Geomathematics | Wikipedia audio article
Channel: wikipedia tts
Date: 2019-02-07

This is an audio version of the Wikipedia Article:
https://en.wikipedia.org/wiki/Geomathematics


00:00:48 1 Applications
00:00:57 1.1 Terrestrial Tomography
00:01:28 1.2 Crystallography
00:02:16 1.3 Geophysics
00:03:14 1.4 Geomorphology
00:04:33 1.5 Glaciology



Listening is a more natural way of learning, when compared to reading. Written language only began at around 3200 BC, but spoken language has existed long ago.

Learning by listening is a great way to:
- increases imagination and understanding
- improves your listening skills
- improves your own spoken accent
- learn while on the move
- reduce eye strain

Now learn the vast amount of general knowledge available on Wikipedia through audio (audio article). You could even learn subconsciously by playing the audio while you are sleeping! If you are planning to listen a lot, you could try using a bone conduction headphone, or a standard speaker instead of an earphone.

Listen on Google Assistant through Extra Audio:
https://assistant.google.com/services/invoke/uid/0000001a130b3f91
Other Wikipedia audio articles at:
https://www.youtube.com/results?search_query=wikipedia+tts
Upload your own Wikipedia articles through:
https://github.com/nodef/wikipedia-tts
Speaking Rate: 0.940423480558476
Voice name: en-US-Wavenet-D


"I cannot teach anybody anything, I can only make them think."
- Socrates


SUMMARY
=======
Geomathematics or Mathematical Geophysics is the application of mathematical intuition to solve problems in Geophysics. The most complicated problem in Geophysics is
the solution of the three dimensional inverse problem, where
observational constraints are used to infer physical properties.
The inverse procedure is much more sophisticated than the normal direct computation of what should be observed from a physical system.
The estimation procedure is often dubbed the inversion strategy (also called the inverse problem) as the procedure is intended to estimate from a set of observations the circumstances that produced them. The Inverse Process is thus the converse of the classical scientific method.