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Fancy Some Fun Fossicking Fossil Fauna? EarthCache

This cache has been locked, but it is available for viewing.
Hidden : 7/3/2010
Difficulty:
2.5 out of 5
Terrain:
2.5 out of 5

Size: Size:   not chosen (not chosen)

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Geocache Description:


What You Need and “Things To Be Aware Of”

There is little room to park at GZ, choose a sensible location where you can be seen from both directions along the road. Parking on the north side of the road may be easier but you'll have to cross it. There is a gateway at roughly S45 55.475 E170 26.065 on the north side of the road but you'll have a wee walk to get to GZ.

You will need: a camera and a source of acid (a bottle of vinegar - contains acetic acid should suffice). A ladder and hand lens aren't essential but could be handy.


Background

The rock that you are looking at is part of a relatively thick (over 120m) unit that crops out over a 40km coastal extent between south of Dunedin and Palmerston. This sedimentary rock formed as the ancient seas slowly receded from the Otago seabed and deposited the sediment that formed this rock. The quartz here (have a look with a hand lens) is evidence of Central Otago uplift. This uplift enhanced the river based erosion of schist, carrying the quartz here. The amount of quartz ranges from 40-70% at various depths.

Some sections of this rock yield a rich array of large fossils but you are more likely to find evidence of smaller fossils such as foraminifera, ostrocods (shrimp). These appear as white specks in the rock about the size of a biro nib. Larger fossils can be found with scrutiny (hence the ladder): bryozoans (eg coral), brachiopods, pectinids (scallop), oyster, gastropods (snails), echinoderms (eg starfish). The occasional whale bone has turned up elsewhere in the formation.

Chert showing foraminiferan fossil inclusions - Source: http://users.stlcc.edu/mfuller/petersonclovis.html

A nice sequence of rock formation occurs here: the rock you are examining is about 17 million years old and behind the road cutting within the quarry is basalt at about 14 million years in age.

Aerial View - Source: www.cityofdunedin.govt.nz

Logging Requirements

0. Preface any email with GC28W5K Fancy Some Fun Fossicking Fossil Fauna? in the subject line and title and clearly note the question number and answer. You don't need to wait for a confirmation email to log but you might be asked for more info if your answers are slim.

Sedimentary Rock Identification Key.

Source: http://www.geomore.com/Sedimentary%20Rock%20Chart.htm

1. Use the above key for identifying sedimentary rocks (and your acid) to find out what type of rock is found at GZ Email the answer.

2. Use your initiative (and your ladder if necessary) to locate a fossil in the rock, identify the type of animal as much as you can. Upload your photo (showing a fossil and your gps and what you think the fossil is.


2010 Stegan’s EarthCache Masters Programme

Since it is not very feasible for many NZers to easily get more than two states for the earthcache.org masters programme and therefore not get past Bronze I’m running my own one on a number of Earthcaches that I plan to release this year (all things being equal) with the following points system:

5 points: First to find

3 points: 2nd to find

1 point: Logging a find

1-5 points: Special bonus questions.

Shared points for joint finds.

At the end of 2010, I’ll issue certificates for 1st, 2nd and 3rd and the first place getter will be awarded a geocoin. If I feel richer and/or it looks like this is popular I’ll upgrade the prizes.

Updated information and Leaderboard at: Stegan’s Earthcache Programme


CO is open to constructive criticism on this cache (via geocaching.com messaging). Cheers!



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