Chapter 9 Earth
9.1 System and structure of the Earth
Earth system
The system consists of four main components, which are interrelated namely geosphere, hydrosphere, biosphere and atmosphere.
Geosphere (Rock and soil zone)
Refers to solid part of the Earth.
Covers the land area of the Earth and also seabed
Geo means soil. Therefore, geosphere includes the rocks, minerals and soil found on the Earth
Hydrosphere (Water zone)
The part of the Earth that is made up of water such as rivers, lakes, oceans, ponds and groundwater, including freshwater, salt water, snow and glaciers.
Covers more than 70% of the Earth. 97.2% of the hydrosphere is salt water and 2.8% is freshwater.
Biosphere (Life Zone)
The region on the Earth's surface that supports life such as humans, animals, plants and microorganisms like bacteria, fungi, algae and protozoa
Can be divided into various ecosystems such as grassland, forest, mangrove swamp and desert. Each ecosystem is a habitat to various populations of animals and plants
Atmosphere (Air Zone)
Traps heat, making the Earth's temperature suitable for living things
Supplies oxygen gas for respiration and carbon dioxide for photosynthesis
Protects living organisms from genetic damage caused by harmful ultraviolet rays and cosmic radiations
Consists of 78% nitrogen, 21% oxygen, 0.03% carbon dioxide and 0.97% inert gases and other elements
A layer of air with a thickness of 1000 km surrounding the Earth.
Atmospheric Stratification
The temperature of atmosphere changes according to layer. For example,
The higher the altitude, the lower the air pressure because the gravitational force becomes weaker as the altitude increase
Most of the scientists divided the Earth's atmosphere into 5 layers.
Is divided into layers according to altitude or known as atmospheric stratification
The temperature decreases with the increase in altitude from troposphere to mesosphere
The temperature increases with the increase in altitude from mesosphere to the thermosphere
Atmosphere
Stratosphere
Mesosphere
Exosphere
Troposphere
Thermosphere
Troposphere
It contains the most cloud. The changes of weather and climate take place here. All weather phenomena such as wind, rain, storm and snow occur in this layer
This layer supports living organisms such as humans, animals and plants
Has the highest air mass, causing it to have the highest air pressure
The thinnest layer to the Earth's surface
Strastosphere
The layer that contains a lot of ozone gas and known as ozone layer is located here (altitude 18 - 38 km)
Mesosphere
The coldest layer. The extremely cold temperature
The destruction of meteorites caused by the collision with gas particles takes place in this layer. This resulted in the phenomenon of shooting star or meteor
Thermosphere
The layer is also known as ionosphere
The phenomenon of aurora occurs in the layer. Aurora is a band of colourful lights, resulting from the magnetic field and atmospheric gases
The layer contains many ions (changes particles) that can reflect radio waves
Exosphere
The outermost and the furthest layer of atmosphere from the Earth's surface
Ocean Stratification
As the depth of the ocean increases:
The ocean is divided into three zones:
The ocean is divided into a few layers known as zone. The zones differ based on the penetration of light (amount of light received)
Midnight zone
Dark zone
Surface zone
The lower is the temperature
The higher is the pressure
The lower is the light intensity (becomes darker)
Surface zone
This zone is suitable as a habitat for photosynthetic organisms. This zone supports living things
Photosynthesis process occurs in this zone
Water is shallow and light can penetrate into this zone
Average temperature is 20c
Midnight zone
A habitat for large marine animals such as whales and giant octopuses
Animals in this zone get leftover food from the light zone or eat among themselves
Not enough light for photosynthesis process. Plants difficult to survive in this zone
This zone has little or no light
Average temperature is 5c
Dark zone
Marine animals that live in this zone have fluorescent bodies that are able to glow in the dark
No plants live in this zone
This zone has no light at all
Average temperature 0c
Distribution of Water on Earth
This can be explained through the water cycle
Water doesn't remain static at one place. The Earth's water supply always moves from one place to another in different forms
Water exists as water vapour in the air, rivers, lakes, glaciers and snow in the polar regions
96.5% of water on the Earth's surface is the ocean
About 71% of the Earth's surface is covered by water
Ocean
Lake
Condensation
Evaporation
Trees
Clouds
