Download Geology and Nonrenewable Mineral Resources - RHS-APES

Geology and Nonrenewable Mineral Resources
Objectives
1.
Briefly describe the layers of the earth's interior. Describe the internal and external earth processes responsible
for forming earth's landscape. Be sure to distinguish three different tectonic plate boundaries and the geologic
features often found at each. Explain how this knowledge is significant for understanding mineral deposits and
evolution.
2.
Distinguish between internal and external geologic processes. Discuss how these processes affect human
activities and natural ecosystems.
3.
List and define three broad classes of rock. Briefly describe the rock cycle and indicate interrelationships
among these classes.
4.
Describe how earthquakes are caused. Describe how tsunamis are formed. Describe the role of volcanoes in
the rock recycling process.
5.
List three types of mineral resources, and give one example of each. Clarify the relationship between identified
resources and reserves.
6.
Distinguish between subsurface and surface mining. Briefly describe the environmental impacts of mining.
7.
Draw a hypothetical depletion curve. Project how this curve would be affected by the following changes in
assumptions: (a) recycling of the resource is increased, (b) discoveries of new deposits of the resource are
made, (c) prices rise sharply, (d) a substitute for the resource is found.
8.
Describe the economics of nonrenewable minerals. Explain the limitations of mining lower-grade ores. Discuss
the option of getting more minerals from the ocean.
9.
Describe how mineral resources can be used more sustainably. Summarize the nanotechnology revolution and
its implications.
Key Terms (Terms are listed in the same font as they appear in the text.)
Acid mine drainage (p. 347)
area strip mining (p. 345)
asthenosphere (p. 336)
biological weathering (p. 340)
biomimicry (p. 352)
biomining (p. 349)
brownfields (p. 352)
buckyballs (p. 335)
chemical weathering (p. 340)
continental crust (p. 336)
continental glaciers (p. 340)
contour strip mining (p. 345)
convection cells (p. 337)
convergent plate boundary (p. 338)
core (p. 336)
crust (p. 336)
currents (p. 337)
cyanide heap extraction (p. 347)
depletion time (p. 348)
divergent plate boundary (p. 339)
earthquakes (p. 339)
economically depleted (p. 348)
erosion (p. 340)
external processes (p. 340)
fossil fuels (p. 341)
frost wedging (p. 340)
gangue (p. 347)
geology (p. 336)
glaciers (p. 340)
high-grade ore (p. 342)
highwall (p. 345)
igneous rock (p. 342)
lithosphere (p. 336)
low-grade ore (p. 342)
magma (p. 337)
manganese nodules (p. 350)
mantle (p. 336)
mass wasting (p. 340)
materials revolution (p. 350)
metallic minerals (p. 341)
metamorphic rock (p. 343)
mineral (p. 341)
mineral resource (p. 341)
molecular economy (p. 335)
mountaintop removal (p. 345)
nanotechnology (p. 335)
nanotubes (p. 335)
nonmetallic minerals (p. 341)
nonrenewable resources (p. 341)
oceanic crust (p. 336)
oceanic ridges (p. 339)
open-pit mining (p. 345)
ore (p. 342)
ore mineral (p. 347)
overburden (p. 345)
physical (mechanical) weathering (p. 340)
resource exchange webs (p. 352)
rock (p. 342)
rock cycle (p. 343)
sedimentary rock (p. 343)
smelting (p. 347)
spoil banks (p. 345)
spoils (p. 345)
strategic metal resources (p. 342)
strip mining (p. 345)
subduction (p. 339)
subduction zone (p. 339)
subsidence (p. 347)
subsurface mining (p. 345)
surface mining (p. 345)
Surface Mining Control and Reclamation Act (p. 346)
tailings (p. 347)
tectonic plates (p. 336)
transform fault (p. 339)
trench (p. 339)
tsunamis (p. 339)
volcanoes (p. 339)
weathering (p. 340)
Outline
Geologic Processes
A. The earth is made up of a core, mantle, and crust and is constantly changing as a result of processes taking
place on and below its surface. Geology is the study of dynamic processes occurring on the earth’s surface
and in its interior.
