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This course explores the fascinating world of intrusive (plutonic) rocks, including their formation, types, and significance in geology. We delve into large plutons like batholiths and stocks, as well as tabular forms such as sills and dikes. Learn about the cooling process that allows crystal growth, the relationship with geothermal features like geysers and hot springs, and the advantages and disadvantages of geothermal energy. Join us to discover the balance of movement and stillness in nature, as described by Francis Bacon.
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In nature things move violently to their placeand quietly in their place. - Francis BasonIntrusive rocks Lecture 6 Webpage for course (daytime) Webpage for course (nighttime)
long cooling time allows crystals to grow larger Intrusive (plutonic) rocks pluton
Pluton: large intrusive igneous rock body can take a variety of shape and sizes massive tabular
Tabular plutons, two general types D I S C O R D A N T CONCORDANT
D I S C O R D A N T Tabular plutons, two general types CONCORDANT Example: sill Example: dike
Massive plutons, two general types Bathylith (“deep rock”) > 100 square km stocks < 100 square km
Associated with modern magma chambers - geysers - hot springs “Old Faithful” Yellowstone N. P. Fig. 10.18
“Old Faithful” http://www.nps.gov/archive/yell/tours/livecams/oldfaithful/images/oldfaithfulbehivelabeled.jpg&imgrefurl=http://www.nps.gov/archive/yell/tours/livecams/oldfaithful/oldfaithfulphoto.htm&usg
Geothermal Energy Advantages • Disadvantages Need Shallow Magma chamber Inexpensive (after initial cost) Long lasting Low environmental cost
(still have time??) The metric system!
Why metric? Convenience Accuracy Economy