International Journal of Trend in Scientific Research and Development

Mass media is a very powerful tool to influence the minds of a teenager. Teenagers are in that stage of growing up where everything influences them. Todays Socialization is turned as a chaos through apps From Facebook to Tinder, Instagram to WhatsApp, YouTube to Ticktock everyone has been socialized. As per Psychological point view... teenagers, young generation are been exploited in the name of Socialization. People under these categories are involved Anti National, Anti Social activities and Crime based activities like Drug abduction, Rape Molestation, Kidnap Murder. The Present Study tries to focus on the x facts of this Problem and try to understand how and what kind of role is played by the media which pressurize the young generation. This Study is Literally focused on the impact of Mainstream Media which includes Social Media, Internet, Entertainment Genres like Cinema, TV Soaps, Reality Shows, YouTube Videos, Entertainment Apps etc. on Young Generation or Teenagers on Negative Side. For this purpose 100 subjects male and female were selected randomly from selected Degree Colleges Undergraduate in southern part of Bangalore City, with a pretested Self Assessment tool to measure the usage and consumption of both mainstream media and internet among students of various stream based on their demographic variables like gender, education, course stream. Findings of the study indicates that there is a significant difference in relation to male, female and respective educational streams between Arts, Science and Commerce. 

Fifteen stream sediment samples were collected in Bwanebwa area, situated southwestern part in the central domain of the Pan African Fold Belt in Cameroon. Samples were analyzed by Aqua Regia Inductive Coupled Plasma Mass Spectrometry analytical technique. The chemical analyses revealed a wide variability of lanthanide concentrations REE = 1471.56 7674.2 ppm displaying a normal distribution pattern. Lanthanides show a high enrichment in La, Ce, Pr, Nd, and the proportion enrichment of REEs is still similar with increasing atomic number. The order of the average concentrations of REEs is Ce La Nd Pr Sm Gd Dy Er Tb Ho Yb Eu Tm Lu, which was different to that found in the Oddo Harkins rule, earth’s crust, upper continental crust, South China Sea, mean REE values in oceanic crust, Redang Island Marine Sediment in Terengganu Coastal Waters, Bayan Obo ores, Edéa, suggesting that REEs set up a complex group. The LREE HREE ratio 31.57 35.24, av. = 32.82 showed that the content of LREE 1425 7449.8, av. = 3699 is significantly higher than that of HREE 46.56 224.4, av. = 112.07 . LREEs account for 97.06 of the total REEs and this percentage is in agreement with the trend that was observed in the earth’s crust and in the Bayan Obo ores. Chondrite normalized REE distribution patterns are identical, indicating the consistency of geochemical distribution of REEs in stream sediments. They are strongly fractionated, with LREEs significantly fractionated LaN YbN = 11.74 27.93, av. = 21.04 relative to HREEs GdN YbN = 7.40 16.69, av. = 13.35 , implying that HREEs are more soluble and more complex than middle or LREE and are more strongly absorbed on most substrates. Positive Ce anomaly Ce Ce = 1.04 1.07 and negative Eu anomaly Eu Eu = 0.097 0.17 were observed, indicating that di erentiation occurred between Ce, Eu and other lanthanides. Therefore the positive Ce anomaly recorded represents an enrichment of Ce compared with its neighboring elements. A five factor model of the REEs that accounts for 1.998 of the total data cumulative variance have been observed, with the communality values 0,996 1 reflecting stronger community structure. Principal component analysis results in five components that explain 100 of the total variance, with the placement of elements in three major principal components, in which elements scattering in the rotated space displaying their mutual association. The results provide evidence for similar input sources and common geochemical characteristics of REEs. Lanthanide concentrations in Bwanebwa area were of geogenic origins and not influenced by anthropogenic sources. The abundance of REEs is related to the lithology made up of granites and associated pegmatites. Cerium shows the highest average content of REEs, followed by La, Nd, Pr, Gd, Sm, hence pattern of Ce distribution shows higher than the other lanthanides. LREEs La, Ce, Pr, Nd and Ga fall above the upper background threshold limit and are considered as anomalous. Therefore the results of this work serve as guide for lanthanides exploration in Bwanebwa area. 