1. The crust is soil and rock that floats on a mantle of partly melted and solid rock.
2. The core is intensely hot. It has a solid inner part surrounded by a liquid core of molten or semisolid
material.
3. The mantle is a thick, solid zone. It is mostly solid rock, but an area called the asthenosphere is very
hot, partly melted rock about the consistency of soft plastic.
4. The crust is thin and is divided into the continental crust and the oceanic crust.
B. Huge volumes of heated and molten rock moving around the earth’s interior form massive solid tectonic
plates that move extremely slowly across the earth’s surface.
1. About 12 or so rigid tectonic plates move across the surface of the mantle very slowly. These thick
plates compose the lithosphere.
2. There are three types of boundaries for lithospheric plates. The boundaries are divergent plate
boundaries, where plates move apart in opposite directions, convergent plate boundaries, where plates
are pushed together by internal forces and one plate rides up over the other. A trench generally occurs
at the subduction zone. The third type of boundary is a transform fault and occurs where plates
slide/grind past one another.
3. The movement of these plates produces mountains on land and trenches on the ocean floor.
4. Earthquakes and volcanic action are violent and disruptive actions of the earth. Volcanoes and
earthquakes are likely to be found at the plate boundaries.
5. The plate tectonic theory also helps to explain certain patterns of biological evolution occurred.
C. Some processes wear down the earth’s surface by moving topsoil and pieces of rock from one place to
another, while other processes build up soil on the earth’s surface. Weathering is the physical, chemical,
and biological processes that break down rocks and minerals into smaller pieces.
Minerals, rocks, and the rock cycle
A. The earth’s crust consists of solid inorganic elements and compounds called minerals and rocks that can
sometimes be used as resources.
1. The crust is the source of the nonrenewable resources we use as well as the source of soil.
2. A mineral is an element or inorganic compound that is solid with a regular internal crystalline structure.
3. A mineral resource is a concentration of naturally occurring material in or on the earth’s crust that can
be extracted and processed into useful materials at an affordable cost.
4. Examples of mineral resources are fossil fuels (coal, oil, and natural gas), metallic minerals (such as
aluminum, iron, and copper), and nonmetallic minerals (such as sand, gravel, and limestone). As they
take so long to produce, these components of the earth’s natural capital are classified as nonrenewable
mineral resources.
5. Mineral resources can be classified into four major categories:
a. Identified resources with a known location, quantity, and quality
b. Reserves are identified resources that can be extracted profitably at current prices
c. Undiscovered reserves are potential supplies of a mineral resource assumed to exist
d. Other resources are undiscovered resources and identified resources not classified as reserves.
6. Future developments in nanotechnology may have potential benefits and drawbacks to the environment
and the economy.
B. Deposits of nonrenewable mineral resources in the earth’s crust vary in their abundance and distribution.
1. Iron and aluminum are fairly abundant whereas manganese, chromium, cobalt, and platinum are fairly
scarce.
2. Massive exports can deplete a countries supply of nonrenewable minerals.
3. Three countries (the United States, Canada, and Russia) with only 8% of the world’s population
consume about 75% of the world’s most widely used metals.
4. Japan has virtually no metal resources and has to rely on resource imports.
5. The United States currently depends on imports of 50% or more of 24 of its 42 most important
nonrenewable mineral resources.
6. Experts are concerned about the availability of four strategic metal resources (manganese, cobalt,
chromium, and platinum) that are essential for the country’s economic and military strength.
C. A very slow chemical cycle recycles three types of rock found in the earth’s crust. The earth’s crust
contains igneous, sedimentary, and metamorphic rocks that are recycled by the rock cycle.
1. Rock is a solid combination of one or more minerals.
2. An ore is a rock that contains a large enough concentration of a particular mineral (often a metal) that
the rock can be mined and processed to extract the desired mineral.
