181
S'
STRUCTURAL GEOLOGIC MAP
SUKABUMI AREA
EROM LANDSAT IMAGERY
yy 1 STRIKE. Sup FAWJ
> of Sukabumi
West Java
t volcanic
It creates
:i fault zone.
igery of West
:ails of this
)ression angle
; emphasize
)e the
SIR-A system is
a wavelength of
, it used the
from an
Lination of 38
-A imagery of
:e to the radar
jntinuation of
in N-E, ENE-WSfc
3 around most of
3 of the
:hern Mountain
Figure 21: Landsat Edge-Qihanced Band-7 imagery,
Lenbang area. West Java.
Figure 22: Relief Map, Lenbang area developed using
information retrieved from EE Band-7 imagery.
x
X /-
Figure 23: a) SIR-A imagery over West Java area. Radar look-direction is from
SE to NW. b) Relief diagram of West Java area based on information retrieved
from SIR-A imagery.
physiographic zone and the sharpness of the drainage
system disected by the Lenbang fault. The distortion
known as "radar layover" is not pronounced in the
SIR-A imagery over West Java area because of the
moderate depression angle, 38 degrees, of the system.
On the SIR-A imagery, the plain of Jakarta in the
North can easily be separated from the hilly and
mountaineous region to the south. The E-W
distribution of ridges found in this hilly region
complement the previous conclusion a N-S maximum
principal horizontal stress responsible for the
development of the structural geologic features in
the area.
SUMARRY AND CONCLUSION
'The Landsat full-scene MSS imagery of West Java area
provides information for systematic, comprehensive
analysis and interpretation of geologic setting in
this area. In this case, the geologic information,
