9:59:59.000,9:59:59.000 Hi guys, 9:59:59.000,9:59:59.000 the objective of this video is to look at 9:59:59.000,9:59:59.000 the bedding structures that form[br]when sediment is deposited. 9:59:59.000,9:59:59.000 These bedding structures all form [br]in different environments. 9:59:59.000,9:59:59.000 These environments which create the bedding [br]structures will be discussed. 9:59:59.000,9:59:59.000 Firstly,[br]we will talk about the horizontal beds, 9:59:59.000,9:59:59.000 or strata,[br]that the sediment is laid down in. 9:59:59.000,9:59:59.000 Sedimentary rock is stratafied,[br]which means that it has layers. 9:59:59.000,9:59:59.000 These layers have formed because sediment [br]is laid down in horizontal layers called strata. 9:59:59.000,9:59:59.000 Between each layer of strata,[br]we have bedding planes. 9:59:59.000,9:59:59.000 And these bedding planes form because [br]the region has experienced 9:59:59.000,9:59:59.000 a change in depositional [br]environment or material. 9:59:59.000,9:59:59.000 We can see here in this photo that we have [br]had one type of sediment laid down. 9:59:59.000,9:59:59.000 And then,[br]a change in depositional environment 9:59:59.000,9:59:59.000 has caused a different type of sediment[br]to be laid down on top, 9:59:59.000,9:59:59.000 in between which is a bedding plane. 9:59:59.000,9:59:59.000 We know that the strata towards[br]the bottom of a series is older 9:59:59.000,9:59:59.000 than the strata at the top. 9:59:59.000,9:59:59.000 And this happens because the sediment [br]is laid in this way. 9:59:59.000,9:59:59.000 Bedforms are formations that occur due to [br]the movement of wind and water. 9:59:59.000,9:59:59.000 Bedforms are created when water or wind,[br]flows over loose sediment. 9:59:59.000,9:59:59.000 And the shape and the texture of the bedform,[br]depends on the velocity of the flowing wind or water, 9:59:59.000,9:59:59.000 and the size of the sediment. 9:59:59.000,9:59:59.000 One type of bedform is ripples. 9:59:59.000,9:59:59.000 Ripples occur to due the flow of water. 9:59:59.000,9:59:59.000 Asymetrical ripples occur when water's [br]just flowing in one direction. 9:59:59.000,9:59:59.000 As we can see here. 9:59:59.000,9:59:59.000 Symetrical ripples will occur [br]when the waves oscillate back and forth. 9:59:59.000,9:59:59.000 As we can see here. 9:59:59.000,9:59:59.000 These bedforms can be preserved in[br]the sedimentary rock, 9:59:59.000,9:59:59.000 because new sediment can be deposited on top. 9:59:59.000,9:59:59.000 And the formation will remain the same[br]and will be lithified in this shape. 9:59:59.000,9:59:59.000 Another type of bedform are dunes. 9:59:59.000,9:59:59.000 Dunes form with the same formation process [br]as the asymetrical ripples when they form 9:59:59.000,9:59:59.000 due to water. 9:59:59.000,9:59:59.000 However,[br]dunes form due to the action of wind. 9:59:59.000,9:59:59.000 Cross Bedding is another type of [br]bedform. 9:59:59.000,9:59:59.000 Cross bedding forms in the process of [br]making ripples or dunes. 9:59:59.000,9:59:59.000 Whether