3. Igneous rock is formed below or on the earth’s surface when molten rock wells up and hardens. They
form the bulk of the earth’s crust.
4. Sedimentary rock is formed from small, eroded pieces of rock that are carried to downhill sites. Layers
accumulate over time and an increase of weight and pressure plus dissolved minerals bind the sediment
particles together to form sedimentary rock.
5. Metamorphic rock is produced from preexisting rock that is subjected to high temperatures, high
pressures, chemically active fluids, or some combination of these.
6. The rock cycle is the interaction of physical and chemical processes that change rock from one type to
another. It is the slowest of the earth’s cyclic processes.
Environmental Effects of Using Mineral Resources
A. The extraction, processing, and use of mineral sources has a large environmental impact. The greatest
danger from mineral extraction may be environmental damage from the processes used to get to the end
product.
1. Higher grade ores are more easily extracted.
2. Greater environmental damage comes with extraction of lower grade ores in higher energy costs and
greater environmental damage to the land.
B Minerals are removed through a variety of methods that vary widely in their costs, safety factors, and levels
of environmental harm. Shallow deposits are removed by surface mining, and deep deposits are removed
by subsurface mining.
1. In surface mining, the overburden of rock and soil is removed and discarded as spoils. This mining
method extracts about 90% of nonfuel mineral and rock deposits and 60% of the coal used in the U.S.
2. Surface mining is done by one of several methods:
a. open-pit mines are large holes dug to remove ores
b. strip mining is useful and economical for extracting mineral deposits that lie close to the earth’s
surface; area strip mining is used where land is relatively flat
c. contour strip mining is used on hilly or mountainous land where a series o f terraces are cut into the
hill
d. mountaintop removal uses explosives, and huge machinery to remove the top of a mountain for the
coal seams beneath it. This method causes considerable environmental damage.
3. The Surface Mining Control and Reclamation Act of 1977 (in the U.S.) requires mining companies to
restore most surface-mined land.
4. Reclamation efforts are only partially successful.
5. Subsurface mining removes coal and various metal ores too deep for surface mining.
6. Subsurface mining disturbs less than 1/10 as much land as surface mining with less waste, but is more
dangerous and expensive.
C. Mining scars the land and produces large amounts of solid waste and air and water pollution.
1. The land is left scarred and the surface is disrupted. Cleanup may cost in the billions.
2. Subsidence from underground mining causes sewer, gas and water systems to break.
3. Mining wastes contain toxins and acid drainage carries to streams and groundwater.
4. Toxic chemicals can also be emitted to the atmosphere.
D. After waste material is removed from metal ores they are smelted or treated with chemicals to extract the
desired metal.
1. Ore has two components: the ore mineral and the waste material called gangue.
2. Removing the gangue from ores produces large piles of solid waste called tailings.
3. Ore is separated from gangue, smelted to obtain the metal, made into products that are used and
discarded or recycled.
4. There can be enormous amounts of air and water pollution from these processes.
5. Cyanide is used to separate about 85% of the world’s gold ore in a process called cyanide heap
extraction. Cyanide is extremely toxic.
Supplies of Mineral Resources
A. The future supply of a resource depends on its affordable supply and how rapidly that supply is used. A
nonrenewable resource generally becomes economically depleted rather than totally depleted. There are
five choices at that point: recycle or reuse existing supplies, waste less, use less, find a substitute, or do
without.
1. Depletion time for a resource depends on how long it takes to use up a certain proportion (usually 80%)
at a given rate of use.
2. Depletion time is extended by recycling, reusing and reducing consumption of a given resource.
3. New discoveries of a resource extend the depletion time also.
4. The demand for mineral resources is increasing at a rapid rate with increased consumption.
5. No one knows whether we will run out of a mineral resource.
B. A rising price for a scarce mineral resource can increase supplies and encourage more efficient use.
1. Economics determines what part of a known mineral supply is extracted and used.
2. Some economists feel that price effect may no longer apply since industry and government often control
the supply, demand, and prices of minerals so that a truly competitive market does not exist.
