: Elsevier Inc. Chapters, 2013-10-22
Pages: 27
Language: en
ISBN_13:9780128083949
ISBN_10:0128083948
Subject: Science

Kenya: A Natural Outlook

Chapter 11. Major Soil and Data Types in Kenya

جزئیات و درخواست

By Christian T. Omuto
Publisher: Elsevier Inc. Chapters, 2013-10-22
Pages: 18
Language: en
ISBN_13:9780128083895
ISBN_10:0128083891
Subject: Science

Kenya: A Natural Outlook

Chapter 6. Remote Sensing Application Supporting IWRM in Ken...

جزئیات و درخواست

By John B. Kyalo Kiema
Publisher: Elsevier Inc. Chapters, 2013-10-22
Pages: 23
Language: en
ISBN_13:9780128083840
ISBN_10:0128083840
Subject: Science

Kenya: A Natural Outlook

Chapter 13. Agricultural Expansion and Its Consequences in t...

جزئیات و درخواست

By Petri K.E. Pellikka, Barnaby J.F. Clark, Alemu Gonsamo Gosa, Nina Himberg, Pekka Hurskainen
Publisher: Elsevier Inc. Chapters, 2013-10-22
Pages: 23
Language: en
ISBN_13:9780128083918
ISBN_10:0128083913
Subject: Science

Kenya: A Natural Outlook

Chapter 15. Importance and Dynamics of the Mangroves in Keny...

جزئیات و درخواست

By Bernard K. Kirui
Publisher: Elsevier Inc. Chapters, 2013-10-22
Pages: 12
Language: en
ISBN_13:9780128083932
ISBN_10:012808393X
Subject: Science

Kenya: A Natural Outlook

Chapter 7. Surface Flows for People and Wildlife in the Tran...

جزئیات و درخواست

By Michael E. McClain, Amanda L. Subalusky
Publisher: Elsevier Inc. Chapters, 2013-10-22
Pages: 23
Language: en
ISBN_13:9780128083857
ISBN_10:0128083859
Subject: Science

Kenya: A Natural Outlook

Chapter 9. Coastal Waters

جزئیات و درخواست

By Christine A. Omuombo, Daniel O. Olago, Eric O. Odada
Publisher: Elsevier Inc. Chapters, 2013-10-22
Pages: 13
Language: en
ISBN_13:9780128083871
ISBN_10:0128083875
Subject: Science

Kenya: A Natural Outlook

Chapter 5. Climate

جزئیات و درخواست

By John P.O. Obiero, Japheth O. Onyando
Publisher: Elsevier Inc. Chapters, 2013-10-22
Pages: 19
Language: en
ISBN_13:9780128083833
ISBN_10:0128083832
Subject: Science

Kenya: A Natural Outlook

Chapter 8. Groundwater Distribution and Aquifer Characterist...

$Comprehensive hydrogeological investigations of Kenya as country have been carried out within various geological settings that range from volcanic terrains and associated quaternary sediments, through sedimentary terrains of northern and coastal Kenya to areas underlain by metamorphic rocks. The objective of the study was to establish groundwater occurrence and distribution in country including characterization of the aquifer properties. The aspects considered in this study of groundwater include: underlying geology, aquifer geometry, groundwater levels in the aquifer, groundwater flow and recharge, specific capacity and transmissivity of the aquifer. The study commences with a systematic analysis of over 13,000 borehole data in relation to geomorphological and geological setting from a regional conceptualization to more specific areas with distinct hydrogeological features. The results reveal that the aquifer within the sedimentary terrains (northern Kenya-Kenya coast) stretches over a distance of 740km in NW-SE direction as a continuum all the way from the Marsabit through Garissa and terminates at Lamu within the Kenyan Coast. Merti aquifer is part of this large aquifer system. The estimated average transmissivity indicate that a net flux of some 75,000m3. The main aquifer within the sedimentary setting of southern Kenya include Sabaki aquifer (at Baricho area), Tiwi Aquifer and Msambweni. The aquifer zone is marked by saturated sandy layers within the Kilindini Formation. The total storage in the northern and central parts of the sandy facies of the Kilindini Formation, assuming an effective porosity of 30%, is in the order of 112 million m3. Within the Rift Valley ground water is confined within lacustrine sediments, weathered and/or fractured zones in the volcanic rocks, and sediments interbedded between volcanic rocks. The aquifers within rift valley include: Turkana aquifer, Baringo-Bogoria aquifer, Nakuru aquifer, and Magadi aquifer. In the areas covered by the basement rocks there is no single identified aquifer with significant amount of groundwater. According to the peizometric map, the aquifer within the basement rocks are localized; examples of these aquifers occur around Isiolo, Meru, Embu, Wote and Kitui areas. Under the geological conditions of the Basement terrains, the groundwater occurs in weathered zones above the crystalline Basement rocks, fractured zones within the crystalline bedrock, and alluvial deposits along the main drainage channels.$

جزئیات و درخواست

By Zachariah Kuria
Publisher: Elsevier Inc. Chapters, 2013-10-22
Pages: 30
Language: en
ISBN_13:9780128083864
ISBN_10:0128083867
Subject: Science

Kenya: A Natural Outlook

Chapter 4. Quaternary Evolution

جزئیات و درخواست

By Daniel O. Olago
Publisher: Elsevier Inc. Chapters, 2013-10-22
Pages: 13
Language: en
ISBN_13:9780128083826
ISBN_10:0128083824
Subject: Science

Kenya: A Natural Outlook

Chapter 23. Monitoring Drought with the Combined Drought Ind...

