Lecture 1 Summary Earth History dl
Introduction
Take time to explore the course materials folder and syllabus.
Be sure to do the assigned reading! You will find the assigned reading on the syllabus.
Do you know the answers to these questions? If not, review the syllabus and course materials folder again!
How is this course graded?
How do I communicate with the instructor?
What's the difference between this course and Earth Dynamics-is this about volcanos, earthquakes, rocks and minerals, too?
What major topics are covered in this course?
How Science works –
inductive and deductive approaches, testing hypotheses
How Geologists look
at Earth’s planetary history
How we can decipher
the natural history of events from long ago
What the legacy
effects of those events are for the modern world
Why understanding
major natural processes can help us understand how the planet works now and how
it worked in the past
How to Approach this dl course:
The course is divided into two parts: the "tools of the trade" and the "events and processes along the Geologic Time Scale". The first part is made of several separate topics. The second part can be followed like a long story with chapters. Many people find part II (most of the course), easier to organize than part I for this reason. Therefore, be alert and be sure to
1) review the topic summary before you listen to the lecture.
2) make notes on the topic summary or in a notebook while you listen/watch the lecture.
Introducing Major Concepts today:
1)
Scientific Method, hypothesis testing, inductive and deductive approaches.
2) Uniformitarianism/Actualism: physical and chemical processes operating today also operated in the past. Events can be singular, but processes that drive them are known and identifiable. What does this mean for us? Events can be unique, but the processes that drive them are not unique, and so in understanding the processes, we can "read" the rock record.
3)
Rock Cycle:
The process known as the Rock Cycle is important in understanding the rock
record.
Three major rock "families" exist, forming, eroding, transforming, recycling
in a continuing process: the three groups are igneous, metamorphic,
sedimentary