Rain
Transpiration
Rain
Clouds
Rain
Water flowing on surface
Water flows underground
Water storage underground
Water storage as ice and snow
Water flows into river
Distribution of Water on Earth
Earth Layer
The Earth is made up of 3 layers according to its physical characteristics with are the crust, mantel and core
The mantle consist of lithosphere, asthenosphere and mesosphere
Earth's layer
Crust
Mantle
Core
Asthenosphere
Mesosphere
Lithosphere
Crust
Consists mainly of rocks and minerals
Made up of layers of different types of hard rocks
0 - 60km thick
The outermost layer of the Earth
Litosphere
100 - 250 km thick beneath the Earth's crust
The coldest and hardest layer of the Earth
Made up of hard solids
Includes the brittle upper part of the mantle and the crust
Asthenosphere
Temperature at 1300c. High temperature and pressure causes the rocks to melt and become semi solids, enabling the lithosphere to float on this layer
80 - 200km thick beneath the lithosphere
Consists of semi-solids that are viscous and elastic
Mesosphere
The rocks in mesosphere layer is extremely hot and can flow gradually due to the convection current of the mantle formed by the heat from the core of the Earth
Temperature at 2000c
2550km thick
Exists as a solid under high pressure
Outer core
Convection current in the outer core generated the Earth's magnetic field
Temperature at 4500 - 5000c
2200km thick
A fluid layer composed of iron and nickel
The layer surrounding the inner core
Inner core
Temperature may reach 5500c
1220km thick
Made up of iron and nickel
Exists in the form of solid due to compression under high pressures
Earth is the only place that can sustain life
Reasons why the Earth is the most suitable place for various living things:
The Earth is the only planet that supports various living things from the tiniest organism such as microorganisms to the most complex organism, such as humans
The Earth is the only place for living things
The Earth's atmosphere consists of gases needed by living things:
The Earth has suitable weather for living things
The position of the Earth is not too near or too far from the Sun. Therefore, the temperature of the Earth is not too cold or too hot
The Earth has water that is vital for all ling things and living processes
The sunlight received by the Earth is enough for living things to survive because of the Earth ideal distance from the Sun. Green plants and producer organisms absorb sunlight to make food and release oxygen as a by-product through the photosynthesis process
21% of the air is oxygen gas. Oxygen is needed for respiration
0.03% of the air is carbon dioxide gas. Carbon dioxide is needed by green plants to carry out photosynthesis process.
Composition of the Earth
The rocks on Earth can be divided into three groups based on the formation process, which are the:
Each group of rocks is formed by a different process and takes a very long time from thousands to millions of years to form
Rack consists of materials known as minerals
Sedimentary rocks
Metamorphic rocks
Igneous rocks
Igneous rock
Sedimentary rock
Metamorphic rock
Does not contain fossils
Contains crystals of various sizes
Very hard and dense
No layer
Has a very high melting point
A coloured rock that depends on its mineral composition
Contains minerals
Fossil fuels are fond in sedimentary rocks
Contains fossil
Has many layer which sometimes hollow
Its texture and grain can easily be distinguished. For example, shale rock (fine grain) and conglomerate rock (pebble size grains)
Softer than igneous rock
The formation process
A coloured rock that depends on its mineral composition
Minerals such as gold and silver can be found in this type of rock
Has foliated texture (the layers are either parallel or wavy
Often contains minerals and crystals
Very hard, Usually harder than the original rock that formed it
The formation process
The formation process
Formed by the process of cooling and freezing of magma or lava that flows out of the mantle
Formed by compression of deposited minerals carried by rivers, glasiers and wind
Formed when igneous rocks or sedimentary rocks are exposed to a very high pressure and temperature
The rock cycle
The process of formation of igneous, sedimentary and metamorphic rocks can be explained using rock cycle
Cooling and freezing of magma
heat and pressure increases
Heated pressure
Sedimentary rock
Sedimentation of eroded materials
Erosion
Weathering
Igneous rock
Metamorphic rock
magma
Uplift to the surface
Melting
Compression
The process of rock formation
The cooling and freezing of magma in the Earth's crust produces igneous rocks. For example, granite, gabbro, basalt and purmice.
