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Painted Bluffs Earthcache EarthCache

This cache has been locked, but it is available for viewing.
Hidden : 1/13/2011
Difficulty:
3 out of 5
Terrain:
4.5 out of 5

Size: Size:   other (other)

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Geocache Description:

Painted Bluffs Provincial Park was established in 1996. It is a 100 hectare area on the north shore of Kamloops Lake, 34km west of Kamloops.


Painted Bluffs is not easy to access. By land, the Sabiston Creek Road travels off the Trans Canada Highway and winds through the hills. One junction leads down to Copper Creek and from there it is still an over-hill trek east to the lakeshore area below the cliffs. By water, boats can launch from Cooney Bay near Kamloops, from Tobiano, or from Savona. Small boats are cautioned to travel only in good weather since Kamloops Lake is a large lake subject to windy conditions. But, the effort is worth it. Painted Bluffs has an unearthly feel to it.



Very little geological information is available on this area. What we do know is that the bluffs have distinctive multi-colored rocks and soils on an intrusion of batholithic rocks.
  • A batholith is a large zone of molten rock under the surface of the earth that cools over time.
  • An intrusion is an arm of the batholith that has risen to the surface and cooled, forming minerals in the process.
  • Batholithic intrusions often stand out (are discordant) from the local geology.
The bluffs have been eroded into distinctively-shaped barren ridges and gullies, all leading down to a fluvial fan.
  • Fluvial fans are formed by the movement of water bringing materials down stream.
  • Alluvial fans are formed when a stream course suddently widens and flattens. Materials are deposited in a fan shape.
The hillsides surrounding are covered in big sagebrush and bluebunch wheatgrass. California bighorn sheep frequent the ridges. The colors off the bluffs are intriguing. Deposits of mercury, copper, and cinnabar have altered the hues of these materials.
  • Mercury was raised to the surface through the intrusions and cooled in cinnabar formations. Most mercury deposits around the world are found in cinnabar.
  • Cinnabar (mercuric sulphide) is the common ore of mercury.
  • Cinnabar is usually brick red to crimson in color. It is an ingredient used in red pigments.
  • Copper is an ore common to the area (ie Copper Creek).
  • Copper compounds are often found as salts of copper, and impart a green or blue color.


To log this earthcache,you must visit the site. Be sure to take photos, but while you are on site, you will be looking at the materials, colors, and shapes. Collect your data as notes,observations, coordinates, or photos. E-mail the owner your hypotheses for the following questions:
  • Where is the fluvial fan in this park?
  • Pick one of the bluffs. Mark a waypoint (take coodinates). Describe the feature and comment on the color and the probable source of the pigment.
  • Inspect the materials in the bluffs. Describe the size and composition of the materials.


You will want to bring your camera here. This is a special site, one well-worth your efforts. Artists are encouraged to bring their sketchbooks or painting easels.



Additional Hints (No hints available.)