lecture notes for week 3
TRANSCRIPT
Our Earth’s Resources
We use things the Earth gives us to help us live better lives
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UGRC 143 : SCIENCE AND TECHNOLOGY IN OUR LIVES
SECOND SEMESTER : 2014/2015 ACADEMIC YEAR
EARTH RESOURCES
Dr. Larry Pax ChegbelehDepartment of Earth ScienceUniversity of Ghana, Legon
OVERVIEW
Purpose and Objectives of lesson Introduction Resources Earth resources Resources management The rock cycle, formation and
classification2
Purpose and Objectives
This lesson is to enable you understand what resources are and how to manage them for sustainable livelihood
It is expected that by the end of the lesson you should be able to …..
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Purpose and Objectives
Define resources in general and earth resources in particular
Identify various categories of resources Differentiate between resources and
reserves Define the types of rocks Explain the formation of the rock types State the major classifications of rocks
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Introduction
To some extend you have prior knowledge of what resources are
More understanding is required to know their differences
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What are Resources?
All those things that are necessary or important to human life and civilization
A source or supply from which benefit is derived or produced
Any material that can be transformed to produce benefit
What are Resources? Typical examples include:
Materials Knowledge Staff (Human resources) skills, energy, talent
and knowledge used for the production of goods or rendering of services
Services Energy Other things that are transformed to produce
benefit
What are Resources? The benefit derived can be utilized/consumed
or made unavailable in the process Some of the benefits of using resources
include: Increase in wealth Meeting our needs Proper functioning of a system Enhancing well being
How we use them We use resources to make things and to
grow things we need
Examples of things we use include: Water to drink and grow plants for food,
shelter, and clothing. Soil to grow plants for food, shelter, and
clothing. Rocks for building and jewelry.
How we use them
Metals to make cans, building parts, and jewelry.
Sand to make glass. Oil to make plastics and gasoline.
Earth or Natural Resources Resources that are involved in or formed by
geologic processes From human point of view is anything
obtained from the environment to satisfy human needs
From ecological or biological view point is anything that satisfies the needs of living organisms
Earth or Natural ResourcesExamples of earth resources include
Groundwater Soil Rocks Minerals Oil and gas
Classification of Earth or Natural Resources
Earth resources are classified into various categories based on:
Source of origin Stage of development Renewability or replenishment
Classification of Earth or Natural Resources
Based on origin, resources may categorized into:
Biotic: - these are obtained from the biosphere (living and organic material)
▪ Examples: forests and animals and materials that can be obtained from them
▪ Coal and petroleum are formed from decayed organic materials
Classification of Earth or Natural Resources
Abiotic: - these are those that come from non-living and non-organic materials
▪ Examples include: air, fresh water, land, minerals
Classification of Earth or Natural Resources
Based on stage of development, resources may categorized into:
Potential resources: - these are those that exist in an area or region and are recoverable in the future
▪ Example: petroleum may occur in various regions, until it is actually drilled out, developed and put into use, it remains a potential resource
Classification of Earth or Natural Resources
Actual resources: - these are those that that have been investigated and quantified and being used in present times
Reserved resources: the part of an actual resource that can be developed profitably with available technology
Stock resources: those that have been investigated but can not be put to use due to lack of technology
Classification of Earth or Natural Resources
Based on the time required to replace the quantity of resources used (renewability) or consumed, resources can beRenewableNonrenewableInexhaustible (Perpetual resources)
Renewable ResourcesResources that can be replenished over fairly
short spans of time, such as months, years, or decades (e.g., trees)
Can be replenished naturallyFrom human perspective, rate of replenishment
or recovery exceeds that of consumptionCan be depleted by human consumption
Nonrenewable Resources
Rate of consumption exceeds rate of replenishment or recovery (time needed to create >>> time needed to consume).
