Faculty Publications
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Item Neotectonic evolution of Coastal Rivers of Mangalore, Karavali Karnataka, India(2011) Ravindra, B.M.; Venkat Reddy, D.The geomorphic evolution of Mangalore is intimately influenced by Neo-tectonic activities that affected the West Coast and peninsular India that led to the upliftment of Sahyadri Range. Mangalore pediplain has preserved signatures of (1) An older cycle of River system that existed prior to the rise of Sahyadri and (2) Several phases of migration paths of the West flowing Sahyadri Rivers, reflecting geomorphic changes in the pediplain in response to the tectonic strains generated during the rise of the Sahyadri range and northward drift of the Indian subcontinent. The compressional stress derived from the phenomenon of Sea floor spreading is manifested in the Karavali pediplain, in the form of EW and NNW intersecting transform faults that activate periodically and trigger microseismic disturbances severe sea erosions or landslides under adverse hydrological conditions. Similarly under the regime of compressional stress, the Mangalore pediplain evinces evidences of sequential development of anticlinal upwarps that broke into horsts and grabens separated by escarpments. The Holocene fluvial evolution of Mangalore consisted of migration of the two Rivers in opposite directions with progressive passage of time in the Holocene. Fluvial geomorphology of Mangalore has also preserved evidences that substantiate shifting of trans-peninsular Mulki - Pulicat Ridge Axis from its original position northwards. The ongoing structural disturbances and micro-seismic and allied recent neo-tectonic activities imply that the processes responsible for the creation of the Sahyadri range have not died down yet and are very much in attendance even today. © 2011 CAFET-INNOVA TECHNICAL SOCIETY. All rights reserved.Item Assessment of water quality of river Ganga along ghats in Varanasi city, U. P., India(2011) Thomas, T.; Mishra, M.; Thomas, H.; David, A.A.; Bharose, R.; Venkat Reddy, D.Assessment of water quality was done in holy River Ganga district of Varanasi, (U.P.) India in 2009. Water samples were collected from fives different sites namely (S 1)- Samne Ghat, (S 2)- Assi Ghat, (S 3)- Harishchandra Ghat, (S 4)- Dasaswamedh Ghat, (S 5)- Dr. Rajendra Prashad Ghat. The Ganga, one of the world's major rivers, has been venerated as the holiest and is bound with countless beliefs and faiths especially in India and adjacent countries. Its water has traditionally been regarded as pure and holy in nature gift to human. Recent experiences however do not warrant such complacency. The water resources are strained to a non-sustainable level due to rapid population growth, urban development, industrialization; livestock and power production on the Ganga Ghats at Varanasi city. The severe pollution stress and causes to which its water is subjected to the contents and quality of water and possible remedial measures. According to the result obtained by analyzing various Physico-chemical parameters of Ganga river in Varanasi City, maximum BOD recoded in (S 2)- Assi Ghat and minimum in (S 1)- Samne ghat whereas maximum DO was observed in Samne Ghat and minimum in (S 2)- Assi Ghat during Jan to March 2009 period respectively. On the basis of our experimental results it can be concluded that (S 2)- Assi Ghat exhibited higher pollution index than other ghats due to higher values of Turbidity, pH, BOD, Hardness, Alkalinity and Nitrate disposal occurring at (S 2)- Assi Ghat as well as disposal of industrial sewage in the (S 2)- Assi Ghat. Regular monitoring of Ganga river water quality is necessary to have a check on surface water quality for the sake of human life & to maintain a balanced aesthetical value of religious. We have to restore the environmental quality of Ganga which is amended by policy makers of Indian constitution. © 2011 CAFET-INNOVA TECHNICAL SOCIETY. All rights reserved.Item Terrain analysis and hydrogeochemical environment of aquifers of the southern west coast of Karnataka, India(2012) Honnanagoudar, S.S.; Venkat Reddy, D.; Mahesha, A.Dakshina kannada district is situated in peninsular region. The peninsula is composed of geologically ancient rocks of diverse original and most of them have undergone metamorphism. The early Precambrian tonalitic gneisses invaded by granites, granulites and dolerite dykes. Granulites are mostly restricted to areas south of Mangalore. High grade alumina rich (corundum bearing) metamorphic schists have been encountered and younger alkaline intrusive rocks like Aegerine syenites have been reported. There are five rivers and estuaries. Number of lineaments cut across each other and some lineaments are parallel to each other. The Arabian sea class is the largest among other land cover features in the study area. The river/tidal creek land cover appear as long irregular and sinous in outline. Mulki river, Netravati river, Gurupur river at southern terrain. The qualities of groundwater at sandy aquifer are good, lateritic/weathered gneissic rocks it is sweet. © 2012 CAFET-INNOVA TECHNICAL SOCIETY.Item Geomorphology and hydrogeology of coastal tracts of the Central West Coast of India(2013) Honnanagoudar, S.S.; Venkat Reddy, D.; Mahesha, A.Dakshina Kannada district which is a coastal district of Karnataka, spreads along the west coast of India covering coastal tract of about 40 km. Dakshina Kannada district is divided into three regions, low land, mid land and high land. The coast line is generally straight and followed the Dharwar rocks trending NNW-SSE.The rocks weathered fractured and jointed granitic gneisses and laterite varies from 10 m to 30 m. The thickness of coastal alluvium varies from 7 to 29 m. There are spits and beach ridges available in coastal tract. The Netravati river flow towards Mangalore where it joins Gurupur River and both the Rivers from common esture discharging into the sea. Gneissic rocks archaean age cover a major part of this region as basement rocks. These are elsewhere overlain by oligomictic quartz conglomerate belonging to Dharwar super group. The recent alluvium and colluvial deposits occur along the river bed and sea coast. The exposure of crystalline rock found as isolated hills along the shore and off shore. The black clay marine sediments with a thickness of 0.30 m to > 1m occur as lenses along the coast and in the deltaic islands. Its occurrence as marked at a depth ranges of 5 to 6 mbgl. The groundwater below the black clay horizons of coastal sediments found with high salinity, which marks the index bed for saline water and fresh water interface. © 2013 CAFET-INNOVA TECHNICAL SOCIETY.