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Devil's Punchbowl Earthcache EarthCache

Hidden : 3/18/2011
Difficulty:
1.5 out of 5
Terrain:
1.5 out of 5

Size: Size:   not chosen (not chosen)

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Geocache Description:

Across from Steamboat Rock State Park, along Washington State Highway 155, is a small inlet on Banks Lake known as the Devils Punch Bowl. This stretch of highway has a turnout with great views of Steamboat Rock and some other rocks that made us need to pull over. My Dad and I have gone on several outings to visit sites created by the Great Ice Age Floods. This site surprised us. Stop by and see what you think about this rock that stopped us in our tracks.

Much has been written about the Great Ice Age Floods. We have several books and DVD's that tell the history of what happened to this area thousands of years ago. One of our favorite DVD's is Ice Age 2: The Meltdown by Blue Sky Studios. Though not entirely historically accurate, it gives a great sense to the height of the glaciers and the force behind the water that is lacking in other DVD's. I feel it gives a great and different perspective to one of the many ice dam breaks that helped form this beautiful landscape. For a great in depth overview of the Great Ice Age Floods visit the Ice Age Floods Institute at: http://www.iafi.org/floods.html
Anyway, all the books and other materials say that you will find only one type of rock throughout the area uncovered by the forces of the water in the Grand Coulee. How did that basalt get here? During late Miocene and early Pliocene times, one of the largest basaltic lava floods ever to appear on the earths surface engulfed about 63,000 square miles of the Pacific Northwest. Over a period of perhaps 10 to 15 million years lava flow after lava flow poured out, eventually accumulating to a thickness of more than 6,000 feet. As the molten rock came to the surface, the earths crust gradually sank into the space left by the rising lava. The subsidence of the crust produced a large, slightly depressed lava plain now known as the Columbia Basin (Plateau). The ancient Columbia River was forced into its present course by the northwesterly advancing lava. The lava, as it flowed over the area, first filled the stream valleys, forming dams that in turn caused impoundments or lakes. In these ancient lake beds are found fossil leaf impressions, petrified wood, fossil insects, and bones of vertebrate animals. With the end of the outpouring of lava, tremendous forces deep within the earth began to warp the plateau in several places. A general uplift of the mountainous region in the north caused the entire plateau to tilt slightly to the south. This tilting and associated stairstep rock folds, called monoclines, in the vicinity of Coulee City and Soap Lake, played an important role in the formation of the Grand Coulee.
More than likely, if you find yourself at this site, you're probably aware of the forces behind what shaped this gorge during the Great Ice Age Floods. If you are driving down from the north, you may have noticed some of this type of rock in some of the highway cutouts along the way from the Grand Coulee Dam in Electric City. If you are driving up from the south, up to now all the rock that you've seen has been the same, the reddish brown basalt lava that cooled into the columns that line the Grand Coulee. At this site there is a new type of rock here. The bedrock that the lava flows were laid upon. From the pull out you can see across the highway at an outcropping of this new type of rock. You do not need to cross the highway to examine this rock, because they blasted this rock to make room for the highway, and large chunks line the pull out. If you choose to cross the highway be mindful of traffic, which could be heavy depending on the season. If the visitor center at the Grand Coulee Dam is open, they have a great display about the rocks found in this area. I hope you enjoy this site.

To get credit for this Earthcache send an email to the owner with the answers to the following:
1. How is this rock different from the basalt rock that forms the coulee? Color, texture, etc.
2. Do you know what type of rock this is? What's it called.
3. How did it get here. Is it part of the bedrock, or could it have been rafted here in the floods?
4. What is the title on the sign that is in the pull out.
You can post a picture as long as it doesn't show the answers,and please do not put your answers in your log or it will be deleted.

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