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Magmatic continental rifts often constitute the earliest stage of nascent plate boundaries. These extensional tectonic provinces are characterized by ubiquitous normal faulting and volcanic activity; the spatial pattern, the geometry, and the age of these normal faults can help to unravel the spatiotemporal relationships between extensional deformation, magmatism, and long-wavelength crustal deformation of continental rift provinces. This study focuses on the active faulting in the Kenya Rift of the Cenozoic East African Rift System (EARS) with a focus on the mid-Pleistocene to the present-day.
To examine the early stages of continental break-up in the EARS, this thesis presents a time-averaged minimum extension rate for the inner graben of the Northern Kenya Rift (NKR) for the last 0.5 m.y. Using the TanDEM-X digital elevation model, fault-scarp geometries and associated throws are determined across the volcano-tectonic axis of the inner graben of the NKR. By integrating existing geochronology of faulted units with new ⁴⁰Ar/³⁹Ar radioisotopic dates, time-averaged extension rates are calculated. This study reveals that in the inner graben of the NKR, the long-term extension rate based on mid-Pleistocene to recent brittle deformation has minimum values of 1.0 to 1.6 mm yr⁻¹, locally with values up to 2.0 mm yr⁻¹. In light of virtually inactive border faults of the NKR, we show that extension is focused in the region of the active volcano-tectonic axis in the inner graben, thus highlighting the maturing of continental rifting in the NKR.
The phenomenon of focused extension is further investigated with a structural analysis of the youngest volcanic manifestations of the Kenya Rift, their relationship with extensional structures, and their overprint by Holocene faulting. In this context I analyzed the fault characteristics at the ~36 ka old Menengai Caldera and adjacent areas in the Central Kenya Rift using detailed field mapping and a structure-from-motion-based DEM generated from UAV data. In general, the Holocene intra-rift normal faults are dip-slip faults which strike NNE and thus reflect the present-day tectonic stress field; however, inside Menengai caldera persistent magmatic activity and magmatic resurgence overprints these young structures significantly. The caldera is located at the center of an actively extending rift segment and this and the other volcanic edifices of the Kenya Rift may constitute nucleation points of faulting an magmatic extensional processes that ultimately lead into a future stage of magma-assisted rifting.
When viewed at the scale of the entire Kenya Rift the protracted normal faulting in this region compartmentalizes the larger rift depressions, and influences the sedimentology and the hydrology of the intra-rift basins at a scale of less than 100 km. In the present day, most of the fault-bounded sub-basins of the Kenya Rift are hydrologically isolated due to this combination of faulting and magmatic activity that has generated efficient hydrological barriers that maintain these basins as semi-independent geomorphic entities. This isolation, however, was overcome during wetter climatic conditions during the past when the basins were transiently connected. I therefore also investigated the hydrological connectivity of the rift basins during the African Humid Period of the early Holocene, when climate was wetter. With the help of DEM analysis, lake-highstand indicators, radiocarbon dating, and a review of the fossil record, two lake-river-cascades could be identified: one directed southward, and one directed northward. Both cascades connected presently isolated rift basins during the early Holocene via spillovers of lakes and incised river gorges. This hydrological connection fostered the dispersal of aquatic faunas along the rift, and in addition, the water divide between the two river systems represented the only terrestrial dispersal corridor across the Kenya Rift. The reconstruction explains isolated distributions of Nilotic fish species in Kenya Rift lakes and of Guineo-Congolian mammal species in forests east of the Kenya Rift. On longer timescales, repeated episodes of connectivity and isolation must have occurred. To address this problem I participated in research to analyze a sediment drill core from the Koora basin of the Southern Kenya Rift, which provides a paleo-environmental record of the last 1 Ma. Based on this record it can be concluded that at ~400 ka relatively stable environmental conditions were disrupted by tectonic, hydrological, and ecological changes, resulting in increasingly large and frequent fluctuations in water availability, grassland communities, and woody plant cover. The major environmental shifts reflected in the drill core data coincide with phases where volcano-tectonic activity affected the basin. This thesis therefore shows how protracted extensional tectonic processes and the resulting geomorphologic conditions can affect the hydrology, the paleo-environment and the biodiversity of extensional zones in Kenya and elsewhere.
