Investigating the Length of Long Shore Occurence

The place I'm studying is Somerset's Pollok Bay. This is a picture of Porlock Bay. [Image] Purpose: To find the beach material of Long Beach drifting to develop a defense mechanism for Pollock Bay to prevent flooding in the marshes. Evidence for coastal drift: There is no breakwater without coastal drift, but the beach will be completely flat.

Based on the information examined in the introduction, we will examine and compare the adaptability of Pelvetia canaliculata in two different places with different conditions. I compare the leaf lengths of Pelvetia canaliculata on a rocky shore of the waves and a rocky shore exposed by the waves. Experimental hypothesis: There is a statistically significant difference between the length of Pelvetia canaliculata grown between coast exposed to wave and protected rocky coast with wave. In many cases, the waves are less likely to be exposed, so the tip is less likely to break at the tip, so it will be longer.

As the white phoenix blue waves drift towards the foamy coast, they bring a long history. Many of these waves have traveled miles to Milwaukee and when they reach the rocky coast the long and troublesome journey turns into a sudden and intense end and the waves are the side of the jagged granite It affects. . Cold water spews scattered water droplets through fresh air, and everyone really does not know where they landed. Some waterdrops will eventually stop splashing on the nearby sand and evaporate only by the heat radiated from the sun. Other people may just disappear in the air. However, many waves do not survive long enough to reach the coast. Upon arriving in any direction from the pier or the embankment, they interact with each other in a complex pattern to share the story of their journey. But not only clear water but also the beauty of the scene will improve

When a large amount of water (such as the sea and the ocean) is drained and a long wave of water reaches the shore, a tsunami is generated. The most common cause of the tsunami is the underwater earthquake, but it can also be caused by other events such as volcanoes and water landslides. Although the tsunami often occurs without warning, scientists have been able to issue tsunami warnings in situations where there is a possibility of causing a tsunami at a monitoring station in some areas of the world