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GeoMuzzy-Adequately Stunning Fountain Of The Pines EarthCache

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GeoMuzzy: goodbye

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Hidden : 3/20/2024
Difficulty:
1.5 out of 5
Terrain:
2.5 out of 5

Size: Size:   other (other)

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Geocache Description:


To log this cache please message me the answer to these 3 questions:

1. How did the overlook get its fountain shape?

2. The sandstone of the overlook is red because______________ is present in the rock

3. Using what you discover at the overlook and what you see in the description, give me in depth detail about one example of orogeny you see at the site and use your knowledge and the description to give me your best guess about why or how your chosen element of the overlook formed.

 

 

Lost Gulch Overlook on Flagstaff Road in Colorado offers a unique opportunity to explore the geology of this fascinating area. Situated atop a rocky outcrop overlooking Boulder and the surrounding Rocky Mountains, this overlook provides a stunning vista of the landscape below. The geological formations visible from this vantage point offer insights into the complex geological history of this region.

One of the most striking features of Lost Gulch Overlook is the prominent presence of the Fountain Formation, a distinctive red sandstone rock formation that is prevalent throughout the area. This formation dates back to the Pennsylvanian period, approximately 300 million years ago, when the region was covered by shallow seas and dunes. The red color of the sandstone is due to the presence of iron oxide, which gives the rock its characteristic hue.

In addition to the Fountain Formation, visitors to Lost Gulch Overlook can also observe the Dakota Formation, a layer of sandstone and shale that is younger than the Fountain Formation. The Dakota Formation was deposited during the Cretaceous period, approximately 100 million years ago, when the region was a coastal plain. Fossilized marine creatures such as ammonites and mosasaurs have been found in this formation, providing evidence of the ancient seas that once covered this area.

The geology of Lost Gulch Overlook also includes evidence of the tectonic forces that have shaped the Rocky Mountains over millions of years. The uplift of the mountains began around 70 million years ago during the Laramide orogeny, a period of tectonic activity that created the modern landscape of the region. The exposed rock layers at the overlook bear witness to the immense forces that have uplifted and deformed the earth's crust, creating the dramatic peaks and valleys that characterize the Rocky Mountains.

The geological features of Lost Gulch Overlook are not only visually stunning but also provide valuable insights into the dynamic processes that have shaped this region over millions of years. By studying the rock formations, fossils, and structures visible from this vantage point, geologists can unlock the secrets of the earth's ancient past and better understand the forces that continue to shape our planet today. Whether you are a geology enthusiast or simply a nature lover, a visit to Lost Gulch Overlook is sure to inspire awe and appreciation for the natural beauty and geological wonders of Colorado.

 

1. Orogeny: is the process of mountain building through the upward and outward movement of the Earth's crust due to tectonic forces, typically involving the folding and faulting of rock layers.

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