Chapter 8: Earth’s Systems & Resources
Description:
The earth is 4.5 Billion years old and has been through incredible changes. In this unit, we will look at the natural processes that change the earth over time, and how those changes can benefit and threaten humans. We will also examine Earth’s mineral, soil and water resources, as well as current issues regarding sustainable use of these resources and providing access for all people.
Unit Focus Question:
Packet Contents:
Assignment |
Due: |
1. Reading Questions 8A, Vocab List 8A, Video Questions 8A |
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2. Reading Questions 8B, Vocab List 8B, Video Questions 8B |
Chapter 8 Vocabulary List
Core |
the innermost layer of earth |
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Mantle |
layer of earth above core, magma |
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Asthenosphere |
layer of earth in outer part of mantle, semi molten rock |
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Lithosphere |
outermost layer of earth, mantle and crust |
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Crust |
outermost layer of the lithosphere |
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Hot spots |
place where molten material reaches the lithosphere |
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Tectonic plates |
plates that shift under earths surface |
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Subduction |
one plate going under another |
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Divergent boundary |
where tectonic plates move away from each other |
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Convergent boundary |
where tectonic plates move toward each other |
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Transform boundary |
where tectonic plates move past each other |
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Fault zones |
rock where a fault has occurred |
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Earthquake |
shaking of earth's surface when potential energy is released and earths |
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crust moves |
Richter scale |
scale to measure the magnitude of an earthquake |
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Minerals |
solid chemical that forms under certain temperatures and pressures |
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Igneous rocks |
rock formed by magma |
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Sedimentary rocks |
rock formed when sediments are compressed |
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Metamorphic rocks |
rock formed when in high temperature and pressure |
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Physical weathering |
mechanical breakdown of rocks and minerals |
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Chemical weathering |
break down of rocks and minerals by chemical reaction |
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Erosion |
physical removal of rock fragments |
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Deposition |
accumulation or depositing of eroded material |
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Soil |
mix of geologic and organic components that form a dynamic membrane |
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around earths surface |
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Parent material |
rock underlying soil, where soil is derived |
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Topography |
lines on a map that indicate distance from sea level |
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O horizon |
organic detritus in various stages of decomposition |
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A horizon |
top layer of soil. organic and mineral material |
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E horizon |
under O or A horizon, zone of leaching |
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B horizon |
mineral material with very little organic material |
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C horizon |
least weathered, beneath the B horizon, like parent material |
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Soil texture |
percentage of clay, silt, and sand in a soil |
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CEC of a soil |
number of exchangeable cations per dry weight that soil is capable of |
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holding |
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Base saturation |
proportion of soil basses to soil acids, percent |
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Soil degradation |
loss of soils ability to support plant life |
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Ores |
concentrated accumulation of minerals where valuable material can be |
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extracted |
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Metals |
element with properties that allow it to conduct electricity and heat |
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energy and other important features |
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Known reserves |
fossil fuel energy source |
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Strip mining |
removal of strips of soil and rock to expose ore |
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Tailings |
unwanted waste materials created during mining |
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Open-pit mining |
surface mining technique by removing from an open pit or borrow |
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Subsurface mining |
mining technique used when desired resource is more than 100 m |
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below |
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SMRCA law |
regulates environmental effects of coal mining |
Reading Questions 8A
The cars are made out of scarce metals and the metal must is shipped over from other countries since they’re not mined in the U.S. Also the mining that is done to get the metals is very damaging to the environment plus they still use up a form of energy that was at one point most likely burned coal.
When the earth was forming the heavier elements sank to the center of the earth while the lighter elements floated to the surface. Heavier elements are located closer to the center of the earth and lighter elements are located near the earths surface.
