554
•mmmhmhmbh
Intervals of 2 in and 4 m, respecitvely. Apart from
topographic details various cultural and landslide
details were also mapped. These included old and
fresh landslide scars, fracture lines, fissures,
broken ground, houses, vegetation. The stereo-pairs
were found to be highly useful for a comprehensive
evaluation of the land-slides and significantly
helped in a quick assessment of the slide areas.
4. DIGITAL TERRAIN MODELLING
The significance of morphomertic and thematic maps
in the comprehensive evaluation of the project
areas, particularly those related to geo-environmen-
tal aspects, hardly need any emphasis. In case
of Nilgiris landslide investigation the 'Surface
Area Ratio' maps of the two areas were prepared.
These established a strong correlation between
the slope parameters and the incidence of landslides
and thereby helped in identifying safe and hazardous
areas. Further, erosion, geomorphological and exist
ing landuse maps of the areas were also prepared.
Integration of the morphometric and the thematic
maps led to a comprehensive evaluation of the areas
(Agarwal & Sharma 1982).
Morphometric mapping requires topographic data
in a digital form at desired intervals, depending
upon the accuracy requirements and the surface
irregularities of the terrain. Computer assisted
analytical stereo-plotters in fact record the topo
graphic data in a digital form. Also, they hold
great promise in simultaneously recording the the
matic data in a coded form, as well. Thus if an
analytical stereo-plotter is used in place of an
analogue stereo-plotter then apart from topographic
base maps, morphometric and thematic maps can also
be produced simultaneously, either independently
or in combination.
DISCUSSIONS
Though the science of photogrammetry owes its origin
to the terrestrial photogrammetry, it was soon
overtaken by aerial photogrammetry due to its obvi
ous advantages in quickly covering larger areas.
However, terrestrial photogrammetry maintained
its relevance and advantages in certain disciplines
like glacier mapping, and surveys of steep inacce
ssible or remote areas. In snow mapping the signifi
cant advantages of the technique has clearly been
demonstrated by Blyth et.al. (1974).
Inspite of the increased applications of terres
trial photogrammetry, particularly in Architectu
ral engineering and various other fields, its appli
cation potential in geo-scientific investigations
has not yet been fully exploited. In this context
the case histories cited, amply demonstrate the
potential and advantages of this technique, in
geo-scientific studies. On account of the numerous
advantages of this technique over conventional
survey, the latter appears obsolete in comparison.
The technique holds great merit in monitoring dyna
mic features, as repeat photography can easily
be carried out from fixed camera stations, at desi
red time invervals.
While preparing maps by this technique on stereo
- plotters the ratio between the model scale to
the map scale is so selected that the maps prepared
have a plan accuracy of 0.5 mm on the map scale,
and the height accuracy lies within a quarter of
the contour interval. This is as per the accuracy
limits followed by the Survey of India (Agarwal
1974:78). Thus, if features to be monitored show
variations larger than 1 mm on plan scale, these
can be resolved through comnparison of different
maps. In case monitoring of smaller variations
is required then either an analytical or semi-analy
tical approach (Marzan & Karara 1976) is to be
applied.
An analytical stereo-plotter, unlike an analogue
one, has no constraints of photographic parameters,
and hence it is more versatile, besides being more
accurate too. Another aspect where it has signifi
cant advantage over analogue stereo-plotter is
in digital terrain modelling which holds great
promise for simultaneous topographical, morphometric
and thematic mapping. However, it is much more
sophisticated, costly and would involve the inter
action with experts for its operation. Accounting
various aspects, Marzan & Karara (1976) have opined
that if the maps produced by analogue stereo-plotter
meet the accuracy requirements for a particular
work, then the anologue method is the simplest,
most straightforward and perhaps the cheapest method
to employ.
It may be summarised that the technique of terres
trial photogrammetry is unique for preparation
of large scale topographic and thematic maps, for
a comprehensive evaluation of the project areas
in the shortest possible time. Simultaneous photo
interpretation, field checks and ground truth
data collection considerably expedites the work.
However, it would be relevant to mention that
the suitability of the technique for a given area
largely depends upon the availability of suitable
locations from where stereo-photographic coverage
of the area could be obtained.
REFERENCES
Agarwal, G.C. 1974. Photogrammetric surveys, their
planning and costing, Tech. Public No.7401,
Survey of India, Hyderabad.
Agarwal N.K. 1985. Mapping of inaccessible escarp
ment slope of left abutment of Supa Dam, Karna
taka, utilizing stereo-terrestrial photogramme
try, Jr. of Engineering Geology Vol.XIV, Nos.
1 & 2, ISEG.
Agarwal, N.K. & Srivastava, G.S. 1982. Geomorpho
logy and Environment of Coconut Island, South
Kanara distt., Karnataka, Proc. Symposium on
Resources surveys for Landuse planning and Envi
ronmental Conservation, ISPI & RS, Dehradun,
India.
Agarwal, N.K & Sharma. R.P. 1982. Terrestrial
photogrammetric evaluation of slide areas, Nil
giris dist., Tamil Nadu, Proc. 4th International
Congress, IAEG, India, Vol. III.
Blyth, K. Cooper, M.A.R., Lindsey, N.E. Painter,
R.B. 1974. Snow depth measurements with terres
trial photos. Photogrammetric Engineering, Vol.
XL, No.8.
Marzan, G.T. & Karara, M.M. 1976. Rational design
for close range photogrammetry, photogrammetry
series No. 43, Deptt. of Civil Engineering,
Univ. of Illinois, Urbana, Illinois, 61891.
Manual of Photogrammetry 1980, Fourth Ed. Am.
Society of Photogrammetry, Falls Church, U.S.A.
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