HSHM 211 Lecture 3: Global Catastrophe 3
Premium

4 Pages
80 Views
Unlock Document

Department
Hist of Science, Hist of Med
Course
HSHM 211
Professor
William Rankin
Semester
Spring

Description
HSHM 211: GLOBAL CATASTROPHE SINCE 1750 1/30/17: Continental drift and its discontents  Plate tectonics 1. Convection currents are the motor 2. Measure motion using GPS  Mass extinction 1. Events causing major environmental change 2. Punctuated equilibrium: neo-Darwinian  How do uniformitarianism and catastrophism coexist? 1. Changing standards of evidence, what it takes for theory to be accepted a. Change from the generally reasonable explanation to the smoking gun o Smoking gun: single piece of evidence from which other things follow  Does not establish fact, we just know that this happened o Does not establish entire explanation but establishes a fact from which other things come 2. How theories change over time a. Paradigm shifts? Scientific revolutions?  Late 19 through mid-20 centuries 1. Do continents move? a. Same facts explained by different theories b. No theories were perfect  Fixism vs. mobilism 1. Fixism (uniformitarianism): earth’s continents have stayed in the same place forever a. Cooling earth as theory of continents o James Dwight Dana (1813-1895): smooth earth with thin ocean that contracted and caused earth to cool, as contraction continued oceans became deeper  Uniformitarianism o Edward Suess (1831-1914): as earth cools, periodically continents will slump and become oceans, and ocean floors will stay in place and become continents  Catastrophism 2. Mobilism (catastrophism): earth’s continents have moved over time a. Alfred Wegener (1880-19): continental drift, 1912 b. Arthur Holmes: continent can be split apart by convection currents, 1929  Do theories need to be supported, or do theories do the supporting? 1. Mountains a. Wegener: mountains are zones of collision o Explained why mountains mostly at edges but also at interior (when continents collide and generally older) b. Dana: oceanic crust becomes deeper/thicker by cooling temperatures c. Dana/Suess synthesis: 2. Fossils: alignment of fossils across different continents, strata, and foldings, suggesting that continents were once joined together a. Others: ancient continental links between present continents o Ancient land bridges 3. Southern glaciation 4. Which is more speculative? a. Land masses moving vertically a few thousand feet? b. Land masses moving horizontally many thousands of miles? 5. Flaws a. Fixism: o Overthrusts  Older rock sitting on top of younger rock  Only explanation: rock layers changed very radically by pressure causing older rock to end up on top of younger rock o Isostasy: earth’s crust floats on semi-liquid mantle below  Evidence: most of Scandinavia slowly rising  Himalayas did not affect earth’s gravity as much as expected if earth is solid  UK:  Continental drift makes sense  US: “Pratt interpretation” crust composed of blocks of different densities with no “roots”  Continental drift does not make sense; how can continents move if no roots?  Takeaways: 1. When faced with 2 theories, both were watertight that had their own strengths and weaknesses a. Why were people committed to one worldview over another? Rather than considering merits and pitfalls of both 2. Similar kinds of science used to come to different conclusions a. Collecting disparate evidence into a generally reasonable explanation that takes account of everything 2/1/17: Plate tectonics and mass extinctions  Fixism vs. mobilism (uniformitarianism vs. catastrophism) 1. Both explained a lot, but both had holes 2. Both were generally reasonable explanations of the earth  Plate tectonics and mass extinction 1. Standar
More Less

Related notes for HSHM 211

Log In


OR

Join OneClass

Access over 10 million pages of study
documents for 1.3 million courses.

Sign up

Join to view


OR

By registering, I agree to the Terms and Privacy Policies
Already have an account?
Just a few more details

So we can recommend you notes for your school.

Reset Password

Please enter below the email address you registered with and we will send you a link to reset your password.

Add your courses

Get notes from the top students in your class.


Submit