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Joel Leonard Sample GLG310 final project presentation (this one went a bit long…)

Joel Leonard Sample GLG310 final project presentation (this one went a bit long…)

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Joel Leonard Sample GLG310 final project presentation (this one went a bit long…). Lake Pleasant South Park Rd. Joel Leonard GLG 310 Structural Geology Final Presentation. Scope. Generally identify/categorize major lithologic units in the area - PowerPoint PPT Presentation

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Page 1: Joel  Leonard Sample GLG310 final project presentation (this one went a bit long…)

Joel LeonardSample GLG310 final project presentation (this one went a bit

long…)

Page 2: Joel  Leonard Sample GLG310 final project presentation (this one went a bit long…)

Lake PleasantSouth Park Rd.

Joel LeonardGLG 310 Structural Geology

Final Presentation

Page 3: Joel  Leonard Sample GLG310 final project presentation (this one went a bit long…)

Generally identify/categorize major lithologic units in the area

Identify structural features within the units Set temporal boundaries for structural

features

Scope

Page 4: Joel  Leonard Sample GLG310 final project presentation (this one went a bit long…)

Observations

Page 5: Joel  Leonard Sample GLG310 final project presentation (this one went a bit long…)

Observations

Stratified Breccia – Fan Breccia/Debris Flows

Page 6: Joel  Leonard Sample GLG310 final project presentation (this one went a bit long…)

Observations

Felsic Igneous: Flow foliated

Page 7: Joel  Leonard Sample GLG310 final project presentation (this one went a bit long…)

Observations

Gneiss: nice…

Page 8: Joel  Leonard Sample GLG310 final project presentation (this one went a bit long…)

Observations

Intrusion Breccia

Page 9: Joel  Leonard Sample GLG310 final project presentation (this one went a bit long…)

Observations

Roadcuts…

Page 10: Joel  Leonard Sample GLG310 final project presentation (this one went a bit long…)

Observations

The Missing Link

Page 11: Joel  Leonard Sample GLG310 final project presentation (this one went a bit long…)

Area is dissected by at least two temporally distinct intrusive igneous events.

Felsic intrusions pre-date mafic intrusions Mafic intrusions occurred syndepositionally

to Fan breccia/Debris flow breccia. Faulting occurs last

Felsic intrusions>Deposition>Mafic Intrusions>Deposition>Faulting

Conclusion