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Chetty, T. R. K., Rao, R. Satyanarayana (1986) Proto-Penner River Course and its Role in the Distribution of Alluvial Diamonds: An Evidence from Landsat Data. Journal of the Geological Society of India, 28 (6). 480-488

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Reference TypeJournal (article/letter/editorial)
TitleProto-Penner River Course and its Role in the Distribution of Alluvial Diamonds: An Evidence from Landsat Data
JournalJournal of the Geological Society of India
AuthorsChetty, T. R. K.Author
Rao, R. SatyanarayanaAuthor
Year1986 (December)Volume28
Page(s)480-488Issue6
PublisherGeological Society of IndiaPlaceBangaluru, India
Classification
Not set
LoC
Not set
Mindat Ref. ID17768034Long-form Identifiermindat:1:5:17768034:4
GUID0
Full ReferenceChetty, T. R. K., Rao, R. Satyanarayana (1986) Proto-Penner River Course and its Role in the Distribution of Alluvial Diamonds: An Evidence from Landsat Data. Journal of the Geological Society of India, 28 (6). 480-488
Plain TextChetty, T. R. K., Rao, R. Satyanarayana (1986) Proto-Penner River Course and its Role in the Distribution of Alluvial Diamonds: An Evidence from Landsat Data. Journal of the Geological Society of India, 28 (6). 480-488
In(1986, December) Journal of the Geological Society of India Vol. 28 (6). Geological Society of India
Abstract/NotesA possible Proto-Penner river course, running in a NNE direction from the elbow of capture near Penna Ahobilarn and joining the river Tungabhadra near Kurnool, in Andhra Pradesh, has been inferred from a Satellite Remote Sensing based geomorphic study. Occurrence of lag-gravel and diamonds, remnant alluvial tracts, anomalous drainage pattern, etc. are cited as evidences. Some potential areas such as remnant alluvial patches along Proto-Penner river course and alluvial plains along adjacent streams and topographic depressions are indicated as possible areas for alluvial diamond exploration. Various geomorphic features occurring in Archaean denudational hill province and Cuddapah structural hill province are delineated.


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