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Unit 3 Rocks, Soil, Erosion and Mass Movements. Including the Geological History of North Carolina!. Classification of Rock. Most rocks have a number of minerals in common. Rocks are grouped on the basis of their physical and chemical properties, but most importantly, their origin.

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Unit 3 rocks soil erosion and mass movements

Unit 3 Rocks, Soil, Erosion and Mass Movements

Including the Geological History of North Carolina!


Classification of Rock

Most rocks have a number of minerals in common. Rocks are grouped on the basis of their physical and chemical properties, but most importantly, their origin.

1. Sedimentary Rocks

Most form under water. Layering (“stratification”) will indicate this.


Classification of Rock

Most rocks have a number of minerals in common. Rocks are grouped on the basis of their physical and chemical properties, but most importantly, their origin.

1. Sedimentary Rocks

Most form under water. Layering (“stratification”) will indicate this.

Sedimentary rocks are classified according to the way they were formed


Classification of Rock

Most rocks have a number of minerals in common. Rocks are grouped on the basis of their physical and chemical properties, but most importantly, their origin.

1. Sedimentary Rocks

Most form under water. Layering (“stratification”) will indicate this.

Sedimentary rocks are classified according to the way they were formed and what was deposited:


Classification of Rock

Most rocks have a number of minerals in common. Rocks are grouped on the basis of their physical and chemical properties, but most importantly, their origin.

1. Sedimentary Rocks

Most form under water. Layering (“stratification”) will indicate this.

Sedimentary rocks are classified according to the way they were formed and what was deposited:

A. Clastics – weathered particles from pre-existing rocks


Classification of Rock

Most rocks have a number of minerals in common. Rocks are grouped on the basis of their physical and chemical properties, but most importantly, their origin.

1. Sedimentary Rocks

Most form under water. Layering (“stratification”) will indicate this.

Sedimentary rocks are classified according to the way they were formed and what was deposited:

A. Clastics – weathered particles from pre-existing rocks

The particles were lithified


Classification of Rock

Most rocks have a number of minerals in common. Rocks are grouped on the basis of their physical and chemical properties, but most importantly, their origin.

1. Sedimentary Rocks

Most form under water. Layering (“stratification”) will indicate this.

Sedimentary rocks are classified according to the way they were formed and what was deposited:

A. Clastics – weathered particles from pre-existing rocks

The particles were lithified (turned into rock) by:


Classification of Rock

Most rocks have a number of minerals in common. Rocks are grouped on the basis of their physical and chemical properties, but most importantly, their origin.

1. Sedimentary Rocks

Most form under water. Layering (“stratification”) will indicate this.

Sedimentary rocks are classified according to the way they were formed and what was deposited:

A. Clastics – weathered particles from pre-existing rocks

The particles were lithified (turned into rock) by: compaction – great pressure from


Classification of Rock

Most rocks have a number of minerals in common. Rocks are grouped on the basis of their physical and chemical properties, but most importantly, their origin.

1. Sedimentary Rocks

Most form under water. Layering (“stratification”) will indicate this.

Sedimentary rocks are classified according to the way they were formed and what was deposited:

A. Clastics – weathered particles from pre-existing rocks

The particles were lithified (turned into rock) by: compaction – great pressure from the layers of sediment above. It can only work if the sediments are


Classification of Rock

Most rocks have a number of minerals in common. Rocks are grouped on the basis of their physical and chemical properties, but most importantly, their origin.

1. Sedimentary Rocks

Most form under water. Layering (“stratification”) will indicate this.

Sedimentary rocks are classified according to the way they were formed and what was deposited:

A. Clastics – weathered particles from pre-existing rocks

The particles were lithified (turned into rock) by: compaction – great pressure from the layers of sediment above. It can only work if the sediments are small (e.g. shale & siltstone from clay and silt)


Cementation – is needed for larger particles.


Cementation – is needed for larger particles. A cement (a mineral that dissolves in water - - CaCO3) holds the sediments together


Cementation – is needed for larger particles. A cement (a mineral that dissolves in water - - CaCO3) holds the sediments together (e.g. sandstone & conglomerate from sand & pebbles).


Cementation – is needed for larger particles. A cement (a mineral that dissolves in water - - CaCO3) holds the sediments together (e.g. sandstone & conglomerate from sand & pebbles).