Crust – outermost layer of the lithosphere, we walk on it
Mantle – layer of earth above core, magma
Core – the innermost layer of earth, ball of iron
The heat from the earths core causes convection currents which causes the movement of the tectonic plates
He saw identical rock formations on both sides of the Atlantic ocean
Oceanic – part of earth's lithosphere that surfaces in the ocean basin, heavy and dense Continental – layer of igneous, sedimentary, and metamorphic rocks which forms continents, relatively light
I think that the continent would be split in the middle between North and South by a ridge or river causing the species to grow differently on either side,ultimately the Northern part of the continent would have less species density because its colder then the tropics
the Islands were created by a volcano that was created by two tectonic plates, as the volcano released magma islands were formed, the whole time the tectonic plates continued to move slowly carrying the islands away from the hot spot
At a convergent plate boundary where oceanic crust meets continental crust a long coastal mountain range will form when the oceanic plate slides under the continental plate lifting the continental plate
Plates that move past each other on a transform plate boundary can cause earthquakes.
An 8.0 earthquake is 100,000 times stronger than a 4.0 earthquake on the Richter scale each number high is 10 times stronger
Volcanos are often located on a fault line where two plates meet
minerals are made up of a single element and rocks are made up of minerals
Igneous rocks and sedimentary rocks form on their own but metamorphic rocks can form from pre existing igneous and sedimentary rocks so there really isn't a particular order in which they form.
physical weathering is the mechanical break down of rocks and minerals, like rain, while chemical weathering is the breakdown of rocks and minerals by chemical reaction like plants.
processes such as weathering, physical and chemical weathering cause erosion, it is also caused by the forces of wind, water, and ice as well as lack of plants because plant roots help hold together soil
weathering and erosion are important to the rock cycle because they help recycle minerals, chemicals and other elements back into the crust and just mix up the soil.
Reading Questions 8B
the breakdown of rocks and primary minerals by weathering provides raw material for sol from below. the decomposition of organic matter from organisms and their waste contributes to soil formation from above.
when soil is in cold/ freezing weather there is little to no decomposition, soil in high altitudes are composed primarily of organic matter that is undecomposed. while soil in tropical temperatures have an acceleration of soil formation because of the weathering of rocks , leaching of nutrients and decomposition of animals, climate also has an indirect effect on soil by influencing the types of vegetation that can grow in the area changing the roots. Boreal forests are colder so the roots of tree must run deep to provide the nutrients while a tropical rain forest is hot and humid so the decomposition of animals is fast allowing for small plants and small roots.
plants remove nutrients from soil but speed up chemical weathering, animals such as worms and gophers tunnel and mix dirt distributing organic and mineral matter uniformly,
horizons are classified by their properties and their functions, they depend on climate, vegetation and parent material; depth of the soil is what can separate one horizon from another
a balance is needed in order for the soil to retain water and let water drain out of it, if soil was sand-heavy then water would easily drain out of it or if soil was clay-heavy then water could not filer through it and plant roots would struggle.
a soil that would be good to line a pit containing hazardous chemicals would be clay because it won't let the chemicals pass through it.
during absorption clay particles are positively charged and attract minerals on the surface “cations” which are negatively charged.
no because CEC means having a lot of clay which then provides minerals to plants however having high CEC means more clay so if you have a lot of clay then a soil can not be porse.
Base saturation is the measure of how much bases to acids there is in the soil represented as a percentage, a high base saturation promotes plant growth as well as a good CEC.
fungi, bacteria and protozoans
compact soil lacks the ability to retain water,reduces the amount of vegetation in the soil which leads to an increase in erosion.
silicon and oxygen
ore veins are small areas with a high concentration of a mineral or metal while disseminating deposits are much larger areas with a smaller concentration. ore veins are easier to mine because its in a small area and its closely packed together.
1.strip mining: removal of strips of soil to expose ores, deep. This can cause the ph of the soil to increase as the miners have to pump water out of the mine
3.Mountaintop removal: miners use explosives and large machinery to literally remove the top of a mountain to extract minerals. the spoils of this are dumped in streams or rivers polluting the water.
extracting deposits of a certain resource increase over time because of a growing demand for cheaper resources, so as one mine closes two more have to open to met the demand.
land be minimally disturbed during the mining process and reclaimed after mining is completed meaning the land is restored.
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