Der vorliegende Text versucht, das in der Humboldt-Forschung weithin bekannte und gut erforschte Thema „Humboldt und die Sklaverei“ biographisch neu einzuordnen und orientiert sich dabei an folgender These: Humboldt durchläuft in den Jahrzehnten nach Beginn seiner Reise durch die amerikanischen Tropen (1799–1804) verschiedene Phasen in der Beschäftigung mit dem Thema Sklaverei. Im Laufe dieser Phasen, die keineswegs einer chronologischen Ordnung folgen, sondern zum Teil parallel verlaufen, nimmt Humboldt verschiedene soziale Rollen an, die ihren Ausdruck in spezifischen Haltungen und Handlungen finden. In ihrer Summe zeichnen sie ein für das Verständnis von Humboldts Persönlichkeit typisches Psychogramm: ein selbstbewusster Moralist, ein rigoroser, beinahe kriminalistisch agierender Wissenschaftler, ein politisch zurückhaltender Akteur.
The 12 January 2010 M-w 7.0 Haiti earthquake occurred in a complex deformation zone at the boundary between the North American and Caribbean plates. Combined geodetic, geological and seismological data posited that surface deformation was driven by rupture on the Leogane blind thrust fault, while part of the rupture occurred as deep lateral slip on the Enriquillo-Plantain Garden Fault (EPGF). The earthquake triggered >4490 landslides, mainly shallow, disrupted rock falls, debris-soil falls and slides, and a few lateral spreads, over an area of similar to 2150 km(2). The regional distribution of these slope failures defies those of most similar earthquake-triggered landslide episodes reported previously. Most of the coseismic landslides did not proliferate in the hanging wall of the main rupture, but clustered instead at the junction of the blind Leogane and EPGF ruptures, where topographic relief and hillslope steepness are above average. Also, low-relief areas subjected to high coseismic uplift were prone to lesser hanging wall slope instability than previous studies would suggest. We argue that a combined effect of complex rupture dynamics and topography primarily control this previously rarely documented landslide pattern. Compared to recent thrust fault-earthquakes of similar magnitudes elsewhere, we conclude that lower static stress drop, mean fault displacement, and blind ruptures of the 2010 Haiti earthquake resulted in fewer, smaller, and more symmetrically distributed landslides than previous studies would suggest. Our findings caution against overly relying on across-the-board models of slope stability response to seismic ground shaking. (C) 2012 Elsevier B.V. All rights reserved.