Clastics are usually stratified,


Cementation – is needed for larger particles. A cement (a mineral that dissolves in water - - CaCO3) holds the sediments together (e.g. sandstone & conglomerate from sand & pebbles).

Clastics are usually stratified, and often contain fossils.


Cementation – is needed for larger particles. A cement (a mineral that dissolves in water - - CaCO3) holds the sediments together (e.g. sandstone & conglomerate from sand & pebbles).

Clastics are usually stratified, and often contain fossils.


Cementation – is needed for larger particles. A cement (a mineral that dissolves in water - - CaCO3) holds the sediments together (e.g. sandstone & conglomerate from sand & pebbles).

Clastics are usually stratified, and often contain fossils.


Cementation – is needed for larger particles. A cement (a mineral that dissolves in water - - CaCO3) holds the sediments together (e.g. sandstone & conglomerate from sand & pebbles).

Clastics are usually stratified, and often contain fossils. These help indicate what conditions existed at the time of sedimentation.


Cementation – is needed for larger particles. A cement (a mineral that dissolves in water - - CaCO3) holds the sediments together (e.g. sandstone & conglomerate from sand & pebbles).

Clastics are usually stratified, and often contain fossils. These help indicate what conditions existed at the time of sedimentation.

  • Chemical Sedimentary rocks formed from material that was


Cementation – is needed for larger particles. A cement (a mineral that dissolves in water - - CaCO3) holds the sediments together (e.g. sandstone & conglomerate from sand & pebbles).

Clastics are usually stratified, and often contain fossils. These help indicate what conditions existed at the time of sedimentation.

  • Chemical Sedimentary rocks formed from material that was dissolved in the water.


Cementation – is needed for larger particles. A cement (a mineral that dissolves in water - - CaCO3) holds the sediments together (e.g. sandstone & conglomerate from sand & pebbles).

Clastics are usually stratified, and often contain fossils. These help indicate what conditions existed at the time of sedimentation.

  • Chemical Sedimentary rocks formed from material that was dissolved in the water. When the water gets saturated, the minerals precipitate out and form solid rock layers.


Cementation – is needed for larger particles. A cement (a mineral that dissolves in water - - CaCO3) holds the sediments together (e.g. sandstone & conglomerate from sand & pebbles).

Clastics are usually stratified, and often contain fossils. These help indicate what conditions existed at the time of sedimentation.

  • Chemical Sedimentary rocks formed from material that was dissolved in the water. When the water gets saturated, the minerals precipitate out and form solid rock layers.

alabaster


Cementation – is needed for larger particles. A cement (a mineral that dissolves in water - - CaCO3) holds the sediments together (e.g. sandstone & conglomerate from sand & pebbles).

Clastics are usually stratified, and often contain fossils. These help indicate what conditions existed at the time of sedimentation.

  • Chemical Sedimentary rocks formed from material that was dissolved in the water. When the water gets saturated, the minerals precipitate out and form solid rock layers.

alabaster

limestone


Cementation – is needed for larger particles. A cement (a mineral that dissolves in water - - CaCO3) holds the sediments together (e.g. sandstone & conglomerate from sand & pebbles).

Clastics are usually stratified, and often contain fossils. These help indicate what conditions existed at the time of sedimentation.

  • Chemical Sedimentary rocks formed from material that was dissolved in the water. When the water gets saturated, the minerals precipitate out and form solid rock layers. Evaporites will form if the rate of evaporation is great.


Cementation – is needed for larger particles. A cement (a mineral that dissolves in water - - CaCO3) holds the sediments together (e.g. sandstone & conglomerate from sand & pebbles).

Clastics are usually stratified, and often contain fossils. These help indicate what conditions existed at the time of sedimentation.

  • Chemical Sedimentary rocks formed from material that was dissolved in the water. When the water gets saturated, the minerals precipitate out and form solid rock layers. Evaporites will form if the rate of evaporation is great.

halite


Cementation – is needed for larger particles. A cement (a mineral that dissolves in water - - CaCO3) holds the sediments together (e.g. sandstone & conglomerate from sand & pebbles).

Clastics are usually stratified, and often contain fossils. These help indicate what conditions existed at the time of sedimentation.

