Geology----Stratigraphy and Sedimentation Article

Geology----Stratigraphy and Sedimentation - Article ExampleTwo pertinent events withstand been intricately discussed. These are namely the episodic events and the continuous events. By definition, the episodic events are used in reference to those that become eminent in a matter of hours or days. It is important to reiterate that their do are distinct and pertinent to this research. On the other hand, Continuous events are differentiated by the fact that they spread over months, years or even decades. Evidently, field mapping and reference chronology were succinctly use in the analysis process. The tree diagram sonority method is a pertinent component in geomorphology. This is unembellished in its multiple applications such as assistance in comprehension ofthe geomorphic processes, the consequent frequency and events. farther to this, the annual precision will also aid in predicting floods and other events in future so as to avert the damages caused by the same. Previous research has revealed that the flood rings in 1826 and 1850. In this regard, it was established that the tree with flood rings were proportionate to the discharge. The primary trees that were subject to the sampling procedure were those determine as are mainly affected by the geomorphic processes. These included trees growing near river banks, trees growing on the edges of gullies and avalanche paths and trees growing right on the sediment plants. In conclusion,the overall relevance of the tree ring method as far geomorphology is concerned includes ascertaining the magnitude and frequency of events, providing an annual precision the tree rings are pertinent as far as predicting continuous and episodic processes as hygienic as delineating the spatial location affected by a process.Howard and Blakey have done a worthy job in relating their observations and interpretations. The data provided is enough for all the facies interpretation. Their interpretation of fluvial channel mobility in no tification with the geometry of sandstone bodies is correct and there