scholarly journals Index maps for large-scale vertical black and white aerial photographs along the San Andreas Fault, California

1979 ◽  
Author(s):  
Charles W. Hedel ◽  
H.A. Villalobos
1989 ◽  
Vol 79 (3) ◽  
pp. 901-909
Author(s):  
James J. Lienkaemper ◽  
Thomas A. Sturm

Abstract The U.S. Geological Survey has formally forecast the next moderate (M6) Parkfield earthquake for 1988 ±5 yr. Sieh and Jahns (1984) forecast that a M7 earthquake is likely to accompany the next Parkfield earthquake. The latter forecast rests on interpretation of 3 to 4 m of 1857 slip on eight gullies near Cholame and slip-loading rate of 3.5 cm/yr since 1857. But Lienkaemper (1987) interprets 1857 slip here as 4 to 8 m. These eight gullies yield larger slip when one includes slip on secondary faults (at three gullies), and one picks gully centerlines judging the post-1857 alteration differently (at five sites). Our goal in this paper is to show our interpretation of slip on one gully deemed the least ambiguous of these eight (as they appear in large-scale, 1966 aerial photographs). We interpret slip as 2-m larger at this key site, suggesting a much lower likelihood of the next Parkfield earthquake triggering a larger Cholame earthquake. Our detailed studies of many sites showing 1857(?) slip are continuing and will be published later. Using 1966 aerial photos, we infer the shape of this key gully before fault offset by eliminating effects of later natural and artificial processes of alteration. On 1986 photos right-lateral offset seems 3.5 ± 0.5 m, but on 1966 photos we measure 5.7 ± 0.7 m. Differencing precise 1966 and 1986 topographic maps shows that little incision occurred, but soil deposited up to a 1-m thickness on the left bank (probably drifted downslope from agricultural disking in the adjacent field). This soil deposit forced the channel bottom 2-m away from the left bank (upstream from fault only), causing offset in 1986 to appear 2-m smaller than in 1966. This 2-m alteration presumably occurred before Sieh (1978) interpreted 3.3-m slip here.


1996 ◽  
pp. 64-67 ◽  
Author(s):  
Nguen Nghia Thin ◽  
Nguen Ba Thu ◽  
Tran Van Thuy

The tropical seasonal rainy evergreen broad-leaved forest vegetation of the Cucphoung National Park has been classified and the distribution of plant communities has been shown on the map using the relations of vegetation to geology, geomorphology and pedology. The method of vegetation mapping includes: 1) the identifying of vegetation types in the remote-sensed materials (aerial photographs and satellite images); 2) field work to compile the interpretation keys and to characterize all the communities of a study area; 3) compilation of the final vegetation map using the combined information. In the classification presented a number of different level vegetation units have been identified: formation classes (3), formation sub-classes (3), formation groups (3), formations (4), subformations (10) and communities (19). Communities have been taken as mapping units. So in the vegetation map of the National Park 19 vegetation categories has been shown altogether, among them 13 are natural primary communities, and 6 are the secondary, anthropogenic ones. The secondary succession goes through 3 main stages: grassland herbaceous xerophytic vegetation, xerophytic scrub, dense forest.


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