WEBVTT 99:59:59.999 --> 99:59:59.999 Hi guys, 99:59:59.999 --> 99:59:59.999 the objective of this video is to look at 99:59:59.999 --> 99:59:59.999 the bedding structures that form when sediment is deposited. 99:59:59.999 --> 99:59:59.999 These bedding structures all form in different environments. 99:59:59.999 --> 99:59:59.999 These environments which create the bedding structures will be discussed. 99:59:59.999 --> 99:59:59.999 Firstly, we will talk about the horizontal beds, 99:59:59.999 --> 99:59:59.999 or strata, that the sediment is laid down in. 99:59:59.999 --> 99:59:59.999 Sedimentary rock is stratafied, which means that it has layers. 99:59:59.999 --> 99:59:59.999 These layers have formed because sediment is laid down in horizontal layers called strata. 99:59:59.999 --> 99:59:59.999 Between each layer of strata, we have bedding planes. 99:59:59.999 --> 99:59:59.999 And these bedding planes form because the region has experienced 99:59:59.999 --> 99:59:59.999 a change in depositional environment or material. 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 99:59:59.999 --> 99:59:59.999 And then, a change in depositional environment