Fifteen stream sediment samples were collected in Bwanebwa area, situated southwestern part in the central domain of the Pan African Fold Belt in Cameroon. Samples were analyzed by Aqua Regia Inductive Coupled Plasma Mass Spectrometry analytical technique. The chemical analyses revealed a wide variability of lanthanide concentrations REE = 1471.56 7674.2 ppm displaying a normal distribution pattern. Lanthanides show a high enrichment in La, Ce, Pr, Nd, and the proportion enrichment of REEs is still similar with increasing atomic number. The order of the average concentrations of REEs is Ce La Nd Pr Sm Gd Dy Er Tb Ho Yb Eu Tm Lu, which was different to that found in the Oddo Harkins rule, earth’s crust, upper continental crust, South China Sea, mean REE values in oceanic crust, Redang Island Marine Sediment in Terengganu Coastal Waters, Bayan Obo ores, Edéa, suggesting that REEs set up a complex group. The LREE HREE ratio 31.57 35.24, av. = 32.82 showed that the content of LREE 1425 7449.8, av. = 3699 is significantly higher than that of HREE 46.56 224.4, av. = 112.07 . LREEs account for 97.06 of the total REEs and this percentage is in agreement with the trend that was observed in the earth’s crust and in the Bayan Obo ores. Chondrite normalized REE distribution patterns are identical, indicating the consistency of geochemical distribution of REEs in stream sediments. They are strongly fractionated, with LREEs significantly fractionated LaN YbN = 11.74 27.93, av. = 21.04 relative to HREEs GdN YbN = 7.40 16.69, av. = 13.35 , implying that HREEs are more soluble and more complex than middle or LREE and are more strongly absorbed on most substrates. Positive Ce anomaly Ce Ce = 1.04 1.07 and negative Eu anomaly Eu Eu = 0.097 0.17 were observed, indicating that di erentiation occurred between Ce, Eu and other lanthanides. Therefore the positive Ce anomaly recorded represents an enrichment of Ce compared with its neighboring elements. A five factor model of the REEs that accounts for 1.998 of the total data cumulative variance have been observed, with the communality values 0,996 1 reflecting stronger community structure. Principal component analysis results in five components that explain 100 of the total variance, with the placement of elements in three major principal components, in which elements scattering in the rotated space displaying their mutual association. The results provide evidence for similar input sources and common geochemical characteristics of REEs. Lanthanide concentrations in Bwanebwa area were of geogenic origins and not influenced by anthropogenic sources. The abundance of REEs is related to the lithology made up of granites and associated pegmatites. Cerium shows the highest average content of REEs, followed by La, Nd, Pr, Gd, Sm, hence pattern of Ce distribution shows higher than the other lanthanides. LREEs La, Ce, Pr, Nd and Ga fall above the upper background threshold limit and are considered as anomalous. Therefore the results of this work serve as guide for lanthanides exploration in Bwanebwa area. 

This Paper has been made in order to examine the potential of natural resources of Bhaderwah. India is a country with diverse of natural resources. It has plenty of water. Neeru Nallha is the main source of water in Bhaderwah it covers nearly about 1.83 square kilometer area. It is also rich in several natural resources. Bhaderwah is the backbone of the timber industry of J and K as it is well developed in forest. It also plays an important role in the economy of Bhaderwah. These gifts of nature are known as natural resources.Remote sensing and GIS techniques have been used to demarcate the areaunder various natural resources. Satellite data have been extracted from different sites which are useful in mapping and quantifying the extent of natural resources of Bhaderwah. The slope map of the study area is generated through Digital Elevation Model DEM . The DEM generate from the digitized topographic contour which can be used through GIS to extract slope morphology.In this study Geographical information system GIS and different satellitesimages have been used to extract the natural resources area which is useful forfuture planning. Geographical information system GIS helps a lot in monitoring the area of these natural resources as compared to convectional techniques. 

The study of water sources used by the population of Ndian for drinking with the exception of the Ekondo Titi beach was carried out by investigating 51 water sources. Due to the lack of pipe borne water in this area, the population is compelled to consume water from unprotected shallow aquifers and surface water sources, there by exposing the population to infections form of water borne diseases. In this perspective, the present study was aimed to check the suitability of these water sources for drinking. The bacteriological quality of the water sources was performed using the Most Probable Number MPN technique. Temperature, pH, electrical conductivity EC and total dissolved solids TDS were also determined. The pH values reflect slightly acidic, neutral and basic water sources. Sixty percent 60 of the ground water samples where slightly acidic 5.5  6.4 and out of the WHO 2011 guideline limit 6.5 8.5 for drinking water. This situation puts the inhabitants at risk to stomach ulcer. The electrical conductivity values 3.00 274 us cm for groundwater sources represents water experiencing slight mineralization. Based on the total coliform bacteria, 96 of water sources were polluted to grossly polluted 75 2400 MPN 100 ml and 4 excellent following the acceptable maximum limits prescribed by the World Health Organization Standards which exposes the population to water borne diseases such as typhoid, cholera and dysentery. The bacteria contamination of the water sources may result from the waste of pit toilets that intersect the water tables of shallow unconfined aquifers and also from poor sanitation practices carried out along stream channels and springs. Proper water treatment at household levels is highly recommended.