Governments at central and sub-national levels are increasingly pursuing participatory mechanisms in a bid to improve governance and service delivery. This has been largely in the context of decentralization reforms in which central governments transfer (share) political, administrative, fiscal and economic powers and functions to sub-national units. Despite the great international support and advocacy for participatory governance where citizen’s voice plays a key role in decision making of decentralized service delivery, there is a notable dearth of empirical evidence as to the effect of such participation. This is the question this study sought to answer based on a case study of direct citizen participation in Local Authorities (LAs) in Kenya. This is as formally provided for by the Local Authority Service Delivery Action Plan (LASDAP) framework that was established to ensure citizens play a central role in planning and budgeting, implementation and monitoring of locally identified services towards improving livelihoods and reducing poverty. Influence of participation was assessed in terms of how it affected five key determinants of effective service delivery namely: efficient allocation of resources; equity in service delivery; accountability and reduction of corruption; quality of services; and, cost recovery. It finds that the participation of citizens is minimal and the resulting influence on the decentralized service delivery negligible. It concludes that despite the dismal performance of citizen participation, LASDAP has played a key role towards institutionalizing citizen participation that future structures will build on. It recommends that an effective framework of citizen participation should be one that is not directly linked to politicians; one that is founded on a legal framework and where citizens have a legal recourse opportunity; and, one that obliges LA officials both to implement what citizen’s proposals which meet the set criteria as well as to account for their actions in the management of public resources.
Die Empirie des beginnenden 21. Jahrhunderts weist mehr autoritäre Regime aus als am Ende des 20. Jahrhunderts angenommen. Die gegenwärtige Autoritarismusforschung versucht die Fortdauer dieses Regimetyps in Hinblick auf die politischen Institutionen zu erklären – dabei bleiben politische Akteure, die nicht zum Herrschaftszentrum gehören, außen vor.
Das vorliegende Projekt untersucht die Rolle und Funktion politischer Opposition in autoritären Regimen. Es wird davon ausgegangen, dass sich an der Opposition eine signifikante Charakteristik autoritärer Regime manifestiert. Das akteurszentrierte Projekt ist der qualitativ orientierten Politikwissenschaft zuzurechnen und verknüpft das Autoritarismuskonzept von Juan Linz mit klassischen Ansätzen der Oppositionsforschung und macht diese Theorien für die gegenwärtige Autoritarismusforschung nutzbar.
Die eigens entwickelte elitenorientierte Oppositionstypologie wird am Beispiel Kenias im Zeitraum 1990-2005 angewendet. Die Oppositionsgruppen werden im Institutionengefüge autoritärer Regime verortet und ihr politisches Agieren in den Dimensionen Handlungsstatus, Handlungsüberzeugung und Handlungsstrategie analysiert. Unter Beachtung der historisch gewachsenen regionalen und kulturellen Spezifika wird angenommen, dass generelle, Regionen übergreifende Aussagen zur Opposition in autoritären Regimen getroffen werden können: Kein Oppositionstyp kann allein einen Herrschaftswechsel bewirken. Der Wechsel bzw. die Fortdauer der Herrschaft hängt von der Dominanz bestimmter Oppositionstypen im Oppositionsgeflecht sowie der gleichzeitigen Schwäche anderer Oppositionstypen ab.
Durch die konzeptionelle Beschäftigung mit Opposition sowie deren empirische Erschließung soll ein substantieller Beitrag für die notwendige Debatte um autoritäre Regime im 21. Jahrhundert geleistet werden.
Kenia erlangt Anfang der 1960er seine Unabhängigkeit und wird in der Folge von den Präsidenten Kenyatta und später Moi autoritär regiert. Als Konsequenz des internationalen und nationalen Druckes werden 1991 wieder Mehrparteienwahlen zugelassen. Die Hoffnungen auf einen Trendwechsel werden zunächst aber nicht erfüllt. Präsident Moi bleibt bei den Wahlen 1992 und 1997 siegreich und versucht jeden möglichen Reformprozess aufzuhalten bzw. zu verlangsamen. Mit dem neu gewählten Präsidenten Kibaki entsteht 2002 die Hoffnung auf Veränderung. Aber als alter Wegbegleiter Mois erfüllt Kibaki nicht die internationalen und nationalen Erwartungen. Moi und Kibaki organisieren jeweils kontra-demokratische Eliten hinter sich und nutzen das mächtige Präsidentenamt, die stärkste Institution im politischen System Kenias, um den Status quo so lange wie möglich zu erhalten. Die Parteien werden weder durch die Regierung noch durch die Opposition zu starken Institutionen transformiert und das unstete Verhalten der Geberländer vermag den Einfluss der autoritären Führung nicht dauerhaft einzuschränken.