Skip to content

Slesse Creek Fossils EarthCache

Hidden : 4/11/2011
Difficulty:
2.5 out of 5
Terrain:
3 out of 5

Size: Size:   not chosen (not chosen)

Join now to view geocache location details. It's free!

Watch

How Geocaching Works

Please note Use of geocaching.com services is subject to the terms and conditions in our disclaimer.

Geocache Description:

This earthcache will take you to a small tributary of Slesse Creek, where you will find fossilised Crinoids.

Fossilization is an exceptionally rare occurrence, because most components of formerly-living things tend to decompose relatively quickly following death. In order for an organism to be fossilized, the remains normally need to be covered by sediment as soon as possible.


Crinoids (sometimes refered to as "Sea Lilies") are a marine animal, (not a plant as their nickname would imply) that live in salt water. These were once abundant in ancient seas, but are still found in modern day in certain locales. They somewhat resemble a small underwater palm tree.

It is the columnal section of the crinoids that are found fossilised in this area. Below are some images of what you are looking for. It is easiest to find these when the rock is wet as the contrasted colors make them much easier to spot. These are all river tumbled specimens and the matrix that surrounds them is all very large/heavy. You may be lucky enough to find a small rock containing them, but most are more suitable for collecting via photographs than physical collection.The rock is limestone and mostly quite dark. The crinoids are all very white calcite.

Limestones are calcareous sedimentary rocks formed at the bottom of lakes and seas with the accumulation of shells, bones and other calcium rich goods. It is composed of calcite (CaCO3). The organic matter upon which it settles in lakes or seas, are preserved as fossils. Over thousands and millions of years, layer after layer is built up adding weight. The heat and pressure causes chemical reaction at the bottom and the sediments turn into solid stone, the limestone. Limestone in the Chilliwack Group is mainly recrystallized. This Lower Pennsylvanian* limestone is medium to dark grey, argillaceous**, and where the primary texture is preserved, is a calcarenite***. Most characteristic of this limestone are large crinoid columnals commonly an inch or more in diameter.



* Pennsylvanian is a time period, not a geographical location. Approx 320-290 Million years ago.
** Argillaceous limestones are limestones consisting predominantly of calcium carbonate.
*** Calcarenite is a rock formed by the percolation of water through a mixture of calcareous shell fragments and quartz sand causing the dissolved lime to cement the mass together.

In order to log this earthcache as a "find" you must email me the answers to the following questions:

1:) Using a metal object (keys, coin, knife etc.) make a scratch on one of the fossil bearing rocks. What did you scratch it with? Does it leave a streak and if so what color?

2:) On your way into the cache site, where you turned off the main road, you passed an old limestone quarry site. Limestone blocks are often mined for use in construction (the pyramids in Egypt are made from limestone blocks). Blocks were not mined from this quarry, but crushed limestone was collected. Looking at the size of these limestone chunks, what do you think this limestone would be used for?

Optional task:) Please post a photo of any fossils you found, with your log.



Additional Hints (No hints available.)