Form slowly or do not naturally form in the environment (may take millions of years to form and accumulate)
E.g. fossil fuels (petroleum)
Inexhaustible ResourcesThese are available continuously
Their quantity is not affected by human consumption
We shall never run out, like sunlight, air, and wind
However it can be ruined by pollution.
Resources may also be categorized based on distribution
Ubiquitous resources: these are found everywhere in the world (e.g. air, light and water)
Localized resources: these are found in certain parts of the world or within certain localities (e.g. Iron ore, copper ore and geothermal power)
ExceptionsAll earth resources, except groundwater, are nonrenewable
Resources, People and standards of living
The more people on earthoThe more water we consumeoThe more food we grow/eat
oThe more fuel we burn
oThe more minerals we use
Resources, People and standards of living
Rates of resources used even increasing faster than rate of population increase.
Why?
Resources, People and standards of living
o Elevated standards of living.
o improvements in life-styles hence, increasing quantities of manufactured goods ( cars, clothes, computers, etc.)
Resources management
In order to make resources last, we must take good care of them
Use resources sustainably
Earth System Science
Population
Population of the planet is growing rapidly
Use of minerals/energy has climbed more rapidly than the overall growth of population
Growth of World Population
REDUCE: How much we useREUSE: What we canRECYCLE: Whatever we can
In order to help our Earth to keep providing for our needs.
3Rs of Resource Management
Use Resources Wisely to Protect our Environment
The biotic and abiotic surrounding of an organism including factors that have influence in the survival, development and evolution of the organisms
Environment (biophysical environment)
Use Resources Wisely to Protect our Environment
Implies surrounds and influences organisms.
Physical environment encompasses water, air, soil and rock.
Environment (biophysical environment)
Marine environment (oceans, e.g. water bodies)
Atmospheric environment(Layer of gases surrounding the earth, e.g. nitrogen and oxygen)
Terrestrial environment(Land, e.g. soil and rock)
Biophysical Environment Subdivision
Number of biophysical environment is myriad if we consider that each living organism has its own environment
The harmful aspect of human activities on the biophysical environment.
The term anthropogenic is used to designate an effect or object resulting from human activity
Environmental Problems
Environmental Problems
Local, regional, and global Caused by people and societies
Urban air pollutionAcid rainOzone depletionAcid mine drainageGlobal warming
Urban air pollution
Acid rain
Ozone depletion
Acid mine drainage
Effects of Global Warming
Resources Vs. Reserves
Resources are not the same as ReservesReserves are measured (proven)
economic resources (e.g. barrels of crude oil or tons of chromium ore)
Look at this graphically:
Resources vs. Reserves
Examples of resources
Water
Soil
Copper and aluminum
Sand and Limestone
Salt and Silver
Clay and coal
REMEMBER TO:
ReduceReuseRecycle
Save our Natural Resources!
What is a rock?
A rock is any solid mass of minerals or mineral-like matter occurring naturally as part of our planet
A rock is simply an aggregate of minerals
What is a rock?
Types of Rocks
Igneous rock is formed by the crystallization of molten magma.
What is a rock?
Types of Rocks
Metamorphic rock is formed by the alteration of pre-existing rock deep within Earth (but still in the solid state) by heat, pressure, and/or chemically active fluids.
What is a rock?
Types of Rocks
Sedimentary rock is formed from the weathered products of pre-existing rocks that have been transported, deposited, compacted, and cemented.
What is a rock?
Important terms to note Magma is molten material that is
formed deep beneath the Earth’s surface. Lava is magma that reaches the surface. Weathering is a process in which rocks
are broken down by water, air, and living things.
Sediment is weathered pieces of Earth elements.
The Rock Cycle
Shows the interrelationships among
the three rock types (igneous, sedimentary, and metamorphic)
Energy That Drives the Rock Cycle
Processes driven by heat from the Earth’s interior are responsible for forming both igneous rock and metamorphic rock.
Energy That Drives the Rock Cycle
Weathering and the movement of weathered materials are external processes powered by energy from the sun.
