chapter 01
DESCRIPTION
intro chapter to the courseTRANSCRIPT
![Page 1: Chapter 01](https://reader033.vdocument.in/reader033/viewer/2022052823/55575ce2d8b42a94728b4711/html5/thumbnails/1.jpg)
SC1150 ENVIRONMENTAL GEOLOGYQUIZ 0 RESULTS
This group:- Needs a science course (27%)- Finds geo interesting (33%)- Feels the info is necessary (27%)- Does not expect EnvGeo to be easy
…
Where should we spend our money in MN?
Ranked answers
need to know
sounds easy
interesting
need a
science
other: told I had to;
needed elective; important for
career
![Page 2: Chapter 01](https://reader033.vdocument.in/reader033/viewer/2022052823/55575ce2d8b42a94728b4711/html5/thumbnails/2.jpg)
SC1150 ENVIRONMENTAL GEOLOGY
Jeff Bartlett [email protected]
QUIZ 0 RESULTS: most people already know some geology
Just one sticking point !
T F
water = over half Earth’s surface 93% 7%
water = over half the Earth’s volume 75% 25%
rocks are made of minerals 100%
there’s more oil than coal 25% 75%
drought is a MN concern 81% 19%
glaciers were important in MN landscape 88% 13%
![Page 3: Chapter 01](https://reader033.vdocument.in/reader033/viewer/2022052823/55575ce2d8b42a94728b4711/html5/thumbnails/3.jpg)
Your news items: ripped from the headlines
![Page 4: Chapter 01](https://reader033.vdocument.in/reader033/viewer/2022052823/55575ce2d8b42a94728b4711/html5/thumbnails/4.jpg)
The Basic Idea
This course includes the examination of Earth processes that influence human activities.
Topics include Earth development, rocks and minerals, internal Earth processes, surface Earth processes, Earth resources, pollution, and waste disposal.
Environmental Geology [email protected]
![Page 5: Chapter 01](https://reader033.vdocument.in/reader033/viewer/2022052823/55575ce2d8b42a94728b4711/html5/thumbnails/5.jpg)
Environmental Geology: the‘environmental’ part
Connects the lithosphere to the hydrosphere, atmosphere, biosphere & human sphere
You
are
here
Environmental Geology [email protected]
![Page 6: Chapter 01](https://reader033.vdocument.in/reader033/viewer/2022052823/55575ce2d8b42a94728b4711/html5/thumbnails/6.jpg)
Scientific MethodHypothesis is formed to explain
observations or dataMakes predictions to test repeatedly and systematically
Conclusion includes direction for further questions - actually continues a cycle
Environmental Geology [email protected]
But really – is this how our investigations work?
wired.com
Chaos – accidents and dead ends are very very common
Mysteries drive curiosity Practical issues drive projectsEconomics is important for
stakeholders
![Page 7: Chapter 01](https://reader033.vdocument.in/reader033/viewer/2022052823/55575ce2d8b42a94728b4711/html5/thumbnails/7.jpg)
Scientific Method
Environmental Geology [email protected]
Actual hypothesis – experiment – result type process
‘Beauty is in the eye of the beer holder’: People who think they are drunk also think they are attractive
Examples of traditional experimental science
![Page 8: Chapter 01](https://reader033.vdocument.in/reader033/viewer/2022052823/55575ce2d8b42a94728b4711/html5/thumbnails/8.jpg)
Geology and the Scientific MethodGeology has unique issues A pressing environmental
issue: Tuvalu and sea level change
“Tuvalu is growing” USGS, 2010
“Sinking feeling in Tuvalu” BBC, 2002
Geology is an environmental scienceRocks record how earth has changedControl of erosion and sedimentationExtraction of resourcesRecognition and mitigation of hazardsIssues with scaleA river is not easily fit within a laboratoryPlate tectonics involves the whole EarthProblems with timeGeologic processes take millions of yearsGeologists are limited by human timeProblems with resolution of dataNew technology and proceduresWe can see more details now
Environmental Geology [email protected]
![Page 9: Chapter 01](https://reader033.vdocument.in/reader033/viewer/2022052823/55575ce2d8b42a94728b4711/html5/thumbnails/9.jpg)
Anyone can be a geologist
What it really takes :
Observation– either natural or controlled
circumstances
Reasoning drive curiosity
Evidence to collect and assess important step!
Environmental Geology [email protected]
Progress includes both conclusions and new questions
![Page 10: Chapter 01](https://reader033.vdocument.in/reader033/viewer/2022052823/55575ce2d8b42a94728b4711/html5/thumbnails/10.jpg)
Formation of the solar systemFormation of the earthComposition of the earth
Interaction with humanityGeologic hazardsPopulation
An Overview of Our Planetary EnvironmentChapter 1
Environmental Geology looks at interactions between
humans and geologic environments
Environmental Geology [email protected]
![Page 11: Chapter 01](https://reader033.vdocument.in/reader033/viewer/2022052823/55575ce2d8b42a94728b4711/html5/thumbnails/11.jpg)
Setting the stageThe Big Bang Theory is the dominant scientific theory about the origin of the universe. widely accepted, but hard to prove
The universe was created 10 - 20 billion years ago from a cosmic explosion that hurled matter and in all directions.[latest estimate = 13.8ish]
Very smallest particles were forced into larger particles, then basic atoms of lightest elements: 1H, 2He, 3Li, and so on up to 16O
Environmental Geology [email protected]
![Page 12: Chapter 01](https://reader033.vdocument.in/reader033/viewer/2022052823/55575ce2d8b42a94728b4711/html5/thumbnails/12.jpg)
Stellar furnacesBigger elements had to be fused in stars themselves… that gets up to iron , 56Fe
Environmental Geology [email protected]
What about very heavy elements like gold, 197Au?
