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EESA06H3 (234)
Lisa Tutty (13)
Chapter 4

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Department
Environmental Science
Course
EESA06H3
Professor
Lisa Tutty
Semester
Winter

Description
Chapter 4 – Sedimentary & Metamorphic Source: other rocks. Sediments formed from the wearing down of other rocks. Eg sand, ions in solution, animal shells Process: deposition, precipitation (things coming out of a solution) and cemented Product: sedimentary rocks. Eg Limestone is found in coral reefs Processes Compaction: When cement piles on top of one another, it gets squished and there’s less air between the grains and they get compacted. Eg: loose sediments like sand turned into a sedimentary rock Cementation: Something sticky is able to stick the grains together. Often, it is silica or calcite cement that sticks them together that turns them from loose sediment into a rock Lithification - turning sediments into rocks Depositional environment aka as environment of formation: Different places where sediments gather together and form sedimentary rocks. Common ones are a beach. You mostly find sediments such as sand. A sedimentary rock found on the beach would be a sandstone. In the deep water there are sediments such as clay or silt. They form a mudstone of shale. Clay forms shale. Clastic sediments- broken parts of other rocks. Sand, silt, pebbles, boulders are examples of clastic sediments. They make clastic sedimentary rocks. Using this you can make chemical or biological rocks. You can form limestone from coral reefs. This would be biological or biochemical sedimentary rocks. Making sedimentary rocks: Read in detail 7.3, 15.1 - 15.4 1) Physical weathering and 2) chemical weathering. Igneous rocks need to undergo weathering in order to be turned into sediments. Clastic sediments are moved and deposited by water, wind and glaciers. Clastic sediments named by size (clay, silt, sand, pebbles, boulders) Clastic sediments are named by grain size (mudstone/shale, sandstone, conglomerate) Conglomerate: made of a mixture of sediments larger than sand. How round and angular a rock tells us their distance of traveling When you transport sediments, the further distance you transport it, there's more chance for it to get rubbed and eroded against each other and as a result they get rounded and smooth. Eg: on a beach But the rocks on a mountain would be angular and sharp because they haven't really travelled far. Clastic sedimentary rocks to know: Breccia: this word means broken. The pieces are angular clasts Conglomerate: more rounded clasts than breccia sandstone Sandstone is formed by sand moving by wind or water such as sand dunes and beach ripples Shale – soft sedimentary rock that is easy to erode. Siltstone: finer than sandstone, clastic, silt sized particles Non clastic sedimentary rocks to know: (precipitate by water or deposited by organisms) BIF - banded iron formation Gypsum – walls in our house. Evaparoite. Dolostone – similar to limestone. It has MG and CA Halite – used on French fries, on driveways during snow Limestone – Its clastic, sedimentary or chemical. Made up of creatures & bits that make up the C reef. You could also precipitate the mineral from the water. Evaporates can form in shallow, restricted basins surrounded by fringing reefs: Sea water evaporates rapidly, precipitating salts. Can form minerals if water evaporates. Eg: halite, gypsum Biogenic sedimentary rocks - Marine organisms - limestone, chalk Loose sediments: - show structures (Ex ripples - how/where sediment was deposited). They need to be lithified as in be made into rock. Graded bedding – sediments sorted by gra
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