1) Use the legends at the bottom of the map to find the locations where metallic sulfide and gold deposits have been identified. Which mountain is closest to the deposits? 2) The hydrothermal fluids carrying the metallic minerals came from igneous rocks, but did they deposit those minerals within igneous rocks? From the map, identify the rock type (igneous or sedimentary) where most of the ore minerals are deposited. 3) Why do you think the ore deposits formed within that rock type?

Applications and Investigations in Earth Science (9th Edition)
9th Edition
ISBN:9780134746241
Author:Edward J. Tarbuck, Frederick K. Lutgens, Dennis G. Tasa
Publisher:Edward J. Tarbuck, Frederick K. Lutgens, Dennis G. Tasa
Chapter1: The Study Of Minerals
Section: Chapter Questions
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1) Use the legends at the bottom of the map to find the locations where metallic sulfide and gold deposits have been identified. Which mountain is closest to the deposits?

2) The hydrothermal fluids carrying the metallic minerals came from igneous rocks, but did they deposit those minerals within igneous rocks? From the map, identify the rock type (igneous or sedimentary) where most of the ore minerals are deposited.

3) Why do you think the ore deposits formed within that rock type?

4) Now look at the high-angle faults shown in the map. Faults often provide pathways for fluids bearing metallic minerals. What is the spatial relationship between the high angle faults and the metallic sulfide and gold deposits? Note: consider "close" to mean within ~500 m.

5) Based on this geologic map and your answer to the question above, what locations are reasonable places to look for similar deposits? Base your answer on whether the rocks that might house those deposits and/or faults that might carry the mineral-bearing fluids are present. 

6) The area around Homestake Mine, Montana, is currently under a “no-mining” rule. In the future, there is a high probability that this region will see active mining once again.
There is a high likelihood of earthquakes in this region due to the igneous activity under Yellowstone National Park, and while most of the earthquakes are small, there have been some large earthquakes (such as a magnitude 7.3 in 1959) in the region. What type(s) of environmental concern(s)/hazards would a large earthquake pose to a mine? Explain your answer.

Handout 1: Generalized Geologic Map of the Area around Homestake Mine
Map modified after Figure 2 of USGS Special Paper 1717, Chapter M: Van Gosen, Bradley S. "The Life Cycle of Gold Deposits Near the Northeast
Corner of Yellowstone National Park–Geology, Mining History, and Fate." (2007). (http://pubs.usgs.gov/pp/1717/downloads/pdf/p1717M.pdf)
110°57'30"
Scotch Bonnet
Mountain
Fisher
Mountain
Homestake
mine
Henderson
Mountain
45°02'30"
4000 feet
1000 meters
Metalic sulfide and gold deposits
High-angle faults*
50-40 Million Year old extrusive rocks and lava flows
Detachment faults*
50-40 Million Year old intrusive rock formations
50-40 Million Year old volcanic rock formations
Contacts
50-40 Million Year old volcanic pipes shattered during eruption
*Faults=a break in rock
Sedimentary rocks and unconsolidated surface deposits
layers. Fluids bearing
minerals often travel
along faults
>2,500 million years old igneous and metamorphic rocks
Transcribed Image Text:Handout 1: Generalized Geologic Map of the Area around Homestake Mine Map modified after Figure 2 of USGS Special Paper 1717, Chapter M: Van Gosen, Bradley S. "The Life Cycle of Gold Deposits Near the Northeast Corner of Yellowstone National Park–Geology, Mining History, and Fate." (2007). (http://pubs.usgs.gov/pp/1717/downloads/pdf/p1717M.pdf) 110°57'30" Scotch Bonnet Mountain Fisher Mountain Homestake mine Henderson Mountain 45°02'30" 4000 feet 1000 meters Metalic sulfide and gold deposits High-angle faults* 50-40 Million Year old extrusive rocks and lava flows Detachment faults* 50-40 Million Year old intrusive rock formations 50-40 Million Year old volcanic rock formations Contacts 50-40 Million Year old volcanic pipes shattered during eruption *Faults=a break in rock Sedimentary rocks and unconsolidated surface deposits layers. Fluids bearing minerals often travel along faults >2,500 million years old igneous and metamorphic rocks
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