Lesson 14 overview
==================
In part two of the `exercises for the final two weeks of the course <../../_static/slides/L13/Intro-to-thermochronology-overview.pdf>`__ we will combine the thermochronometer age prediction code used last week with an age dataset from the Bhutan Himalaya to quantify the long-term rates of erosion recorded in the thermochronometer data.
These results will be presented in detail in your :doc:`Final paper description <../../final-paper/final-report>`\ .

1. `Basic concepts of thermochronology lecture slides <../../_static/slides/L13/Basic-concepts-of-thermochronology-lecture-slides.pdf>`__
2. `Low-temperature thermochronology lecture slides <../../_static/slides/L13/Low-temperature-thermochronology-lecture-slides.pdf>`__ (not presented in class)
3. `Quantifying erosion with thermochronology lecture slides <../../_static/slides/L13/Quantifying-erosion-with-thermochronology-lecture-slides.pdf>`__ (not presented in class)
4. `Overview of Exercises 13 and 14 lecture slides <../../_static/slides/L13/Intro-to-thermochronology-overview.pdf>`__
5. :doc:`Exercise 14 <ex-14>`
6. :doc:`Exercise 14 hints <exercise-14-hints>`
7. :doc:`Final paper description <../../final-paper/final-report>`

Scientific journal articles
---------------------------

- :doc:`Some useful final paper references <../../final-paper/articles>`
- `Google scholar <https://scholar.google.fi/>`__
- `Web of Science <https://webofknowledge.com>`__ (Only works on campus or via VPN)

Additional materials
--------------------

- `Low-temperature thermochronology short course website <https://thermochron.github.io/2017/>`__

..
    Learning objectives
    -------------------
    After completing this week's lesson you should be able to:

        - State what a fluid is and how its flow is related to its viscosity
        - Explain why geological fluids deform in a nonlinear fashion
        - Model the flow of ice in valley glaciers using viscous flow equations