“…Therefore, it is important to measure the dose rates at different geological areas (Martin & Harbinson, 1972). In the past years, several radiation surveys were carried out in many countries to measure outdoor terrestrial g radiation doses (Brígido, Caballero, Montalv an Estrada, Queipo García, S anchez, 1999;Gabdo, Ramli, Sanusi, Saleh, & Garba, 2014;Kapdan, Taskin, Kam, & Osmanlio glu, 2012;Morishima et al, 2000;Mustapha et al, 2013;Nizam, Ginnah, Rahman, Kamal, & Chowdhury, 2013;Otansev, Karahan, Kam, Barut, & Taskin, 2012;Pashazadeh, Aghajani, Nabipour, & Assadi, 2014;Saleh et al, 2013;Shahbazi-Gahrouei, 2003). Many rivers in India and other countries have been studied such as river Pannoiyar (Ramasamy, Suresh, Meenakshisundaram, & Gajendran, 2009), Palar (Ramasamy, Murugesan, & Mullainathan, 2006),Cauvery (Murugesan, Mullainathan, Ramasamy, & Meenakshisundaram, 2011;Ramasamy, Murugesan, & Mullainathan, 2004), Kali, Sharavathi, Netravathi (Narayana, Rajashekara, & Siddappa, 2007) and Godavari (Reddy, Reddy, Reddy, & Reddy, 2014) in India and Chao Phraya river in Thailand (Santawamaitre et al, 2011), Ribble Estuary in England (Punt, Tyler, Saleh, Bradley, & Copplestone, 2011) Ogun river in Nigeria (Jibiri & Okeyode, 2012) and river Pearl in China (Song, Chen, Tang, Zhang, & Xie, 2012).…”