The same process happens to metamorphic rocks, which are embedded deeply into the Earth's crust that are exposed to hot magma. The metamorphic rocks will melt to form magma again and flows into the mantle due to the tectonic motion. The molten rocks will reform igneous rocks once again and the cycle continues
Sedimentation, compression and cementation of the sediments for millions of years will produce sedimentary rocks such as coal, limestone, shale, sandstone and conglomerate stone
Furthermore, the sedimentary rocks are embedded deeply into the Earth's crust and exposed to a high temperature and high pressure. Sedimentary rocks undergo physical and chemical changes to form metamorphic rocks. For example, limestone changes into marble, coal changes into diamond and sandstone into quartzites
The process of denudation such weathering and erosion, and the effect of weather and climate on the 3 types of rocks cause the rocks to break into pieces and form sediment
Main processes of the Earth
Geomorphology
Exogenic process
Endogenic process
The study and knowledge about physical features of the Earth's surface such as the land, ocean and also the layers of the Earth.
Occurs on Earth cause the formation and changes in the surface of the Earth's crust
There are 2 main types of geological processes
Exogenic process
Endogenic process
The geological process occurs on the surface of theEarth.
Exogenic forces that originate from outside the Earth's surface ( atmosphere ):
Driven by exogenic force that originate from the Earth's surface or outside the Earth's surface ( atmosphere ).
The gravitational force of the moon causes the formation of waves and the phenomena of tides and the tidal in the ocean that can erode beaches and high cliffs along the beaches.
The collision of meteoroid onto the surface of the Earth changes the landforms
The radiation from the Sun causes the movement of water, ice and air. The movement of air forms wind, which is the main agent in the exogenic processes such as erosion and weathering.
Erosion
Transport and sedimentation
Weathering
Mass and land depletion
The wearing away of the Earth's surface by agents of erosion such as water, wave and wind
The geomorphological process that changes the physical characteristics of rocks but does not change the chemical and biological characteristics of the rocks
Can also caused by human activities, the roots of plants that creep along and break the rocks and animals that dig the ground such as worms, rats and chipmunks
A process of fragmentation and decomposition of rocks on the Earth's surface into smaller pieces when exposed to physical, chemical and biological processes such as changes in temperature, rainwater, frost action and microorganism
The results of weathering are the landforms and landscapes such as limestone cave, stalactites and stalagmites
The process of movement of the Earth's materials down the slope by gravitational force
The Earth's materials from the highland areas are broken down by erosion and weathering agents, which results in the lowering of altitude of the highland areas
Examples of mass depletion are the movement of soils and rocks from the top of a slope and landslide phenomenon
Topographical and geological factors affect the rate of mass depletion
Water acts as a lubricant that helps to move or deplete the mass ( rocks and soils ) down the slope. Landslides and mass depletion often occur at slope areas during heavy rains
The movement of weathered or eroded materials from one place to another by the action of wind, water, waves, glaciers and force of gravity
The accumulation and deposition of eroded materials or sediment when the velocity of the weathering agents decreases
The same as the agents of erosion, weathering and mass depletion but their power and reaction rate are slower and weaker.
Fragmentation
Decomposition
The geological process that occurs beneath the Earth's surface, which is driven by endogenic forces originated from within the Earth's crust.
There are 3 endogenic processes:
Magma activity
Mantle convection process
Earth's crust movement (plate tectonics)
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Magma activity
Magma activities cause volcanic eruptions
Volcanic eruption is a phenomenon whereby hot magma from the Earth's core erupts to the surface of the Earth. The hot magma that flows out is known as lava.
Although the phenomenon of volcanic eruption is not direct cause in producing terrain topography, but the formation of volcanic rocks on the surface of the Earth's crust provides the site or surface for exogenic processes such as weathering, erosion and mass depletion that change the Earth's landforms
Lava cools and hardens to form two types of igneous rock, which are the intrusive rocks and plutonic rocks
Plate tectonic movement
Mantle convection process
Is formed as a result of heat action in the Earth's core on the rocks in the mantle
The hotter magma is less dense and moves upwards and is replaced by a cooler magma, which is denser that moves downwards.
