https://padlet.com/420182/s3jqk0ppx808 https://www.pandora.com/artist/juice-wrld/goodbye-and-good-riddance-explicit en-us 2019-03-29 15:20:26 UTC 2024-11-08 05:36:57 UTC hello@padlet.com 420182 https://padlet.com/420182/s3jqk0ppx808/wish/346595339 2019-03-29 15:21:43 UTC https://padlet.com/420182/s3jqk0ppx808/wish/346595339 420182 https://padlet.com/420182/s3jqk0ppx808/wish/346598741 https://geology.com/rocks/pictures/conglomerate.jpg ]]> 2019-03-29 15:28:34 UTC https://padlet.com/420182/s3jqk0ppx808/wish/346598741 420182 https://padlet.com/420182/s3jqk0ppx808/wish/346599412 https://geology.com/rocks/pictures/gneiss.jpg]]> 2019-03-29 15:29:54 UTC https://padlet.com/420182/s3jqk0ppx808/wish/346599412 420182 https://padlet.com/420182/s3jqk0ppx808/wish/346599585 https://geology.com/rocks/pictures/granite-coarse-grained.jpg]]> 2019-03-29 15:30:12 UTC https://padlet.com/420182/s3jqk0ppx808/wish/346599585 420182 https://padlet.com/420182/s3jqk0ppx808/wish/346834905 Heat and Pressure]]> 2019-03-31 00:04:56 UTC https://padlet.com/420182/s3jqk0ppx808/wish/346834905 420182 https://padlet.com/420182/s3jqk0ppx808/wish/346835460 Melting followed by cooling]]> 2019-03-31 00:16:01 UTC https://padlet.com/420182/s3jqk0ppx808/wish/346835460 420182 https://padlet.com/420182/s3jqk0ppx808/wish/346837638 Melting followed by cooling]]> 2019-03-31 00:49:31 UTC https://padlet.com/420182/s3jqk0ppx808/wish/346837638 420182 https://padlet.com/420182/s3jqk0ppx808/wish/346837656 Erosion , deposition, compaction, cementation of sediment]]> 2019-03-31 00:49:56 UTC https://padlet.com/420182/s3jqk0ppx808/wish/346837656 420182 https://padlet.com/420182/s3jqk0ppx808/wish/346837884 Heat and Pressure]]> 2019-03-31 00:54:35 UTC https://padlet.com/420182/s3jqk0ppx808/wish/346837884 420182 https://padlet.com/420182/s3jqk0ppx808/wish/346837930 Erosion, deposition
compaction, sedimentary of sediment.]]> 2019-03-31 00:55:14 UTC https://padlet.com/420182/s3jqk0ppx808/wish/346837930 420182 https://padlet.com/420182/s3jqk0ppx808/wish/346838037 2019-03-31 00:56:52 UTC https://padlet.com/420182/s3jqk0ppx808/wish/346838037 420182 https://padlet.com/420182/s3jqk0ppx808/wish/346838047 2019-03-31 00:57:07 UTC https://padlet.com/420182/s3jqk0ppx808/wish/346838047 420182 https://padlet.com/420182/s3jqk0ppx808/wish/346885431 Igneous rocks are made from molten magma bubbling out of the earths crust. As the magma cools down , it crystallizes and forms into igneous rocks. Magma can cool on the earth surface quickly or under the crust slowly. There are 2 types of igneous rocks, intrusive rocks and extrusive rocks. Intrusive Igneous rocks is when magma cools slowly beneath the ground causing large formed crystals. These rocks usually have a rough texture and have a well defining pattern. Some examples are Diorite, Dunite and Granite .The other form of Igneous rocks are Extrusive rocks. These forms when magma cools quickly on the surface. These rocks have small crystals and a non-defining pattern. Some examples of extrusive Igneous Rocks are Basalt, Andesite and Obsidian. These are the main differences in Igneous Rocks. ]]> 2019-03-31 13:04:12 UTC https://padlet.com/420182/s3jqk0ppx808/wish/346885431 420182 https://padlet.com/420182/s3jqk0ppx808/wish/346899164 Sedimentary rocks are made from Erosion, Deposition, compaction, and Cementaton of Sediment.The rock first erodes into individual grains of rock. Then they are deposited over an area on top of the earth. Then they are compacted into a rock like shape. Finally, they are cemented into a rock. This is the main process of creating a sedimentary rock. There are 2 types of Sedimentary Rocks, Clastic and Non-Clastic. Clastic Rocks form by Weathering Processes that break down the rocks into different pieces. Clastic Rocks are named by the size of their grain particles. Some Clastic Rocks are Conglomerate, Sandstone and Shale. The other type of Sedimentary Rock is Non-Clastic Rocks. These rocks form from Chemical Reactions, mostly in oceans. Some examples of Non-Clastic Rocks are Limestone, Rock Salt, and Rock Gypsum. ]]> 2019-03-31 15:04:44 UTC https://padlet.com/420182/s3jqk0ppx808/wish/346899164 420182 https://padlet.com/420182/s3jqk0ppx808/wish/347227496 https://assets.fishersci.com/TFS-Assets/CCG/product-images/F58962~p.eps-650.jpg]]> 2019-04-01 15:19:20 UTC https://padlet.com/420182/s3jqk0ppx808/wish/347227496 420182 https://padlet.com/420182/s3jqk0ppx808/wish/347228840 https://geology.com/rocks/pictures/obsidian-380.jpg]]> 2019-04-01 15:21:53 UTC https://padlet.com/420182/s3jqk0ppx808/wish/347228840 420182 https://padlet.com/420182/s3jqk0ppx808/wish/347236012 https://geology.com/rocks/pictures/sandstone.jpg]]> 2019-04-01 15:32:25 UTC https://padlet.com/420182/s3jqk0ppx808/wish/347236012 420182 https://padlet.com/420182/s3jqk0ppx808/wish/347420433 https://geology.com/rocks/pictures/limestone-chalk-380.jpg]]> 2019-04-01 23:45:57 UTC https://padlet.com/420182/s3jqk0ppx808/wish/347420433 420182 https://padlet.com/420182/s3jqk0ppx808/wish/347420536 Metamorphic rocks are formed from Heat and Pressure. There are 2 types of Metamorphic Rocks, Foliated Rocks and Nonfoliated Rocks. Foliated Rocks are formed when there is extremely high pressure and the pressure is greater in one direction. This causes the rock to have a stripped look, and the minerals in different bands. Some Foliated Rocks are Slate, Schist and Gneiss. The other type of Metamorphic rock are Nonfoliated Rocks. These rocks occur when the temperatures are high but not extremely high. The pressure is equal in all directions and the rocks have big crystals. The rock becomes very dense and heavy. Some examples are Quartzite and Marble. ]]> 2019-04-01 23:46:33 UTC https://padlet.com/420182/s3jqk0ppx808/wish/347420536 420182 https://padlet.com/420182/s3jqk0ppx808/wish/347422936 https://geology.com/rocks/pictures/muscovite-schist.jpg]]> 2019-04-02 00:04:53 UTC https://padlet.com/420182/s3jqk0ppx808/wish/347422936 420182 https://padlet.com/420182/s3jqk0ppx808/wish/347423146 https://geology.com/rocks/pictures/marble.jpg]]> 2019-04-02 00:06:20 UTC https://padlet.com/420182/s3jqk0ppx808/wish/347423146