Skip to content

Burney Creek Talus Slope EarthCache

This cache has been archived.

Geocaching HQ Admin: It has now been over 30 days since Geocaching HQ submitted the disabled log below and, unfortunately, the cache owner has not posted an Owner maintenance log and re-enabled this geocache. As a result, we are now archiving this cache page.

More information in the Help Center.

For locations where new EarthCaches may be permitted, please remember that any cache submission must meet all current EarthCache guidelines and expectations on the Geological Society of America web site and in the Help Center.

More
Hidden : 8/13/2009
Difficulty:
2 out of 5
Terrain:
2 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:

As Burney Falls eroded upstream, it left a relatively narrow steep canyon through layers of basalt. These steep canyon walls eroded off in large pieces and fell to the valley floor creating a geomorphologicaal feature called a talus slope.

The exposure of diatomite is along one of the trail in McArthur Burns Falls State Park. You can pay the entrance fee for close parking or find parking elsewhere and hike in. In either case, there is a short and easy walk along a forested lakeside trail.

Ancient Lake Britton formed about 1.8 million years ago close to the Plio- Pleistocene boundary. At that time lava flows from the Modoc Plateau blocked the Pit River. This natural dam flooded an area of forest much larger than the current Lake Britton, about 120 square miles. Once formed, the lake began filling with the remains of freshwater diatoms ( Ancestral Lake Britton Diatomite Deposits) and other lake deposits such as clay.

In the middle of the Pleistocene (about 20,000 to 30,000 years ago) the Hat Creek Lava Flow (originating from near the Splatter Cone Trail Visit the EarthCache) covered the lake deposits. As these basalt lava flows cooled, they contracted creating many fractures within the flow.

Recent erosion by Burney Creek over Burney Falls ( Visit EarthCache) eroded through the lava flow. Over time, the falls have moved upstream due to erosion at the bottom of the falls leaving a relatively steep narrow canyon. These steep canyon walls were composed of the fractured basalt.

Water filled these fractures and froze, expanding and pushing the crack wider. Eventually a piece of the lava flow was wedged off falling down onto an ever-growing pile of rocks at the bottom of the cliff called a talus slope

Talus slopes are important habitats for various rodents.

Logging requirements:
Send me a note with :

  1. The text "GC1X720 Burney Creek Talus Slope" on the first line
  2. The number of people in your group.
  3. How large are the pieces of basalt that compose the talus slope?
  4. Based on the sign near the coordinates, what does the presence of the talus slope provide evidence for?

This EarthCache conforms to the California State Park Geocaching Guidelines as of the hidden date.

The following sources were used to generate this cache:

  • Splatter Cone Self Guided Trail Guide, Lassen National Forest, Hat Creek Ranger District
  • Falls Trail Nature Saunter at McArthur-Burney Falls Memorial State Park, Video Transcript California State Parks, 2004

Find more Earthcaches

Additional Hints (No hints available.)