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Donnelly Dome EarthCache

This cache has been locked, but it is available for viewing.
Difficulty:
1.5 out of 5
Terrain:
4 out of 5

Size: Size:   not chosen (not chosen)

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Geocache Description:

Donnelly Dome, a popular hiking spot near Delta Junction. Donnelly Dome is refered to as a Fleiberg. A Fleiberg is a mountain that has been over ridden by ice.



Standing alone in the Delta River Valley 18 miles south of Delta Junction, Donnelly Dome always sparks a few questions by those who drive past. People have been heard to muse over whether the Dome is a lonely volcano.

Donnelly Dome is a bit odd. In fact, it shouldn't even be here. It is out of place.Thousands of years ago, A glacier went down the (Delta River) valley. The glacier should have sheared Donnelly Dome off, but it didn't.

There's a word for bumps like Donnelly Dome. Donnelly Dome is a fleigberg.


A fleigberg is a mountain that has been overridden by ice. There is evidence on the top of the dome that glaciers touched it, even if they didn't shave it from the valley floor. Buick-sized "erratics," rocks that came from somewhere else, sit on top of the dome. The erractics were conveyor-belted out on the ice and dropped on top of Donnelly Dome.

How did the dome resist being scraped from the earth while those around it crumbled under the force of an Alaska Range glacier that covered the area 70,000 to 100,000 years ago? Donnelly Dome may have had the luck to squeeze between two separate tongues of the glacier. And there was another glaciation that just missed it. In the Donnelly Glaciation, from 30,000 to 10,000 years ago, glaciers reached just the base of the dome and did not cover it.

Once overlain by glaciers, the geology around Donnelly Dome is marked by glacial moraines as well as alluvial deposits from the Delta and Tanana Rivers. Numerous mineral deposits are found in the vicinity of Delta Junction ranging from gold to molybdenum to coal. Donnelly Dome was formed as a glacier coming from the Alaska Range split in two, carving away sides of a former mountain.

The trail head and parking for Donnelly Dome trail is at N63 46.428 W145 45.723.

To get credit for this EC, post a photo of you with GPS and Donnelly Dome in the back ground, or if you are up to the challenge hike to the top of the dome and take your picture up there. The picture can be from the trail head or on top of Donnelly Dome. Please answer the following questions.

1. What is the elevation at trail head?

2. What type of stone are most of the Erratics laying around Donnelly Dome?

3. How many years ago was the Donnelly Glaciation period?

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Do not log this EC unless you have answered the questions and have a picture ready to post! Logs with no photo of the actual cacher (human face included) logging the find or failure to answer questions or negative comments will result in a log deletion without notice. Exceptions will be considered if you contact me first (I realize sometimes we forget our cameras or the batteries die). You must post a photo at the time of logging your find. If your picture is not ready then wait until you have a photo.

Sources of information for the EarthCache The information for this EarthCache from the Alaska Geological Survey and the University of Kentucky Geology Department. I am by no means a geologist.. I use books, internet, and ask questions about geology just like 99.9 percent of the geocachers who create these great Earth Caches. I enjoy Earth Caches and want people to get out and see what I see every time I go and explore this great place we live in.

Additional Hints (No hints available.)