  • Chemical Sedimentary rocks formed from material that was dissolved in the water. When the water gets saturated, the minerals precipitate out and form solid rock layers. Evaporites will form if the rate of evaporation is great.

  • All chemical sedimentary rocks are monomineralic.





Oolitic limestone


Oolitic limestone


Oolitic limestone



2. Nonsedimentary Rocks processes (decay of plant material [e.g. coal] or cementing of shell material [e.g. fossil limestone]). The shell material, however, is not organic.


2. Nonsedimentary Rocks processes (decay of plant material [e.g. coal] or cementing of shell material [e.g. fossil limestone]). The shell material, however, is not organic.

A. Igneous -


2. Nonsedimentary Rocks processes (decay of plant material [e.g. coal] or cementing of shell material [e.g. fossil limestone]). The shell material, however, is not organic.

  • Igneous - form as lava or magma cools & solidifies.


2. Nonsedimentary Rocks processes (decay of plant material [e.g. coal] or cementing of shell material [e.g. fossil limestone]). The shell material, however, is not organic.

  • Igneous - form as lava or magma cools & solidifies.

1. Intrusive (plutonic) rocks formed


2. Nonsedimentary Rocks processes (decay of plant material [e.g. coal] or cementing of shell material [e.g. fossil limestone]). The shell material, however, is not organic.

  • Igneous - form as lava or magma cools & solidifies.

  • Intrusive (plutonic) rocks formed under the earth’s surface.


2. Nonsedimentary Rocks processes (decay of plant material [e.g. coal] or cementing of shell material [e.g. fossil limestone]). The shell material, however, is not organic.

  • Igneous - form as lava or magma cools & solidifies.

  • Intrusive (plutonic) rocks formed under the earth’s surface. It usually takes a long time to cool, so the minerals crystallize at different temperatures and separate.


2. Nonsedimentary Rocks processes (decay of plant material [e.g. coal] or cementing of shell material [e.g. fossil limestone]). The shell material, however, is not organic.

  • Igneous - form as lava or magma cools & solidifies.

  • Intrusive (plutonic) rocks formed under the earth’s surface. It usually takes a long time to cool, so the minerals crystallize at different temperatures and separate. Dark colors (mafic) harden first (higher temp); while light colors (felsic) harden last.


2. Nonsedimentary Rocks processes (decay of plant material [e.g. coal] or cementing of shell material [e.g. fossil limestone]). The shell material, however, is not organic.

  • Igneous - form as lava or magma cools & solidifies.

  • Intrusive (plutonic) rocks formed under the earth’s surface. It usually takes a long time to cool, so the minerals crystallize at different temperatures and separate. Dark colors (mafic) harden first (higher temp); while light colors (felsic) harden last.

  • The longer it takes for magma to cool, the _____ the crystals will be


2. Nonsedimentary Rocks processes (decay of plant material [e.g. coal] or cementing of shell material [e.g. fossil limestone]). The shell material, however, is not organic.

  • Igneous - form as lava or magma cools & solidifies.

  • Intrusive (plutonic) rocks formed under the earth’s surface. It usually takes a long time to cool, so the minerals crystallize at different temperatures and separate. Dark colors (mafic) harden first (higher temp); while light colors (felsic) harden last.

  • The longer it takes for magma to cool, the larger the crystals will be (coarse grained).


Intrusive Igneous Rocks processes (decay of plant material [e.g. coal] or cementing of shell material [e.g. fossil limestone]). The shell material, however, is not organic.

granite


Intrusive Igneous Rocks processes (decay of plant material [e.g. coal] or cementing of shell material [e.g. fossil limestone]). The shell material, however, is not organic.

diorite


Intrusive Igneous Rocks processes (decay of plant material [e.g. coal] or cementing of shell material [e.g. fossil limestone]). The shell material, however, is not organic.

gabbro


Intrusive Igneous Rocks processes (decay of plant material [e.g. coal] or cementing of shell material [e.g. fossil limestone]). The shell material, however, is not organic.

Pegmatite




All molten rock originates in the upper mantle and lower crust. Heat comes from pressure and radioactive decay of the materials deep within the earth.


All molten rock originates in the upper mantle and lower crust. Heat comes from pressure and radioactive decay of the materials deep within the earth. When magma is forced through cracks in the bedrock, intrusions are formed.