The repetition movement of hot magma upwards and cool magma downwards forms mantle convection current
The theory of plate tectonic states that the Earth's crust is made up of several pieces of plates that glides over the mantle
These plates are hard and brittle rocks that float on the flowing magma in the mantle. Therefore, the plates glide like a layer of oil on the water. Observations from the researchers' data showed that the energy from the convection current causes the movement of the Earth's plate at a rate of 3cm.
The movement of the Earth's plates involves the process of collision and divergence of plates. Both processes produce various landforms and continental drifts.
Geohazard Phenomena
Geohazard
Volcanism
Landslide
Tsunami
Global Warming and Greenhouse Effect
Earthquake
In general, volcanic eruption occurs due to the magma beneath the Earth's crust being forced out by high pressure gases
The gas bubbles exert high pressure. The high pressure causes the magma to erupt out to the surface of the Earth. This volcanic eruption is called volcanism.
The earthquake is the shaking of the surface of the surface of the Earth's crust caused by sudden release of energy from within the Earth's crust in the form of seismic waves that move in between the layers of the Earth's crust
The sudden release of energy occurs when the tectonic plates meet and collide abruptly in the area of intersection of the tectonic plates and the fault lines.
Effect of earthquake:
Strong earthquake may cause tsunami and landslides
This results in the destruction of many properties, roads, railways and airports.
The collapse of buildings and landslides due to earthquakes have caused many humans and animals to lose their lives.
Is known as seismic waves of the sea, which is a series of waves in a water body caused by the displacement of a large volume of water.
The causes of tsunami:
The movement of plates and the collision of oceanic crust plates
The occurrence of undersea earthquakes
The eruption of undersea volcanoes
The occurrence of undersea landslides
The effects of tsunami:
Destruction of the environment
Loss of human and animals lives
Destruction of infrastructure
A process of mass depletion caused by the instability of the mass of soil
The movement of the soil and rocks down the slope under the influence of gravity is due to the instability of the mass of soil and rocks, causing it to move to undergo a restructuring to become more stable
The process of landslides involves ground movements such as earth flow, soil movement, rockfalls, debris flows or mudflows and ice slides
The increase in the Earth's temperature globally due to greenhouse effect
A phenomenon where hear energy from the sunlight is trapped by the greenhouse gases in the lower layer of the Earth's atmosphere that causes warming of the Earth's surface.
Effect of global warming:
The melting of ice and glaciers in Arctic, Greenland ad Antartica. This leads to an increase in the sea level
The oceans become warmer, destroying the planktons and affecting the food chain
The changes in the Earth's climate. The occurrence of the flood and drought becomes more frequent
Acid rain
Formed when acidic gases such as sulphur dioxide and oxides of nitrogen dissolve in water vapour in the atmosphere before falling to the Earth as acid rain in the form of nitric acid and sulphuric acid
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When rocks melt into magma, their volume increases and becomes less dense than the rocks in the surroundings
Factors causing acid rain:
The effect of acid rain:
The burning of fossil fuels such as petroleum and coal in power station, factories and motor vehicles releases sulphur dioxide and nitrogen dioxide into the air
The process of smelting tin releases sulphur dioxide
Open burning of non-biodegradable materials such as plastic releases sulphuric acid
Acid rain also occurs naturally through volcanic eruptions that release sulphur dioxide, nitrogen dioxide and carbon monoxide gases
Reduces the fertility of soil and plants
Damages forests
Increases the acid content in the soil, making the soil infertile. This affects the yield of crops
Destroys the photosynthesis cells in the leaves. Thus, the leaves cannot carry out photosynthesis. The plants will wither and die
Damages buildings and the external structure of buildings
Aquatic ecosystem will be affected. Aquatic plants and planktons are destroyed due to the reduction in the pH values of the water in the lakes, rivers and oceans
Sinkholes
Quicksand
Sinkholes are holes in the ground caused by the collapse of the surface of the ground
The occurrence of sinkholes is related to the types of rocks and soil and also underground water drainage
Sinkholes usually formed due to dissolution of rocks when there are water soluble rocks such as salt or gypsum, or sedimentary rocks containing carbonates, like limestone and dolomite
Quicksand forms in saturated loose sand when the sand is suddenly agitated.