3. Governments subsidize development of domestic mineral resources. In the U.S. mining companies get
depletion allowances of 5-22% of their gross income. They are also allowed to deduct much of the cost
of finding and developing mineral deposits.
4. Rather than receiving billions in government subsidies, critics feel that taxing extraction of nonfuel
mineral resources would create incentives for more efficient resource use, reduce waste and pollution,
and encourage recycling and reuse of these resources.
C. New technologies can increase the mining of low-grade ores at affordable prices, but harmful
environmental effects can limit this approach.
1. In 1900, the average copper ore mined in the U.S. was about 5% copper by weight; today that ratio is
0.5%.
2. One limiting factor in mining low-grade ore is the increased cost of mining; another is the availability
of freshwater that is needed to mine and process some minerals; a third is the environmental impacts of
increased land disruption, waste material, and pollution produced during mining and processing.
3. One way to improve mining is to use microorganisms for in situ mining. However, the process is slow
and biological mining may only be feasible with low-grade ores for which conventional techniques are
too expensive.
D. Most minerals in seawater and on the deep ocean floor cost too much to extract, and there are squabbles
over who owns them.
1. Rich hydrothermal deposits of gold, silver, zinc, and copper are found as sulfide deposits in the deepocean floor and around hydrothermal vents.
2. Another potential source from the ocean floor is potato-size manganese nodules that cover about 2550% of the Pacific Ocean floor.
3. High costs of extraction of both the nodules and hydrothermal ore deposits are prohibitive.
Using Mineral Resources More Sustainably
A. Scientists and engineers are developing new types of materials that can serve as substitutes for many
metals. This is known as the materials revolution.
1. Development of silicon and ceramics may replace the need for as much metal.
2. Ceramics have many advantages over conventional metals (harder, stronger, lighter, last longer) and do
not corrode.
3. Automobiles and planes are being made of plastics and composite materials since they cost less to
make, are lower maintenance and can be molded to any shape.
4. Use of plastics has drawbacks; they require the use of oil and other fossil fuels.
5. Nanotechnology is the use of science and engineering at the atomic and molecular level to build
materials with specific properties.
a. Buckyballs are soccer-ball shaped forms of carbon that have been engineered.
b. Nanotechnology is a new area that could provide many things in the near future.
c. One concern about nanotechnology is that smaller particles tend to be more reactive and potentially
more toxic due to large surface area compared to mass.
d. They can pass through the natural defenses of the body.
e. Analysts say we need to carefully investigate its potential harmful aspects and then develop
guidelines and regulations to control and guide this new technology.
B. Recycling valuable and scarce metals saves money and has a lower environmental impact than mining and
extracting them from their ores.
C. We can use mineral resources more sustainably by reducing their use and waste and by finding substitutes
with fewer harmful environmental effects.
D. Growing signs point to an ecoindustrial revolution taking place over the next fifty years.
1. The goal is to make industrial manufacturing processes cleaner and more sustainable by redesigning
them to mimic how nature deals with wastes.
2. One way is to mimic nature by recycling and reusing most minerals and chemicals instead of disposing
of them. Another is to have industries interacvt through resource exchange webs.
3. Figure 15-19 shows the industrial ecosystem in Kalundborg, Denmark.
4. These industrial forms of biomimicry provide many economic benefits for business and the
environment.
5. In 1975, the 3M company began a Pollution Prevention pays (3P) program. Other companies are also
adopting similar pollution and prevention programs.
Summary
1.
2.
Major geological processes that occur within the earth are known as internal processes, and they build up the
surface of the earth. Geological processes that occur on the surface of the earth include erosion and
weathering.
Tectonic plates have rearranged the earth’s continents and ocean basins over millions of years like pieces of a
gigantic jigsaw puzzle. The plates have three types of boundaries. Natural hazards such as earthquakes and
volcanoes are likely to be found at plate boundaries.
3.
Rocks are large, natural, continuous parts of the earth’s crust. There are three major types of rocks: igneous,
sedimentary, and metamorphic. Rocks are affected by changes of physical and chemical conditions that
change them over time from one type to another through the rock cycle.
