Geo 101 Lab 1 Measurements and Measuring-4
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101
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Geology
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Dec 6, 2023
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Cochise Community College
Geology 101
Instructor: J.Deakin
Laboratory One
Observing and measuring Earth Materials and Processes
Objectives:
1.
Know what the geologic record is and how it is similar yet different from a book.
2.
Know that Geology is based on a logical, testable process of science that is ground truthed with data obtained
by direct observation, investigation and measurement in the field and in the laboratory.
3.
Measure and calculate length, area, volume, mass and density of Earth materials using basic scientific
equipment and techniques.
4.
Develop and test physical and quantitative models of isostasy based on floating wood blocks and icebergs.
Apply these concepts to basalt and granite densities to calculate the isostasy of average blocks of oceanic and
continental crust.
Introduction: Thinking About Time
Two key features of geoscientists' temporal thinking distinguish them from the general population: They take a long view
of time, and they expect low-frequency, high-impact events. Geoscientists have internalized the vastness of the age of the
Earth and the relative brevity of human history. They can envision Earth in states drastically different from the planet
they have personally experienced: an Earth without humans, an Earth without life, a hothouse Earth, a snowball Earth.
In the long view of time, exceedingly slow processes such as erosion or evolution can effect huge changes, such as the
removal of a mountain or the establishment of new species. Infrequent but powerful processes, such as floods, volcanic
eruptions, landslides, and asteroid impacts, are routine rather than abnormal when considered across the whole of Earth's
history.
Most People Do Not Understand Geologic Time
Substantial impediments stand in the way of society achieving a broad understanding of geologic time. Geologic time
involves scales and events far removed from human experience; thus, envisioning the cumulative impact of slow processes
or infrequent events over geological timescales is not intuitive. Scientists' timekeeping tools rely on exponential numbers,
ratios, and proportional reasoning, all of which present well- documented difficulties for many students. Finally, some
religious teachings oppose the idea of an old Earth.
The most widely known geologic feature in the United States is probably the Grand Canyon.
It is a mile deep and cuts
through millions of rock layers that are like pages of an immense stone book of geologic history called the geologic record.
The layers are like pages and vary in thickness, but no one layer is exactly like another.
Each has distinguishing features
such as tiny microscopic fossils or grains of sand and some have large fossil trees, dinosaur bones or ancient stream
channels.
These stone pages have recorded the events of the past and are there for us to read.
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From:httphttp://images.nationalgeographic.com/wpf/media-live/photos/000/696/cache/skywalk-grand-canyon-
arizona_69640_990x742.jpgl
Spatial and Temporal Scales
Spatial scales are used by geologists to study Earth materials from the smallest atoms to the entire globe.
At each spatial
scale of observation, they identify materials and characterize relationships.
Each scale is related to the others as shown
in the table below.
SCALE OF OBSERVATION
USED TO STUDY THINGS
LIKE….
MEASURED IN….
GLOBAL
ENTIRE PLANET AND ITS
INTERACTIVE SPHERES
THOUSANDS OF KILOMETERS
OR MILES
REGIONAL
PORTIONS OF OCEANS,
CONTINENTS, COUNTRIES,
PROVINCES, STATES OR
ISLANDS
KILOMETERS AND MILES
2
LOCAL (OUTCROP OR FIELD
SITE)
SPECIFIC LOCATIONS THAT
CAN BE PIN POINTED ON A
MAP
METERS AND FEET
HAND SAMPLE (FIELD OR
LAB SAMPLE
SAMPLE OF A MINERAL OR
ROCK, AIR, WATER OR AND
ORGANISM THAT CAN BE
HELD IN YOUR HAND
CENTIMETERS, MILIMETERS
AND INCHES
MICROSCOPIC
FEATURES OF A HAND
SAMPLE THAT CAN ONLY BE
SEEN WITH A HAND LENS
(MAGNIFIER OR MICROSCOPE)
FRACTIONS OF
MILLIMETERS AND
MICROMETERS
ATOMIC
ARRANGEMENTS OF THE
ATOMS AND MOLECULES IN A
SUBSTANCE
Geologists also think about temporal scales of observation. They group the events, and relationships into paragraphs,
chapters, sections and parts of geologic history that has occurred over epochs, periods eras and eons of time. The index of
this geologic book is called the geologic time scale. Notice that it is a chart showing named intervals of the geologic record
(rock units), the sequence in which they formed (oldest at the bottom) and their ages in millions of years.
3
From: http://factsanddetails.com/world.php?itemid=2213&catid=51&subcatid=323
Questions:
1.
Match each item below with the appropriated scale that should be used to study it.
a.
The Grand Canyon ______________
b.
The Mississippi River______________
c.
The Earth’s Atmosphere______________
d.
The Paul Spur Reef (this is located on highway 80 towards Bisbee, see picture at end of lab)
_______________
e.
The arrangement of atoms in a diamond________________
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f.
A quartz crystal_____________
2.
Recall that the geologic record is the millions of rock layers that record events and times in geologic history. Also
recall that the geologic time scale is a chart showing named intervals of the geologic record and their ages in
millions of years.
a.
Compare and contrast the geologic record with a history book. How are they the same? How are they
different?
___________________________________________________________________________
___________________________________________________________________________
___________________________________________________________________________
_______________In what geologic period of time did the first amphibian appear on Earth?
_________________________________
b.
What era was this? ________________________________
c.
How many years ago was this? ________________________
d.
How old is the Earth in millions of years?
e.
How long ago did man evolve? _________________________
f.
When did the dinosaurs go extinct? ____________________
3.
During the Paleozoic, 290 to 350 million years ago two periods called the Mississippian and Pennsylvanian
occurred.
These two periods are lumped together and often referred to as the Carboniferous.
Why do you think
geologists call this time the Carboniferous?
______________________________________________________________________________
______________________________________________
Field Geology and Lab Work
The most reliable information about Earth is obtained by direct observation, investigation and measurement in the field
and laboratory. Most geologists study outcrops – field sites where rocks crop out, stick out of the ground. The outcrops
are comprised of minerals.
Samples obtained in the field are often moved to the lab for further analysis.
Physical and
chemical analysis and tests can be done to determine the composition of the rock sample.
Many times the rocks are
crushed and powdered then put into a solution where a qualitative analysis is performed to determine the chemical
composition.
This technique is often used at mines to determine the percentage of gold, silver or other precious metals in
an ore (host rock) and is called an assay.
In an assay both a qualitative and a quantitative assessment are performed to
determine how much and what type of elements are in the sample. The mineral chalcopyrite is a good example.
Chalcopyrite is a copper bearing mineral that is mined, crushed, put into solution with detergents and water, and finally
agitated.
The chalcopyrite rises to the surface because it is less dense then the other constituents.
These small grains are
skimmed off and then smelted (roasted) to separate the copper from the other parts of the chalcopyrite and melted rock
(slag).
The remaining copper powder is then leached in sulfuric acid and subjected to electrolysis, whereupon the copper is
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