When water in the sand cannot escape, it creates a liquefied soil that loses strength and cannot support weight and will suck down objects that fall into it
Quicksand usually occurs in areas with weak structure of soil such as spring, riverbanks, lakes, swamp or coastal areas.
Technology Used to prepare for Geohazards
Seismograph
A device used for recording seismic wave amplitude at a specific point above surface of the Earth.
Measures the earthquake magnitude using a graphical presentation called seismogram
Used to get information about the magnitude, depth and location of the earthquake and to predict the epicenter of the earthquake
Shock absorber
Tsunameter and tsunami buoy
installed in skyscrapers and bridges to absorb earthquake shaking
Decrease the risk of collapsing and damaging the buildings during earthquakes
Used to confirm the presence of tsunami waves due to the undersea earthquakes
Measures the change in the height of the water by measuring the changes in the water pressure. The information recorded by tsunameter is sent to tsunami buoy
By using this technology, the changes in sea level can be detected and this improves the capability of early detection of the tsunami before it hits the land
Tsunami buoy then sends the information to the tsunami warning center through satelites
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9.5 Age of the Earth
Geological Time Scale
The chronological arrangement of geological events. It is used by geologists and Earth scientists to describe the relationship of events that have occurred during the history of the Earth
Used today in the 18th century and is continuously improved over the time. The geological time scale is considered as estimated real geological time made based on carbon dating using the oldest radiometric techniques and fossil age found in the layer of the rocks.
Is divided into four eras, namely cenozoic, mesozoic, paleozoic and precambrian.
Each era is divided into several durations known as period
Determining the Age of the Earth
Through study and research by modern scientists since the late 18th century, the Universe was formed about 13.7 billion years ago from a major explosion
The method to determine the age of the Earth consists of 2 ways:
Based on the research done by scientist and geologists using radiometric dating method, the age of the Earth is estimated about 4.6 billion, which is younger than the Universe
Relative dating:
Used to determine the approximate age of a fossil by comparing the similar rocks and fossils of known ages. For example, by comparing the layers of rocks formed earlier and the layer of rock formed later.
Is less accurate because it dosen't show the age of the rock in the unit of time
Absolute dating
Used to determine a precise age of a rock or fossil through the radiometric dating method
Uses radioactive decay properties of radioactive elements contained in the rock to determine the age of the rocks. This radioactive decay process occurs at a constant rage for each radioactive element. Due to this, we can use it to determine the age of the rocks and fossils
Radioactive elements are normally found in fossil embedded rocks
The common type of radioactive decay used by geologists in radioactive decay of carbon-14 into nitrogen-14
By comparing the remaining total amount of carbon-14 and the total amount of nitrogen-14 in a fossil, the age of the fossil can be determined
Fossils
The remains or traces of organisms whether plants or animals that lived in the past which were naturally preserved in the rocks
Most fossil is found embedded in sedimentary rocks such as limestones, sandstone and shale
Found in the form of skeletons or animal bones, shells, leaves and plant woody parts that have been preserved or in the form of footprints or animal trail only.
The importance of fossils to science:
The process of fossil formation takes a very long time, which may reach to million of years
Fossils are discovered when the rocks that contain fossils are exposed by natural weathering processes and human exploration activities.
