Lesson 7 overview
=================

In part two of the :doc:`exercises for the final two weeks of the course <../L6/intro-to-exercises>` 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 <../../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

Lesson video
------------

Lesson video will be linked below after class.

.. 
    .. admonition:: Lesson 7.1 - Final paper update and Exercise 7 overview
        :class: admonition-youtube
    
        ..  youtube:: -zPDFRBD73o
    
        Dave Whipp, University of Helsinki @ `Quantitative Geology channel on Youtube <https://www.youtube.com/channel/UClNYqKkR-lRWyn7jes0Khcw>`_.