Titlebook: Recent Studies in Geophysical Hazards; M. I. El-Sabh,T. S. Murty,K. Andah Book 1994 Springer Science+Business Media Dordrecht 1994 Earthqu

BAN

Mhc-Molecule

Mass Movements in Hilly Areas (with Examples from Nigeria)ovements also occur in areas of lower relief, i.e. in areas of less geomorphic activity. An extreme case of this type has been found in the development of cracks in a flat savannah area of Nigeria which has generally been ascribed to purely hydrological causes. Nevertheless, it can be shown that the

notification

羊齒

Seismic Hazard Analysis with Randomly Located Sourceslts. The uncertainty associated with the description of the geographical coordinates of a source zone boundary is modeled by introducing the concept of ‘random boundary’, where the location of the boundary is assumed to exhibit a spatial bivariate Gaussian distribution. Here the mean vector denotes

ALIAS

Regional Fracture Analysis South Latitude 29° N of Egypt and Their Influence on Earthquakesthe locations where fractures have relatives high densities..The Fracture pattern of Egypt south Latitude at 29° N was studied regionally based on Landsat images and aerial photomosaics. Fractures in the Eastern Desert have the prominent trends, NW, E-W, NNW and ENE, showing high density in the nort

Endemic

菊花

Evaluation of Climatic Change through Harmonic Analysisam and Blackman-Tukey method through to the Maximum Entropy method. The results do not show the existence of climatic cycles, though they do show a clear tendency toward increased precipitation and decreased temperature, since the last years of series.

債務(wù)

Bumble

anthropologist

Storm Surge Mitigation through Vegetation Canopiesght. The vertical rate of change of friction velocity depends on the mean water current, the wind stress, the bottom roughness, and the water depth. This work has a possible application in the mitigation of storm surges.