the Congo River. The Zaire Fan is a mud-rich turbidite system of particular importance to scientists as it is currently active. This activity was first documented in 1964 as cable breaks located across the Congo River. These events were correlated with periods of flood activity and determined to be the result of turbidity currents [2]. A submarine fan is an accumulation of sediment that forms in a cone-like shape. The sediment is generally transported from a canyon into a main feeder channel to be deposited
significance of fine-grained sediment fluxes in fluvial systems continues to underscore the need for reliable information on the principal sources. Traditional monitoring techniques are unable to solve the source estimation alone and had many spatial and temporal limits, but sediment source fingerprinting method has emerged as a potentially valuable supplement to address these issues. Despite the rapidly increasing numbers of studies reporting that the use of sediment source fingerprinting method
Heavy metal distribution in sediments around Kallur Mandli and Sagar road Industial estate Shimoga, Karnataka, India. Jayaram G. N.1, Chandrashekarappa K. N.2 and Anantha Murthy K S2 1 Dept. Of Civil Engineering, Shree Devi Institute of Technology, Kenjar, Mangalore – 574142 Email: jayaramhonnavar@gmail.com 2 Dept. of Applied geology, Kuvempu University, Shimoga, Karnataka - 577451 Abstract The present study was taken up to identify trace metals as well as to assess the extent of anthropogenic
This is concerning as, presently, over 40 million people reside in coastal shoreline counties in the Northeast USA, and this number is still growing. This number stresses the importance of vegetation stabilizing soil profiles and flood reduction through wave attenuation provided by coastal marsh areas. Also, coastal sediment inputs, a key
(at least its southern portion). In addition to the geological developments described above, the aquifer area also comprises the upper Nile Platform in Egypt, as well as the Northern Sudan Platform in Sudan. These are, however, areas of minor importance for groundwater resources. The NSAS changes gradually from continental sandy facies in the southern regions, to intercalations of sandstones and clays of alternating continental and shallow marine facies in the central regions, to mainly marine
imbalances the different natural systems, eventually disturbing the sediment transport equilibrium which affects the system efficiency, reducing benefits derived from the dam construction. Bed aggradations on upstream of dams are seen as a result of such disturbance. Sediment particles in the river are in form of sand, silt, gravel and even larger boulders. Water flowing in the river, scours its bed and banks, detaching these sediment panicles from the surface and carries them to the downstream. If
It can be argued by some geologists that significantly more time is lost at bedding planes than is recorded by the accumulation of sediment and its later lithification into a sedimentary rock. In the present paper, the continuity of the sedimentary record is investigated. It is hypothesized that sedimentary strata preserved predominately records episodic sedimentation events and gaps represented by bedding planes symbolize more time than the preserved strata. The incompleteness of the geologic record
Sayleen Arocha South Florida Landscapes Prof.Bueno LAA5541 When we think of nature, many do not know that solutions exist within nature itself. Albert Einstein once said “Look Deep into Nature, and then you will understand everything better”. The importance of protecting natural ecosystems has never been brought to light as much as in present day today. Humans are now trying to figure out ways to restore and protect natural ecosystems. I’m absolutely certain that we will succeed in protecting and restoring
The majority of the world freshwater is shallow and confined to lowland areas (Beklioglu et al., 2011). These shallow polymictic lakes usually with a depth of less than three meters are an important natural resource and facilitate numerous services, as result having a crucial economical and conservation value (Beklioglu et al., 2011). High quality of these lakes has become a political obligation with initiatives such as the European commission’s water frame work directive implemented both locally
). Extreme storms can have greater effects, for example by completely destroying sand bars or other sediment deposits. All this implies that when there are strong waves estuary mouths open wider and when there are no waves the estuary mouths remain closed. River flow or fresh water in flow has a significant influence on estuaries (Levin and Boesch et