Logging Requirements (Please email me the answers
to these tasks and keep the details out of your log.)
- Take a look at the entire stretch of geodes and measure the
largest one you found and the smallest and send me the sizes. What
could this range tell us about their formation?
- Take a look at the colours of the crystals inside the
geodes, are they all the same? If they are not, describe the
variations and explain why you think that might happen (in terms of
geological process).
Optional Tasks:
- Measure the size and amount of geodes in one rock and
calculate the ratio (in surface area) of geodes to host rock by
taking some measurements of it as well. Why do you think that ratio
exists? What could have made that amount
increase/decrease?
- Take a picture of the coolest geode you could find and share
it with us. This is not required to log the EC, it is
totally optional, but feel free to do so.
When you reach this wall of geodes you will be amazed at how
beautiful they can be and yet so unique from one to the next. I
have always been amazed at how the geological processes of our
planet are able to manifest in such wacky ways.
What are Geodes?
Geodes are rock formations that occur within other types of
rock. For the most part they appear in sedimentary or volcanic
rock, but wherever they are they contain a beautiful
surprise.1 They may appear like a small roundish (or
bumpy) rock. They might even appear ugly, but the weight can be the
key to identifying them. They are far lighter than rocks of the
same size.
How are Geodes Formed?
Time and energy are an amazing cocktail for geological
formations and with geodes the proof is evident. Thousands of years
ago while the surrounding rock was undergoing changes, small
pockets of gas, moisture and minerals were trapped inside a host
rock formation. The outer layer hardened and allowed dissolved
silicates or carbonates to reach the inner surface. As time
continued on and mineral rich groundwater is able to "fertilize"
these pockets, crystals grow and remain there until the host rock
is removed to leave these hard little "pearls" of
wonder.2
The resulting crystals (usually quartz or calcite) are amazingly
unique and at times can grow with such enthusiasm that they can
fill the entire space. These are no longer referred to as geodes,
they are nodules. With the concentration of colours and shapes
varying from geode to geode you can spend hours analysing and
comparing all the different types. You will see at least four
different examples at GZ and all along this group of rocks. Keep
track of the variations for the logging requirements. As we walk
each day we can see evidence of our beautiful planet hard at work,
have fun turning this walk in the park into an introduction to
Geodes.
References
1. Geode
on Wikipedia
2.
Thunder Eggs & Geodes at the Australian Museum
* Special thanks to
dezerter for showing me this location.