All molten rock originates in the upper mantle and lower crust. Heat comes from pressure and radioactive decay of the materials deep within the earth. When magma is forced through cracks in the bedrock, intrusions are formed.


All molten rock originates in the upper mantle and lower crust. Heat comes from pressure and radioactive decay of the materials deep within the earth. When magma is forced through cracks in the bedrock, intrusions are formed. If cracks lead to the surface, extrusions are formed (volcanoes).


All molten rock originates in the upper mantle and lower crust. Heat comes from pressure and radioactive decay of the materials deep within the earth. When magma is forced through cracks in the bedrock, intrusions are formed. If cracks lead to the surface, extrusions are formed (volcanoes).


2. crust. Heat comes from pressure and radioactive decay of the materials deep within the earth. When magma is forced through cracks in the bedrock, Extrusive (eruptive or volcanic) rocks form from


  • Extrusive (eruptive crust. Heat comes from pressure and radioactive decay of the materials deep within the earth. When magma is forced through cracks in the bedrock, orvolcanic) rocks form from lava that cooled on the surface.


  • Extrusive (eruptive crust. Heat comes from pressure and radioactive decay of the materials deep within the earth. When magma is forced through cracks in the bedrock, orvolcanic) rocks form from lava that cooled on the surface. Small crystal grains indicate that it cooled


  • Extrusive (eruptive crust. Heat comes from pressure and radioactive decay of the materials deep within the earth. When magma is forced through cracks in the bedrock, orvolcanic) rocks form from lava that cooled on the surface. Small crystal grains indicate that it cooled quickly.

basalt

Lava cooling into basalt


  • Extrusive (eruptive crust. Heat comes from pressure and radioactive decay of the materials deep within the earth. When magma is forced through cracks in the bedrock, orvolcanic) rocks form from lava that cooled on the surface. Small crystal grains indicate that it cooled quickly. Glassy texture shows it cooled very fast (usually under water).


  • Extrusive (eruptive crust. Heat comes from pressure and radioactive decay of the materials deep within the earth. When magma is forced through cracks in the bedrock, orvolcanic) rocks form from lava that cooled on the surface. Small crystal grains indicate that it cooled quickly. Glassy texture shows it cooled very fast (usually under water).

obsidian


  • Extrusive (eruptive crust. Heat comes from pressure and radioactive decay of the materials deep within the earth. When magma is forced through cracks in the bedrock, orvolcanic) rocks form from lava that cooled on the surface. Small crystal grains indicate that it cooled quickly. Glassy texture shows it cooled very fast (usually under water).

  • Sometimes the lava is ejected onto the surface and cools with gases trapped inside pockets (“vesicles”) in the rock.

pumice


B. Metamorphic Rock – used to be crust. Heat comes from pressure and radioactive decay of the materials deep within the earth. When magma is forced through cracks in the bedrock,




1. Regional – occurs over wide areas,


  • Regional – occurs over wide areas, usually due to extreme temperature and pressure conditions.


  • Regional – occurs over wide areas, usually due to extreme temperature and pressure conditions. This happens deep within the crust, usually due to mountain building processes.

slate


  • Regional – occurs over wide areas, usually due to extreme temperature and pressure conditions. This happens deep within the crust, usually due to mountain building processes.

slate

(used to be shale; the pressure made it darker & denser, the shale layers became foliated)


  • Regional – occurs over wide areas, usually due to extreme temperature and pressure conditions. This happens deep within the crust, usually due to mountain building processes.

quartzite


  • Regional – occurs over wide areas, usually due to extreme temperature and pressure conditions. This happens deep within the crust, usually due to mountain building processes.

quartzite

(used to be sandstone; the “scaliness” is from the distorted sand grains)


  • Regional – occurs over wide areas, usually due to extreme temperature and pressure conditions. This happens deep within the crust, usually due to mountain building processes.

gneiss


  • Regional – occurs over wide areas, usually due to extreme temperature and pressure conditions. This happens deep within the crust, usually due to mountain building processes.

gneiss

(used to be granite; the heat & pressure made the minerals recrystallize and form bands)


  • Contact they were changed as a result of heat, pressure and/or chemical changes. (thermal) – occurs at the interface of hot magma and existing rock.


  • Contact they were changed as a result of heat, pressure and/or chemical changes. (thermal) – occurs at the interface of hot magma and existing rock. Chemical changes forming new minerals often occur.

