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What are the different types of rocks
Igneous
Metamorphic
Sedimentary
What are intrusive rocks
Magma that displaces rock inside the crust
What are extrusive rocks
Magma that flows onto the surface
How are extrusive rocks formed
Lava cools on the earths surface
How are intrusive rocks formed
Magma cools on the inside of the earth
Characteristics of igneous rocks
Massive, it forms one large mass with no layers
Crystalline
Consists of many elements
When magma cools elements combine to form crystals and minerals
Elements that igneous rocks may consist of
Silica
Iron
Magnesium
Relation of how quickly magma cools to the size of the crystals of igneous rocks
Quickly cooling magma forms small crystals (extrusive rocks)
Slowly cooling magma forms large crystals (intrusive rocks)
Uses of igneous rocks
Contains valuable metals
Mining companies mine the metals if its economical
Building materials
Stone chips extracted from quarries reinforce cement
Work surfaces and gravestones are made from granite
Types of igneous rocks
Granite
Basalt
Dolerite
Granite characteristics
Intrusive
Magma cools slowly forming large crystals
What are the different types of granite
Quartz-glassy appearance
Mica- black, flaky appearance
Feldspar-large white/pink crystals
Characteristics of basalt
Extrusive
Cools quickly forming small crystals
Hard, black rock forming on the earth surface
Lava flows over the surface to form a plateau
Characteristics of dolerite
Intrusive
Magma cools slowly forming small crystals
Forms closer to the surface
Greenish appearance
Forms at the top of most flat-topped hills
The different intrusive igneous rocks features
Batholith
Laccolith
Lopolith
Sill
Dyke
Volcanic pipe
Monolith
Batholith
Largest type, forms deep within earths surface by cooling slowly (granite)
Laccolith
Mushroom shaped structure, forms when magma forces overlying layers upwards, cools moderately and has medium sized crystals
Lopolith
Saucer shaped. Caused by the weight of the overlying rock strata causing it to sink
Sill
Magma intrudes horizontally between laters along the bedding plane
Dyke
Magma intrudes vertically across the layers of rock
Volcanic pipe
Deep carrot shaped pipe of solidified magma and often contains diamonds
Monolith
Similar to a batholith, when exposed at the surface it formed a doomed rock
Characteristics of a granite dome
Forms from batholiths which are exposed at the surface
Softer rock layers above the batholith are eroded away leaving granite dome
Extent of the batholith can extend thousands of km2
Found in western and northern cape. E.g. paarlbeg
Landforms associated with igneous rocks
Granite domes
Tors
Characteristics of a tor
Form when a granite dome below the surface undergoes chemical weathering
Chemical weathering forms core stones
Less resistant sedimentary layers above core stones erode at the surface leaving piles of core stones and creating a stacked appearance
What are sedimentary rocks formed from
Layers of compressed sediments
What are sedimentary layers formed through
Mechanical processes ad compression and consolidation
Process of forming sedimentary rocks
Layers of broken down material are deposited on top of one another in layers called sediments. The combined weight of it and water compresses the layers till it eventually consolidates to form rock layers called strata
What separates layers in sedimentary rocks
Bedding planes
Characteristics of sedimentary rocks
Sediments of different sizes form in different areas
Layers can be bent and shaped as earth’s crust moves
Plants and animals can be preserved in layers to form fossils
Where are larger pebbles deposited in
Shallow water
Where are medium sized pebbles deposited
In deeper water
Where are fine pebbles deposited
In very deep water
Uses of sedimentary rocks
Building material
Dolomites and shale can be heated and crushed into a dine powder to form cement
Clay is used to build houses, make bricks and tiles
Shale is used for floors and decorative purposes
The different types of sedimentary rocks
Conglomerate
Sandstone
Shale
Limestone
Coal
Sandstone characteristics
Medium sized sediments accumulate in layers on the ocean floor
Beige colour
Layers are evident
Shale characteristics
Fine grained sediments become consolidated
Distinctive layers of various shades
Limestone characteristics
Organically consolidated layers
Formed from shells of marine animals
Shells are made of calcium carbonate/lime
Layers of crushed shells are consolidated to form limestone
Coal characteristics
Organically consolidated layers
Formed from dead plants and trees
Other rocks compressed the organic layers to form it
Conglomerate characteristics
Pebbles cemented together by fine grained sediments
Mixed texture with air spaces
Description of a plateau
Extensive flat/gently undulating area of land elevated above the surrounding terrain
Main characteristics of a plateau
Large areas with relatively flat top and steep sides
Example of a plateau
Karoo plateau
High veld plateau
Description of a mesas
Flat-topped with steep sides, smaller than a plateau, larger than a butte
Main characteristics of a mesa
Flat top, steep cliff like sides, isolated
Examples of a mesa
Carina on area
Namaqualand
Description of a butte
Isolated hill with steep, often vertical sides and often a small flat top
Characteristics of a butte
Smaller than a mesa; flat top significantly eroded
Example of a butte
Karoo region
Description of a pointed butte
Further eroded butte where the top is pointed rather than flat
Characteristics of a pointed butte
Steep, narrow, pointed peak
Example of a pointed butte
Some formations in the eastern cape and Karoo
Description of a conical hill
Hill shaped like a cone, typically the final stage of erosion of a plateau type landform
Characteristics of a conical hill
Rounded/pointed peak steep slopes
Examples of a conical hill
Scattered conical hills in the Karoo
Regional metamorphism
A large amount of pressure changes rocks
Contact metamorphism
Heat causes crystals to melt and form new crystals
Characteristics of metamorphic rocks
Appear in layers/bands
Hardest type of rock
Contain valuable metals/minerals
Uses of metamorphic rocks
Metals and minerals within can be mined
Crushed gneiss is used to build roads
Thinly layer rocks such as slate are used for roof and floor tiles
Gem stones are polished for jewelry and decoration
Marble is used as a material for sculpting
Marble characteristics
Originally limestone
Made of recrystallized calcite
Can be polished
Relatively soft
Smooth
Often pink, white or grey
Crystalline
Shiny
Characteristics of quartzite
Originally sandstone
Usually light coloured: white, grey or pink
Very hard
Formed from quartz grains fused together under heat and pressure
How does metamorphic rocks change into igneous rock
It melts into magma and then cools
How does sedimentary rock change into metamorphic rock
It undergoes heat and pressure
How does igneous rock change into metamorphic rock
It undergoes heat and pressure
How does igneous rock change into sedimentary rock
It undergoes weathering and erosion to form sediments which are then compacted and cemented
How do sediments change into sedimentary rocks
It is compacted and cemented
How does metamorphic rocks change into sediments
It undergoes weathering and erosion
Slate characteristics
Fine grained
Splits easily into flat sheets
Formed under low grade metamorphism
Dull To slightly shiny
Layered in appearance
Originates from shale
How does igneous rock change into magma
It melts
Why is it called the rock cycle
Rocks are always changing from one type to another in a continuous never ending process
What is erosion
land, soil, and rocks are worn away and transported by natural forces like wind, water, and ice
What is weathering
the natural process of breaking down rocks and minerals on the Earth's surface, primarily by physical and chemical means. This process does not involve the movement of the broken-down material,
Characteristics of gneiss
Originates from granite
Coarse grained
Shows banding due to mineral segregation under high pressure
Alternating light and dark bands]looks striped
The different types of metamorphic rocks
Quartzite
Marble
Slate
Gneiss