The fossil record explains the biodiversity of prehistoric organisms, including all animals, plants and microorganisms that ever existed
The fossil record becomes a guideline on the history of living organisms on the Earth
The fossil record provides information about species that have become extinct
Through carbon dating on fossils, the age of an area or historical remains can be determined
9.6 Earth's Resources and Applied Geology
Surface water
Surface water may affected by human activities. Therefore, surface water is at risk experiencing the following:
Surface runoff formed when rainwater could not seep into the soil because the soil is saturated with water due to rainfall exceeding the rate of soil absorption
Rainwater sweeps into the soil and some flows on the surface of the Earth or slopes as surface runoff
Water found on the surface of the Earth such as ponds, lakes, swamps, rivers and seas
a. Pollution
Surface water can be polluted by waste materials that are released into the rivers, lakes and seas from residential and industrial areas
Surface water near agricultural areas is polluted due to the use of excessive fertilisers and pesticides
b. Dryness
c. Destruction
Besides pollution, surface water is also at the risk of getting dry. This may be caused by drought due to global climatic change as well as the phenomenon of global warming
Natural water catchment areas such as lakes may be destroyed due to unplanned land development
Underground Water
Originated from water that falls to the ground such as rain or snow that seeps into the soil
The depth of land where the layer of the underground water started varies, depending on the thickness and location of the layer of soil above it
Is water found in the layer beneath the surface of the ground
Soil and most rocks are porous, causing water to absorb into it. When the soil and rocks are saturated, they cannot absorb water anymore. The stagnant there. The underground water stagnant is also known as an aquifer.
The importance of underground water and its risk:
May experience vaporisation due to the heat of magma in the Earth's mantle, causing it to burst into steam and gushes spraying and spurting, hot water within the Earth also comes out as hot springs
Springs are formed when the pressure in the aquifer causes some water to flow out to the surface of the Earth.
a. Humans have been using underground water for thousands of years and are still using it until now, as a drinking water source and for irrigation activities
b. Factors that contribute to underground water pollution:
Rapid urbanisation activities have resulted in the increase of domestic waste disposal and sewage discharges into the rivers that may affect the water quality and thus causing underground water pollution
Rapid industrial activities increase plant waste discharges into water sources and cause sleeping of polluted water into the soil.
Agricultural activities such as excessive use of fertilisers and pesticides cause pollution of underground water sources with high sulfate and phosphate content
Economic Minerals
A rare earth mineral contains one or more rare earth elements as main metal components
Non-metallic minerals
Metallic mineral
Economic minerals are materials that have economic values. Economic minerals consist of metallic minerals, non-metallic minerals, and rare earth minerals
The main materials that form the Earth and other planets. Minerals are inorganic solid compounds that are formed naturally
Minerals that contains metals
Are found naturally in the Earth's crust as metal ores such as tin ore (cassiterite), iron ore (hematite), pyrite, lead ore (galena) and aluminum ore (bauxite) or found as free metals such as silver and gold
Include mineral fuels such as petroleum, natural gas and coal
Other examples of non-metallic minerals are sand, limestone, granite, quartz, kaolin and marble
Formation of petroleum and Natural Gas
Examples of fossil fuels. Petroleum and natural gas are formed from decaying organic matter such as phytoplankton residues and the remains of animals and plants that lived millions of year ago.
The decayed organic matter is mixed with mud and buried under heavy layers of sediment
Under extremely high heat and within hundreds of years of millions of years, the sediment of organic waste residues transform into petroleum and natural gas
Name
Uses
Petroleum
Gold, Silver
Tin
Sand
Fuels for vehicles, for making solvent, plastic and soap
For making coins, jewellery and art works
For coating cans, making cans, welding electronic devices
For making bricks, cement and glass items
Formation of coal
Formed from the remains of plants (trees, ferns, and mosses) that lived millions of years ago in swampy areas
Organic waste materials from the dead plants experienced high pressure and heat due to the pressure exerted by the buried sediment on them and turned them into coal
Hydrothermal
The hot spring area can also become a recreational park and this is a potential attraction of eco-tourism. For example, hot spring in Sungai Klah, Perak and hot spring in Poring, Kundasang, Sabah
Hydrothermal sources that have low to medium temperatures (20c - 150c) are used to supply direct heating to homes, commercial buildings and industries
Steam from hot spring and geysers is used to rotate the turbine to generate electricity
commonly occurs near sources of heat in the Earth's crust such as near the volcanoes. An example of hydrothermal is underground hot water that spurts out geysers and hot springs
Circulation refers to the circulation of hot water from the hot rock area to a cold rock area in the Earth's crust
Related to the action of hot water in the Earth's crust. 'Hydro' means water and 'thermal' means temperature