External processes produce sedimentary rocks.
Formation of Igneous Rocks
1. Intrusive igneous rocks are formed when magma hardens beneath Earth’s surface.
2. Extrusive igneous rocks are formed when lava hardens.
Classification of Igneous Rocks Igneous rocks can be classified based on
their
TextureChemical composition
Classification of Igneous Rocks
Texture
Coarse-grained texture: Caused by slow cooling resulting in larger crystals.
Fine-grained texture: Caused by rapid cooling resulting in smaller, interconnected mineral grains.
Classification of Igneous Rocks
Texture
Glassy texture: Caused by very rapid cooling.
Porphyritic: Caused by differential rates of cooling resulting in varied sized mineral grains.
Course-Grained Igneous Texture
Fine-Grained Igneous Texture
Obsidian Exhibits a Glassy Texture.
Porphyritic Igneous Texture
Classification of Igneous Rocks
Chemical composition
Granitic: Made mostly of light-colored quartz and feldspar.
Andesitic: Between granitic light-color minerals and basaltic composition dark-colored minerals.
Classification of Igneous Rocks
Chemical composition
Basaltic: Mostly of dark-colored silicate minerals and plagioclase feldspar.
Ultramafic: Made mostly from iron and magnesium-rich minerals.
Basalt
Classification of Igneous Rocks
Formation of Sedimentary Rocks
Erosion involves the weathering and the removal of rock.
Deposition occurs when an agent of erosion such as water, wind, ice, or gravity loses energy and drops sediments.
Weathering, Erosion, and Deposition
Formation of Sedimentary Rocks
Compaction is a process that squeezes, or compacts sediments.
Cementation takes place when dissolved minerals are deposited in the tiny spaces among the sediments.
Compaction and Cementation
Classification of Sedimentary Rocks
1. Clastic sedimentary rocks are composed of weathered bits of rocks and minerals.
• Classified by particle size
Two Main Groups
- Shale (most abundant)
• Common rocks include
- Conglomerate
- Sandstone
Shale with Plant Fossils
Conglomerate
Classification of Sedimentary Rocks
Two Main Groups2. Chemical sedimentary rocks form when dissolved
substances precipitate, or separate, from water.
• Common rocks include
- limestone—most abundant chemical rock
- microcrystalline quartz known as chert, flint, jasper, or agate
- evaporites such as rock salt or gypsum - coal
Fossiliferous Limestone
Classification of Sedimentary Rocks
Formation of Metamorphic Rocks
Metamorphism means “to change form”Most metamorphic changes occur at elevated temperatures and pressures
Conditions for formation - a few kilometers below the Earth’s surface and extend into the upper mantle
Formation of Metamorphic Rocks
Contact metamorphismRegional metamorphism
Formation of Metamorphic Rocks
Contact metamorphismOccurs when magma moves into rock. Occurs near a body of magmaChanges are driven by a rise in
temperature
Metamorphic Rocks
Regional metamorphism Results in large-scale deformation and
high-grade metamorphismDirected pressures and high temperatures
occur during mountain buildingProduces the greatest volume of
metamorphic rock
• .
Agents of Metamorphism
Heat Pressure Hydrothermal Solutions
Agents of Metamorphism
Heat Provides the energy needed
to drive chemical reactions
Agents of Metamorphism
Pressure Causes a more compact
rock with greater density
Origin of Pressure in Metamorphism
Agents of Metamorphism
Hydrothermal Solutions Hot water-based solutions escaping
from the mass of magma Promote recrystallization by
dissolving original minerals and then depositing new ones
Classification of Metamorphic Rocks
1. Foliated Metamorphic Rocko Has a banded or layered appearance
2. Nonfoliated Metamorphic Rocko Does not have a banded texture
Two main categories
Classification of Metamorphic Rocks
Gneiss Typically Displays a Banded Appearance
Marble—A Nonfoliated Metamorphic Rock
End of Lesson 2