Elements have to form during solar collapse, and resulting supernova explosions
The only known process with energy that can form these elements…
![Page 13: Chapter 01](https://reader033.vdocument.in/reader033/viewer/2022052823/55575ce2d8b42a94728b4711/html5/thumbnails/13.jpg)
Solar systemFormed ~5 billion years ago, out of swirling mass of gas and dust - the ‘solar nebula’Planet compositions dependedon distance from the hot sunnear = rocky / metallic far = gaseousNearest planets: metallic iron, few very high temp minerals, little water or gas. Farther from the sun: lots of low temp minerals, water, & condensed gases.
Environmental Geology [email protected]
1.4
5.6
g/c
c
Planet #3:• >4 billion years old• 15 o C, not really
too hot or cold• Tilted >20º• Rocky with gases
![Page 14: Chapter 01](https://reader033.vdocument.in/reader033/viewer/2022052823/55575ce2d8b42a94728b4711/html5/thumbnails/14.jpg)
Earth – planetary formation
One impact made our moonAs cooling progressed, dense materials [Fe] sanklighter, low-density minerals [Si] floated out toward the surface
Early Earth – a barren world with a cratered surface Earth was target of many impacts
Asteroids MeteorsComets Dust Particles
Environmental Geology [email protected]
= =
![Page 15: Chapter 01](https://reader033.vdocument.in/reader033/viewer/2022052823/55575ce2d8b42a94728b4711/html5/thumbnails/15.jpg)
Earth – differentiation and change
Heat from core escapes by convection, keeping the planet constantly changing
Figure 1.4
Differentiation Core: dense, hot
Ni + FeMantle: thick zone that
surrounds the coreMushy, hot ultramafic rocks
Crust: Zone of interactionOceanic (mafic)continental (felsic)
Environmental Geology [email protected]
![Page 16: Chapter 01](https://reader033.vdocument.in/reader033/viewer/2022052823/55575ce2d8b42a94728b4711/html5/thumbnails/16.jpg)
Composition
Crust has loads of Si, O, and Al
Atmosphere lacked free oxygen (O2)Dominated by N, CO2 & SO2
A
Heating and differentiation of the early earth formed crust, atmosphere and oceans. Minerals released gasesImpacts brought extraterrestrial elements!
Environmental Geology [email protected]
![Page 17: Chapter 01](https://reader033.vdocument.in/reader033/viewer/2022052823/55575ce2d8b42a94728b4711/html5/thumbnails/17.jpg)
Early environment
Very early in the world, life began and interacted with the earth
Earliest fossils show that bacteria used ancient atmosphere and ‘polluted’ the seas with O2 Iron rained out of seas
Result – oxygen in the atmosphere, and iron in the rocks!This is a great example of a feedback between biosphere, lithosphere and atmosphereEcological interactions were responsible for changing the world: We would not exist if they hadn’t
Environmental Geology [email protected]
Curiosity Rover Finds No Sign of Methane
![Page 18: Chapter 01](https://reader033.vdocument.in/reader033/viewer/2022052823/55575ce2d8b42a94728b4711/html5/thumbnails/18.jpg)
Geologic Hazards
Rising tide of acid mine water
threatens Johannesburg
Fig 1.6-1.9
A dangerous place!
Partly because of us:- Choosing to live near hazards- Poor understanding- Contributing to risk
Residents on edge over eroding bluff
Environmental Geology [email protected]
![Page 19: Chapter 01](https://reader033.vdocument.in/reader033/viewer/2022052823/55575ce2d8b42a94728b4711/html5/thumbnails/19.jpg)
Population GrowthExponential growth:
• Possibly 9 billion people by 2050
• Life span & birthrate up, mortality down
• Mass mobility
Inflection [change] point:• Acceleration is
slowing to zero• Population decline
in many countries
Environmental Geology [email protected]
Overcrowding? Nah — the World’s
Population May Actually Be Declining
![Page 20: Chapter 01](https://reader033.vdocument.in/reader033/viewer/2022052823/55575ce2d8b42a94728b4711/html5/thumbnails/20.jpg)
Global population density
Figure 1.18
Figure 1.15
Environmental Geology [email protected]
Density is highly variable and depends on resources, space, culture, economics etc
![Page 21: Chapter 01](https://reader033.vdocument.in/reader033/viewer/2022052823/55575ce2d8b42a94728b4711/html5/thumbnails/21.jpg)
Environmental Geology [email protected]
The Earth has some time left before the sun gets too hot. Based on their models, the scientists calculate that the planet will fall out of the habitable zone some time in the next 1.75bn to 3.25bn years. Then, the habitable zone will start beyond Earth's orbit, and make Mars more earth-like
Earth Expected to Be Habitable for
Another 1.75 Billion Years