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Firepit and Spendlove Knolls EarthCache

Hidden : 11/2/2006
Difficulty:
1 out of 5
Terrain:
1.5 out of 5

Size: Size:   not chosen (not chosen)

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Geocache Description:

These two cinder cones are can be seen from Kolob Road. There is ample parking on the side of the road. I did not see any trail leading to the peak of the cones.

The coordinates take you to a turnout along Kolob Road. To the north is Firepit Knoll and to the southwest is Spendlove Knoll. These are two cinder cones that are approximately 200,000 years old. These cinder cones are thought to be the source of the Grapevine Wash basalt flow.

Kolob Road to the south is built on this flow. Cinder cones often are formed near the end of an eruption. Any cones that are created early in the eruption are likely to be destroyed by a later episode in the eruption.

Cinder cones are formed from cooled chunks of lava ejected from a single central vent. Gas-filled lava is blown into the air where it breaks apart into small fragments and quickly cools creating cinders. These cinders are typically air filled and relatively light for rocks of their size. The cinders usually build up around the central vent to create a circular or oval cone with a crater at the summit.
Image Source: http://pubs.usgs.gov/gip/volc/types.html

Basalt is one of the four major categories of volcanic rocks. It has the least amount of silica of the four types of volcanic rocks. (Silica is a common compound found in the earth’s crust). Basalt also tends to be the hottest and most fluid of the volcanic rocks. See http://volcanoes.usgs.gov/Products/Pglossary/VolRocks.html for a further description and graphics regarding types of volcanic rocks.

Logging requirements:
Send me a note with :

  1. The text "GCZ5Z6 Firepit and Spendlove Knolls" on the first line
  2. The number of people in your group.
  3. Comparing the current shape of the two cinder cones to the idealized diagram presented in the discussion.
  4. Account for the similarities and differences. .
  5. Optional: Please post a picture of yourself or another member of your party with one of the 'knolls' in the background.

The above information was compiled from the following sources:

  • Hamilton, Wayne L. 1987, Geological Map of Zion National Park, Utah Miek, Robert F., et. al.,
  • Geology of Zion National Park, Utah in Geology of Utah’s Parks and Monuments, 2003 Utah Geological Association Publication 28 (second edition) D.A. Sprinkel, T.C. Chidsey, Jr. and P.B. Anderson, editors
  • USGS, Principal Types of Volcanoes, http://pubs.usgs.gov/gip/volc/types.html
  • USGS, Types of Igneous Rocks, Volcano Hazards Program – Reducing volcanic risk, http://volcanoes.usgs.gov/Products/Pglossary/VolRocks.html

Placement approved by the
Zion National Park


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