4.
Mineral resource extraction methods include surface and subsurface mining. Surface mining types are openpit, strip, contour strip mining, and mountain removal.
5.
Mineral resources that can be reused and recycled have a longer depletion time compared to those that cannot
be reused or recycled and there is no increase in reserves discover.
6.
Scientists are developing new types of materials as substitutes for many metals. Mineral conservation and more
sustainable manufacturing processes are helping to decrease our use and waste of such resources. An
ecoindustrial revolution is underway in some parts of the world.
Glossary
area strip
mining
Type of surface mining used where the terrain is flat. An earthmover strips away the overburden,
and a power shovel digs a cut to remove the mineral deposit. After removal of the mineral, the
trench is filled with overburden, and a new cut is made parallel to the previous one. The process is
repeated over the entire site. Compare dredging, mountaintop removal, open-pit mining,
subsurface mining.
contour strip
mining
Form of surface mining used on hilly or mountainous terrain. A power shovel cuts a series of
terraces into the side of a hill. An earthmover removes the overburden, and a power shovel
extracts the coal, with the overburden from each new terrace dumped onto the one below.
Compare area strip mining, dredging, mountaintop removal, open-pit mining, subsurface mining.
convergent
plate boundary
Area where earth's lithospheric plates are pushed together. See subduction zone. Compare
divergent plate boundary, transform fault.
core
Inner zone of the earth. It consists of a solid inner core and a liquid outer core. Compare crust,
mantle.
crust
Solid outer zone of the earth. It consists of oceanic crust and continental crust. Compare core,
mantle.
depletion time
The time it takes to use a certain fraction, usually 80%, of the known or estimated supply of a
nonrenewable resource at an assumed rate of use. Finding and extracting the remaining 20%
usually costs more than it is worth.
divergent plate
boundary
Area where earth's lithospheric plates move apart in opposite directions. Compare convergent
plate boundary, transform fault.
earthquake
Shaking of the ground resulting from the fracturing and displacement of rock, which produces a
fault, or from subsequent movement along the fault.
economic
depletion
Exhaustion of 80% of the estimated supply of a nonrenewable resource. Finding, extracting, and
processing the remaining 20% usually costs more than it is worth. May also apply to the depletion
of a renewable resource, such as a fish or tree species.
erosion
Process or group of processes by which loose or consolidated earth materials are dissolved,
loosened, or worn away and removed from one place and deposited in another. See weathering.
geology
Study of the earth's dynamic history. Geologists study and analyze rocks and the features and
processes of the earth's interior and surface.
high-grade ore
Ore that contains a fairly large amount of the desired mineral.
identified
resources
Deposits of a particular mineral-bearing material of which the location, quantity, and quality are
known or have been estimated from direct geological evidence and measurements. Compare
undiscovered resources.
igneous rock
Rock formed when molten rock material (magma) wells up from the earth's interior, cools, and
solidifies into rock masses. Compare metamorphic rock, sedimentary rock. See rock cycle.
lithosphere
Outer shell of the earth, composed of the crust and the rigid, outermost part of the mantle outside
the asthenosphere; material found in earth's plates. See crust, mantle.
low-grade ore
Ore that contains a smaller amount of the desired mineral.
magma
Molten rock below the earth's surface.
mantle
Zone of the earth's interior between its core and its crust. Compare core, crust. See lithosphere.
metamorphic
rock
Rock produced when a preexisting rock is subjected to high temperatures (which may cause it to
melt partially), high pressures, chemically active fluids, or a combination of these agents. Compare
igneous rock, sedimentary rock. See rock cycle.
mineral
Any naturally occurring inorganic substance found in the earth's crust as a crystalline solid. See
mineral resource.
mineral
resource
Concentration of naturally occurring solid, liquid, or gaseous material in or on the earth's crust in a
form and amount such that extracting and converting it into useful materials or items is currently or
potentially profitable. Mineral resources are classified as metallic (such as iron and tin ores) or
nonmetallic (such as fossil fuels, sand, and salt).
mountaintop
removal
Type of surface mining that uses explosives, massive shovels, and even larger machinery called
draglines to remove the top of a mountain to expose seams of coal underneath a mountain.
