1 99:59:59,999 --> 99:59:59,999 Hi guys, 2 99:59:59,999 --> 99:59:59,999 the objective of this video is to look at 3 99:59:59,999 --> 99:59:59,999 the bedding structures that form when sediment is deposited. 4 99:59:59,999 --> 99:59:59,999 These bedding structures all form in different environments. 5 99:59:59,999 --> 99:59:59,999 These environments which create the bedding structures will be discussed. 6 99:59:59,999 --> 99:59:59,999 Firstly, we will talk about the horizontal beds, 7 99:59:59,999 --> 99:59:59,999 or strata, that the sediment is laid down in. 8 99:59:59,999 --> 99:59:59,999 Sedimentary rock is stratafied, which means that it has layers. 9 99:59:59,999 --> 99:59:59,999 These layers have formed because sediment is laid down in horizontal layers called strata. 10 99:59:59,999 --> 99:59:59,999 Between each layer of strata, we have bedding planes. 11 99:59:59,999 --> 99:59:59,999 And these bedding planes form because the region has experienced 12 99:59:59,999 --> 99:59:59,999 a change in depositional environment or material. 13 99:59:59,999 --> 99:59:59,999 We can see here in this photo that we have had one type of sediment laid down. 14 99:59:59,999 --> 99:59:59,999 And then, a change in depositional environment 15 99:59:59,999 --> 99:59:59,999 has caused a different type of sediment to be laid down on top, 16 99:59:59,999 --> 99:59:59,999 in between which is a bedding plane. 17 99:59:59,999 --> 99:59:59,999 We know that the strata towards the bottom of a series is older 18 99:59:59,999 --> 99:59:59,999 than the strata at the top. 19 99:59:59,999 --> 99:59:59,999 And this happens because the sediment is laid in this way. 20 99:59:59,999 --> 99:59:59,999 Bedforms are formations that occur due to the movement of wind and water. 21 99:59:59,999 --> 99:59:59,999 Bedforms are created when water or wind, flows over loose sediment. 22 99:59:59,999 --> 99:59:59,999 And the shape and the texture of the bedform, depends on the velocity of the flowing wind or water, 23 99:59:59,999 --> 99:59:59,999 and the size of the sediment. 24 99:59:59,999 --> 99:59:59,999 One type of bedform is ripples. 25 99:59:59,999 --> 99:59:59,999 Ripples occur to due the flow of water. 26 99:59:59,999 --> 99:59:59,999 Asymetrical ripples occur when water's just flowing in one direction. 27 99:59:59,999 --> 99:59:59,999 As we can see here. 28 99:59:59,999 --> 99:59:59,999 Symetrical ripples will occur when the waves oscillate back and forth. 29 99:59:59,999 --> 99:59:59,999 As we can see here. 30 99:59:59,999 --> 99:59:59,999 These bedforms can be preserved in the sedimentary rock, 31 99:59:59,999 --> 99:59:59,999 because new sediment can be deposited on top. 32 99:59:59,999 --> 99:59:59,999 And the formation will remain the same and will be lithified in this shape. 33 99:59:59,999 --> 99:59:59,999 Another type of bedform are dunes. 34 99:59:59,999 --> 99:59:59,999 Dunes form with the same formation process as the asymetrical ripples when they form 35 99:59:59,999 --> 99:59:59,999 due to water. 36 99:59:59,999 --> 99:59:59,999 However, dunes form due to the action of wind. 37 99:59:59,999 --> 99:59:59,999 Cross Bedding is another type of bedform. 38 99:59:59,999 --> 99:59:59,999 Cross bedding forms in the process of making ripples or dunes. 39 99:59:59,999 --> 99:59:59,999 Whether