DOC PREVIEW
UA GEO 102 - how the earth works
Type Lecture Note
Pages 2

This preview shows page 1 out of 2 pages.

Save
View full document
View full document
Premium Document
Do you want full access? Go Premium and unlock all 2 pages.
Access to all documents
Download any document
Ad free experience
Premium Document
Do you want full access? Go Premium and unlock all 2 pages.
Access to all documents
Download any document
Ad free experience

Unformatted text preview:

GEO 102 Lecture 10Outline of Last Lecture I. How the earth works Outline of Current Lecture II. Rock TypesIII. IgneousIV. MetamorphicV. SedimentaryCurrent LectureRock Types► Igneous-Extrusive-Intrusive► Metamorphic-Differing grades -Differing stress► Sedimentary-Clastic-Chemical-When two oceanic plates meet the older and the colder plate sinks-younger rock is more buoyant-When two continental plates meet nothing sinks. Mountains form.These notes represent a detailed interpretation of the professor’s lecture. GradeBuddy is best used as a supplement to your own notes, not as a substitute.-The passive margin is the back part of the plate.-most extrusive igneous rocks form on divergent boundaries.-Water: evaporates, plants use it, percolates down to become groundwater, flows to the river and down to the


View Full Document

UA GEO 102 - how the earth works

Type: Lecture Note
Pages: 2
Download how the earth works
Our administrator received your request to download this document. We will send you the file to your email shortly.
Loading Unlocking...
Login

Join to view how the earth works and access 3M+ class-specific study document.

or
We will never post anything without your permission.
Don't have an account?
Sign Up

Join to view how the earth works 2 2 and access 3M+ class-specific study document.

or

By creating an account you agree to our Privacy Policy and Terms Of Use

Already a member?