Pix of meta rocks

Quartzite (used to be sandstone)


  • Contact they were changed as a result of heat, pressure and/or chemical changes. (thermal) – occurs at the interface of hot magma and existing rock. Chemical changes forming new minerals often occur.

Marble bookends (used to be limestone)

More pix of meta



We can learn a lot about the environment when rock formed by looking at its composition,

What can we infer from this rock?

Pix of conglom


We can learn a lot about the environment when rock formed by looking at its composition,

Large rounded particles imply that this conglomerate formed from sediment at the mouth of a river.

Pix of conglom


We can learn a lot about the environment when rock formed by looking at its composition, structure,

Foliation in this schist implies that the basalt underwent tremendous pressure deep under the surface.

Pix of schist


We can learn a lot about the environment when rock formed by looking at its composition, structure and texture.

The course grains in this diorite implies that it cooled deep within the crust.


We can learn a lot about the environment when rock formed by looking at its composition, structure and texture.

The course grains in this diorite implies that it cooled deep within the crust.

The glassy luster in this obsidian implies that it cooled quickly, most likely under water.

Pix of obsidian


The Rock Cycle looking at its composition, structure and texture.


The Rock Cycle looking at its composition, structure and texture.

There is evidence that rocks continue to be “recycled”


The Rock Cycle looking at its composition, structure and texture.

There is evidence that rocks continue to be “recycled” - sedimentation & sedimentary rocks


The Rock Cycle looking at its composition, structure and texture.

There is evidence that rocks continue to be “recycled”

- sedimentation & sedimentary rocks

- similarities between metamorphic & other rocks


The Rock Cycle looking at its composition, structure and texture.

There is evidence that rocks continue to be “recycled”

- sedimentation & sedimentary rocks

- similarities between metamorphic & other rocks


The Rock Cycle looking at its composition, structure and texture.

There is evidence that rocks continue to be “recycled”

- sedimentation & sedimentary rocks

- similarities between metamorphic & other rocks

- transition zones from unaltered to altered rock can be found where magma came in contact with local rock


The Rock Cycle looking at its composition, structure and texture.

There is evidence that rocks continue to be “recycled”

- sedimentation & sedimentary rocks

- similarities between metamorphic & other rocks

- transition zones from unaltered to altered rock can be found where magma came in contact with local rock

- lava can be seen cooling into igneous rock


The Rock Cycle looking at its composition, structure and texture.

There is evidence that rocks continue to be “recycled”

- sedimentation & sedimentary rocks

- similarities between metamorphic & other rocks

- transition zones from unaltered to altered rock can be found where magma came in contact with local rock

- lava can be seen cooling into igneous rock


The Rock Cycle looking at its composition, structure and texture.

There is evidence that rocks continue to be “recycled”

- sedimentation & sedimentary rocks

- similarities between metamorphic & other rocks

- transition zones from unaltered to altered rock can be found where magma came in contact with local rock

- lava can be seen cooling into igneous rock

- the composition of sedimentary rocks suggest that they had varied origins

conglomerate


The Rock Cycle looking at its composition, structure and texture.

There is evidence that rocks continue to be “recycled”

- sedimentation & sedimentary rocks

- similarities between metamorphic & other rocks

- transition zones from unaltered to altered rock can be found where magma came in contact with local rock

- lava can be seen cooling into igneous rock

- the composition of sedimentary rocks suggest that they had varied origins

- some rocks show multiple transformations


The Rock Cycle looking at its composition, structure and texture.

There is evidence that rocks continue to be “recycled”

- sedimentation & sedimentary rocks

- similarities between metamorphic & other rocks

- transition zones from unaltered to altered rock can be found where magma came in contact with local rock

- lava can be seen cooling into igneous rock

- the composition of sedimentary rocks suggest that they had varied origins

- some rocks show multiple transformations

- the age of rocks ≠ the age of the earth


Oceanic igneous rocks tend to be in the basalt family looking at its composition, structure and texture.



Oceanic igneous rocks tend to be in the basalt family (darker & denser), while continental igneous rocks tend to be of the granite family


Oceanic igneous rocks tend to be in the basalt family (darker & denser), while continental igneous rocks tend to be of the granite family (lighter).

(Granitic)

(Basaltic)

Pix of crustal rock


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