Unit 5 Planet Earth.

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Presentation transcript:

Unit 5 Planet Earth

Unit 5 Topic 1 - Minerals

Minerals Rocks contain naturally occurring, non-living minerals Most minerals are rare and can be elements (pure substances) or compounds (combinations of pure substances) Minerals are not only found in rocks, but they are also found in your body

Now everyone will know how minerals are! Mohs’ Hardness Scale Friedrich Mohs developed a scale with 10 values of 'hardness' in 1812 (see Table 5.1 p. 355) Diamond is the hardest and talc is the softest

Crystals Crystals are the building blocks of minerals They occur naturally, having straight edges, flat sides and straight angles There are 6 different crystal types… Cubic Tetragonal Hexagonal Orthohombic Monoclinic Triclinic (Table 5.2 p. 355)

Identification of Minerals The properties that can be used to identify minerals are… - Lustre This refers to the 'shininess' of the mineral (how light is reflected off the surface) Colour Colour can vary even within the same mineral, like corundum (it can be white, blue or red), depending on what other elements are present Streak A streak is the color, of the powdered form, of the mineral

Identification of Minerals Cleavage and Fracture Is the way a mineral breaks apart If it breaks along smooth, flat surfaces or planes, it has cleavage If it breaks with rough or jagged edges, it has fracture Transparency it can be transparent (see through) or translucent (shadowy), opaque (non-see through).

Applications of Minerals … Iron and pyrite help the blood carry oxygen Kidneys produce crystals, called kidney stones Calcium and dolomite help regulate water in body cells Diamonds are used in surgery, razor blades, computers, dentistry, oil drilling and a glass- cutter's wheel has diamonds embedded in it.

Topic 2 – Rocks & Rock Cycles Unit 5 Topic 2 – Rocks & Rock Cycles

Rock Classifications Rocks can be classified into 3 different groups … 1) Igneous Rock 2) Sedimentary Rock 3) Metamorphic Rock

Igneous Rock Forms when hot magma (lava) cools and solidifies Magma is melted rock found below the Earth's crust Types of Igneous rock are… Intrusive Cooled and hardened magma below the Earth's surface Extrusive Rock that forms when lava - magma released during a volcanic eruption - cools on the surface Magma can contain crystals, their size depending on how quickly or slowly the rock cools (Ex: large crystals form when the rock cools slowly)

Igneous Rocks - Formation

Igneous Rocks – Maybe?

Sedimentary Rock Is formed from sediment Stratification Cementation Loose material - rock, minerals, plant and animal remains - that is layered and compacted together by the pressure of the material above it  Stratification  Is the visible evidence of the layers Cementation  Some of the minerals that dissolve with the addition of water, makes a natural cement that glues the pieces of sediment together

Sedimentary Rocks - Formation

Sedimentary Rock Cont … Types of sedimentary rock include: Shale Formed from fine clay or mud Sandstone Sand, made of quartz Conglomerate Pebbles and small stones cemented together Limestone Organic sedimentary rock, containing fossils - plant and animal remains

Metamorphic Rock This type of rock has changed its form from what it was originally It is formed below the Earth's surface by extreme pressure and heat The parent rock will become another type of rock depending on how much pressure and heat is used to change it Ex: Shale  Slate  Schist

Metamorphic Rock - Formation

Rock Cycle Rocks are constantly changing. The Rock Cycle does not have a set order as they are weathered, consolidated, buried, melted and solidified

Techniques for Identifying Rocks Appearance Type of mineral(s) present Viewed through a microscope

Sediment & Soil Some sediment becomes soil Soil formation is determined by climate, type of rock present, amount of water, organic material, air spaces, living organisms in the soil Decaying material in the soil is called compost, when mixed with other matter, it becomes the dark- coloured portion of the soil called humus Humus is rich in nitrogen, phosphorus, sulphur and potassium, which dissolve in water, making the soil fertile (supplying nutrients for plant growth)

Soil Profiles Soil forms slowly over time It has been classified into layers, giving it a soil profile! Topsoil  Dark rich soil containing humus and small grains of rock Subsoil  Lighter in colour with little or no humus - contains minerals that have been leached from the topsoil & Leaching is the removal of materials in the soil that can be dissolved in water The bottom layer contains partly weathered rock and minerals leached from above and closely resembles the parent rock below it.

How Good Is My Soil?