Compare area strip mining, contour strip mining.
nanotechnology Using atoms and molecules to build materials from the bottom up using the elements in the
periodic table as its raw materials.
open-pit mining Removing minerals such as gravel, sand, and metal ores by digging them out of the earth's
surface and leaving an open pit. Compare area strip mining, contour strip mining, dredging,
mountaintop removal, subsurface mining.
ore
Part of a metal-yielding material that can be economically and legally extracted at a given time. An
ore typically contains two parts: the ore mineral, which contains the desired metal, and waste
mineral material (gangue).
other resources Identified and undiscovered resources not classified as reserves. Compare identified resources,
reserves, undiscovered resources.
overburden
Layer of soil and rock overlying a mineral deposit. Surface mining removes this layer.
plate tectonics
Theory of geophysical processes that explains the movements of lithospheric plates and the
processes that occur at their boundaries. See lithosphere, tectonic plates.
plates
See tectonic plates. Various-sized areas of the earth's lithosphere that move slowly around with
the mantle's flowing asthenosphere. Most earthquakes and volcanoes occur around the
boundaries of these plates. See lithosphere, plate tectonics.
reserves
Resources that have been identified and from which a usable mineral can be extracted profitably
at present prices with current mining technology. See identified resources, undiscovered
resources.
rock
Any material that makes up a large, natural, continuous part of the earth's crust. See mineral.
rock cycle
Largest and slowest of the earth's cycles, consisting of geologic, physical, and chemical processes
that form and modify rocks and soil in the earth's crust over millions of years.
sedimentary
rock
Rock that forms from the accumulated products of erosion and in some cases from the compacted
shells, skeletons, and other remains of dead organisms. Compare igneous rock, metamorphic
rock. See rock cycle.
smelting
Process in which a desired metal is separated from the other elements in an ore mineral.
spoils
Unwanted rock and other waste materials produced when a material is removed from the earth's
surface or subsurface by mining, dredging, quarrying, and excavation.
strip mining
Form of surface mining in which bulldozers, power shovels, or stripping wheels remove large
chunks of the earth's surface in strips. See area strip mining, contour strip mining, surface mining.
Compare subsurface mining.
subduction
zone
Area in which oceanic lithosphere is carried downward (subducted) under the island arc or
continent at a convergent plate boundary. A trench ordinarily forms at the boundary between the
two converging plates. See convergent plate boundary.
subsurface
mining
Extraction of a metal ore or fuel resource such as coal from a deep underground deposit.
Compare surface mining.
surface mining
Removing soil, subsoil, and other strata and then extracting a mineral deposit found fairly close to
the earth's surface. See area strip mining, contour strip mining, dredging, mountaintop removal,
open-pit mining. Compare subsurface mining.
tectonic plates
Various-sized areas of the earth's lithosphere that move slowly around with the mantle's flowing
asthenosphere. Most earthquakes and volcanoes occur around the boundaries of these plates.
See lithosphere, plate tectonics.
transform fault
Area where the earth's lithospheric plates move in opposite but parallel directions along a fracture
(fault) in the lithosphere. Compare convergent plate boundary, divergent plate boundary.
tsunami
Series of large waves generated when part of the ocean floor suddenly rises or drops, usually
because of an earthquake.
undiscovered
resources
Potential supplies of a particular mineral resource, believed to exist because of geologic
knowledge and theory, although specific locations, quality, and amounts are unknown. Compare
identified resources, reserves.
volcano
Vent or fissure in the earth's surface through which magma, liquid lava, and gases are released
into the environment.
weathering
Physical and chemical processes in which solid rock exposed at earth's surface is changed to
separate solid particles and dissolved material, which can then be moved to another place as
sediment. See erosion.