mining_sand_activity_students
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University of California, Irvine *
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Course
5B
Subject
Geology
Date
Dec 6, 2023
Type
docx
Pages
8
Uploaded by LieutenantSteelButterfly23
1
GEORGIA
FLORIDA
Trail Ridge deposit
Mining minerals from sand
Learning objectives
By completing this activity, you will:
Use ilmenite (a mineral which contains the element titanium), which is mined by DuPont
to use as a white pigment, as an example of a mineral resource formed by sedimentary
processes.
Summarize the processes that act to make clastic sedimentary rocks.
Diagram how sedimentary processes link together to form placer deposits (the heavy
mineral sands).
Explain how the sedimentary processes of mechanical weathering, erosion, and
deposition, redistribute and concentrate mineral resources.
Analyze graphs to interpret erosion and deposition processes that create heavy mineral
sand deposits.
Apply knowledge of sedimentary environment and processes to infer potential types
and locations of heavy mineral sand.
Explain how climate influences chemical weathering and how chemical weathering
concentrates certain mineral resources.
Brief background
Figure 1.
Map showing the location of the Trail Ridge heavy mineral sand deposit in Florida.
The southern portion of the deposit is being actively mined by the DuPont Corporation. Map
created using Google Maps; deposit located with Google Earth imagery and sketch map in Force,
1991.
TIC OCEAN
Layers of dark sand, rich in heavy minerals, can be mined for the heavy minerals they contain.
For example, the DuPont Corporation mines heavy mineral sand from the Trail Ridge sand
deposit in northern Florida. The mineral ilmenite is used as a source of titanium dioxide (TiO
2
),
which is used to make white plastic and paints more opaque. Other minerals, like zircon and
staurolite, are mined to be used as abrasives (to use in sandblasting and to etch tombstones, for
example).
The right combination of factors existed in central Florida to make these heavy mineral sand
deposits, and incorporate aspects of the geosphere, hydrosphere, and atmosphere. By studying
these processes, geoscientists can predict other places that might have heavy mineral deposits,
and thus guide exploration.
Part 1. How the sand at the Trail Ridge deposit came to be
Quartz is found in many rocks, but some of the heavy minerals like sillimanite and
kyanite only form in metamorphic rocks that make up the cores of mountains. These
rocks broke apart into sand. The sand was carried to the ocean by streams and deposited.
Waves picked up the sand from offshore and deposited it on the beach. Winds picked up
some of the sand and deposited it in dunes behind the beach.
1.
In the description of how the sand deposit formed, circle examples of weathering.
2.
In the description of how the sand deposit formed, draw rectangles around examples of
erosion.
3.
Draw a diagram of how the sand deposit formed.
4.
Although its exact age is not known, the Trail Ridge deposit formed in the Pliocene or
Pleistocene (sometime between 12 thousand and 5.33 million years ago). Based on
today’s location of the Trail Ridge deposit, what happened to sea level between the time
this sand was deposited and today. Explain how you came up with your answer.
Part 2. Characteristics of the heavy mineral sands, and how sedimentary processes led to
their formation
Heavy minerals
Formula
Specific
gravity
ilmenite
FeTiO
3
4.7–4.79
zircon
ZrSiO
4
4.6–4.7
staurolite
(Fe,Mg)
2
(Al,Fe)
9
O
6
(SiO
4
)
4
(O,OH)
2
3.74–3.83
sillimanite
Al
2
SiO
5
3.23–3.27
kyanite
Al
2
SiO
5
3.53–3.65
Other minerals
Formula
Specific
gravity
quartz
SiO
2
2.65
Table 1.
Some minerals found in the Trail Ridge sands. Recall, specific gravity is a mineral
property akin to density. Except for quartz, all the minerals listed are considered “heavy
minerals.”
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