جزئیات و درخواست

By Zoltan Balint, Francis Mutua, Peris Muchiri, Christian T. Omuto
Publisher: Elsevier Inc. Chapters, 2013-10-22
Pages: 24
Language: en
ISBN_13:9780128084014
ISBN_10:0128084014
Subject: Science

Kenya: A Natural Outlook

Chapter 19. Seismic Hazard

$The East African Rift System (EARS) and by extension the Davie Ridge, which is considered as the seaward extension of eastern branch (Kenya Rift Valley) of the East African Rift Valley (), are characterized by divergence whose maximum rate is estimated to be about 7mm/year (). This rate of divergence is somewhat much slower than that found at most active mid-ocean ridges or even the convergence of India–Burma plates or that between the Australian and Sunda plates (). Despite this slow rate of divergence, the East African Rift Valley and the Davie Ridge are characterized by frequent seismicity with large and shallow earthquakes occurring occasionally. Seismic reflection, gravity, and magnetic data from offshore East Africa allow the Davie Fracture Zone to be traced from 11oS to its intersection with the Kenyan coast at 2oS, constraining the relative motion of Madagascar and Africa (). Further, numerous faults and fractures probably associated with the Davie Fracture have been mapped using recent gravity and magnetic data between latitudes 2o21′S and 3o03′S and longitudes 40o08′E and 40o45′E by . Seasat-derived free-air gravity anomalies and slope/rise positive magnetic anomalies observed in shipboard data help to locate the continent–ocean boundaries (COB) off the shore of East Africa and Madagascar. Furthermore, the EARS, and precisely the Kenya Rift Valley, is characterized by ~3-km-thick sediments and normal-faulting mechanism. Deformation has been active along the Kenya Rift Valley as evidenced by high seismic activity. Surface deformation studies from SAR interferometry in the southern sector of the Kenya Rift Valley in Magadi show that it is characterized by 14cm of deformation over 10-km-long stretches (). If the Davie Ridge is an extension of the East African Rift Valley, we cannot rule out the occurrence of tsunami-generating earthquakes, which are bound to have devastating consequences on the eastern coast of Africa. Earthquakes as deep as 40km have been recorded below Davie Ridge (). However, evaluation of recent seismic data shows that magnitude 6.0–7.2 earthquakes at relatively shallow depths of 10–30km are a common occurrence along the Kenya Rift Valley and the Davie Ridge in the Mozambique Channel. The focal mechanism of these earthquakes supports what has previously been proposed that the Davie Ridge is a southward extension of the eastern arm of the EARS. The earthquake focal mechanism indicates that the Davie Ridge is characterized by predominantly normal faulting with occasional oblique faulting. Consequently, Kenya and generally the East African coast are prone to both seismic hazards on land and tsunami-generating earthquakes. This chapter begins with general overview of the seismicity in Kenya from the 1900s to the present. Seismicity in Kenya up to 1963 is mainly based on macroseismic data while that from 1963 to the present is based on data from instrumental recordings. In the past, a number of microseismic and seismicity studies in Kenya have previously been undertaken and the results from these studies are rather disjointed. In this chapter, we have made an attempt to merge all the existing results into one database from which the general seismicity, and subsequently seismic hazard in Kenya has been evaluated. The main goal of this chapter is to bring into focus the area(s) in Kenya more prone to seismic hazards either due to ground shaking occasioned by an earthquake or due to tsunami as a result of earthquakes occurring along the Davie Ridge.$

جزئیات و درخواست

By Josphat K. Mulwa, Fumiaki Kimata, Nguyen Anh Duong
Publisher: Elsevier Inc. Chapters, 2013-10-22
Pages: 36
Language: en
ISBN_13:9780128083970
ISBN_10:0128083972
Subject: Science

Kenya: A Natural Outlook

Chapter 10. Renewable Energy Resources in Kenya

جزئیات و درخواست

By Christopher Oludhe
Publisher: Elsevier Inc. Chapters, 2013-10-22
Pages: 16
Language: en
ISBN_13:9780128083888
ISBN_10:0128083883
Subject: Science

Kenya: A Natural Outlook

Chapter 18. Environmental Impact Assessment in Kenya

جزئیات و درخواست

By Elijah K. Biamah, Jacqueline Kiio, Benjamin Kogo
Publisher: Elsevier Inc. Chapters, 2013-10-22
Pages: 36
Language: en
ISBN_13:9780128083963
ISBN_10:0128083964
Subject: Science

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