The role of public involvement in wildlife‐livestock conflicts: The case of Narok ranchers in Kenya
Abstract Economic activity associated with wildlife is an important source of foreign exchange in Kenya. Not surprisingly, the needs and interests of those involved in this sector are given due consideration. The exception is the farmers and ranchers who live among the wildlife and whose cooperation is necessary for maintaining this resource. As a result, farmers and ranchers have developed increasingly negative attitudes toward wildlife. On the basis of field study data collected in the Narok District of Kenya, the article argues that ranchers have in the past derived traditional and economic uses from wildlife and that their acquired negative attitude is a result of their exclusion from involvement in the design and planning of wildlife projects and policies. Four strategies for dealing with this potential conflict and incorporating ranchers and farmers into the wildlife economic sector are discussed: (1) involving the ranchers in planning and implementing wildlife projects, (2) strengthening wildlife e...
Towards promotion of local tourism: A case study of the Kenya Wildlife Service outreach program
Introduction Wildlife is Kenya's foremost natural resource and defines the base of Kenya's tourism industry. A state agency, the Kenya Wildlife Service (KWS) is responsible for wildlife management in the country. A major criticism against Kenya's tourism industry has been that its facilities and services are geared towards meeting the interests of foreigners at the expense of locals. Ordinary Kenyans including communities neighboring its wildlife protected areas have, with time, developed the feeling that recreational wildlife viewing is for foreigners and a few rich Kenyans, but not for the common man. Fredrick Nyongesa Kassilly
Mesozoic rifting and basin inversion along the northern African Tethyan margin: an overview
Abstract The northern African Tethyan margin registered three major rifting episodes from the latest Palaeozoic-earliest Mesozoic to the earliest Cenozoic. Break-up of Gondwana was initiated in the late Carboniferous. Along the northern African-Arabian plate margin rifting propagated westward from the northeastern Arabian margin to Morocco during the Permian and Triassic, and was accompanied by Mid-Late Triassic-earliest Liassic extensive alkaline flow basalts. Rifting continued during the Liassic, e.g. in the Moghrebian Atlas troughs. A second stage of rifting occurred in the Late Jurassic and continued into, or was rejuvenated during, the Early Cretaceous. Along the east Mediterranean margin, some large E-W trending rifts formed, often with associated volcanism, e.g. southern Sirt and Abu Gharadig. Most researchers believe the oceanization of the eastern Mediterranean basin occurred at this time. Flexural subsidence affected the Moghrebian Atlas, including the Riffian-Tellian domain, where a thick flysch series was deposited. Two short-lived, but widespread and tectonically important, compressional or wrench-dominated events occurred during the Santonian and the latest Maastrichtian. From Morocco to Oman, most sedimentary basins were folded and inverted at these times. The Santonian event resulted from onset of the collision between the African-Arabian and Eurasian plates. New stress-fields favoured NE-SW extension along the African plate margin, generating or rejuvenating some rifts, e.g. in the Euphrates trough and in the Libya-Tunisia region (northwestern Sirt, Pelagian Sea). Rifting and magmatism continued in these regions into the Paleocene. During the Mesozoic, therefore, the northern margin of the African-Arabian plate registered both rifting resulting in the oceanization of the Tethys and rifting resulting from the initiation of the closure of the Tethys. The intraplate domain exhibited echoes of the tectonic events affecting the margin.