Red Stane is a prominent geological feature located on the northeastern coast of Shetland, an archipelago in Scotland. It is a cliff composed predominantly of red sandstone, hence the name. The cliff face stretches for approximately 200 meters, towering above the North Sea.
The formation of Red Stane dates back millions of years to the Devonian period, when sedimentary rocks were deposited in a shallow marine environment. Over time, the layers of sand and mud compacted and solidified, forming the distinctive red sandstone seen today.
The cliff exhibits striking geological characteristics, including horizontal bedding planes that are clearly visible. These bedding planes were formed when the sediment layers were deposited horizontally and subsequent tectonic forces caused them to tilt. The reddish hue of the sandstone is a result of iron oxide minerals present in the rock.
Red Stane is not only visually impressive but also provides a habitat for various bird species, including fulmars, kittiwakes, and puffins. The cliff face provides nesting sites and protection from predators. The surrounding area is also home to a diverse range of flora and fauna, making it a popular spot for nature enthusiasts and photographers.
Visitors can access Red Stane via a footpath that winds along the coastline, offering breathtaking views of the rugged cliffs and the crashing waves below. However, caution is advised as the cliffs can be unstable, and it is important to adhere to safety guidelines and stay away from the cliff edge.
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Images are sourced within 2km of 60.02768/-1.2334586 or Grid Reference HU4227. Thanks to Geograph Open Source API. All images are credited.
Red Stane is located at Grid Ref: HU4227 (Lat: 60.02768, Lng: -1.2334586)
Unitary Authority: Shetland Islands
Police Authority: Highlands and Islands
///reframe.endings.scrubber. Near Sandwick, Shetland Islands
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