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The riddle of the stones EarthCache

This cache has been locked, but it is available for viewing.
Hidden : 1/1/2010
Difficulty:
1.5 out of 5
Terrain:
2 out of 5

Size: Size:   not chosen (not chosen)

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Geocache Description:




Stonehenge is a prehistoric monument located in the English county of Wiltshire, about 2 miles west of Amesbury and 8 miles north of Salisbury. One of the most famous sites in the world, Stonehenge is composed of earthworks surrounding a circular setting of large standing stones. It is at the centre of the most dense complex of Neolithic and Bronze Age monuments in England, including several hundred burial mounds.

Stonehenge has long been regarded as a mystery in early human culture and technology. Although the monument has been studied extensively by archaeologists, many questions still remain on who built Stonehenge and for what reason. Geologists have concluded that the rocks at Stonehenge did not come from the local area, adding questions about how the rocks were transported to their current location in the Salisbury Plain so that the monument could be built.
Salisbury Plain itself is underlain with a soft chalk formation that was deposited during the Cretaceous period. The stones that make up the monument are of two rock types: sedimentary and igneous. The sedimentary rock is called sarsen sandstone. This sandstone was deposited over much of southern England at the beginning of the Tertiary period about 60 million years ago. These are the larger stones that make up the outer circle of the monument and rock beams across the top of the standing stones. This sandstone is not native to Salisbury Plain and petrological analysis has suggested its source as being an outcrop located at Marlborough Downs 30 kilometres away.
The smaller stones located within the monument are an igneous rock called bluestone. This rock is also not native to Salisbury Plain and must have been transported. The chemical composition of the bluestone - named so because they have a blue-grey colour when wet - suggests a combination of intrusive and extrusive rock formations that make up this stone. The intrusive rock is gabbro, which is the same composition as its extrusive counterpart, basalt lava rock. The rock is also rhyolite and other types of pyroclastic rock. The bluestones are arranged in a circle inside the larger sarsen circle. Geologists have used geochmical analysis to match the bluestones to an outcrop located more than 200 km away at Preseli Hills in western Wales.
These bluestones hold another clue - although geologists have confirmed that they did not form in or near the Salisbury Plain, archaeologists have come across fragments of bluestones in the Salisbury Plain that were in place long before Stonehenge was built. This evidence supports the theory that the blue stones were not transported to the Salisbury Plains by humans, but must have been transported by some other force.



There are two theories that can explain how these sedimentary and igenious rocks came to be at Salisbury Plain. One theory, favoured by archaeologists, is that the stones were transported there by the monument's makers. However, this theory does not explain how the bluestones came to Salisbury Plain since it has been established that they were brought there before any development of the monument started. The second theory is that glaciers transported the stones to Salisbury Plain.
In 1971, a geologist published an article in Nature suggesting that the bluestones are actually glacial deposits  - boulders that get transported by glacial movement. Moreover, subsequent geochemical studies have established that the bluestones did not just come from one quarry, but multiple quarries throughout Preselli Hills, some as much as 13 kilometers apart.Geologists conclude that these bluestones must have already been conveniently close to the monument's site, transported there by glaciers.

To claim this earthcache I need you to email me through my profile the answers to these questions - 

1. identify the geologist who wrote the 1971 article, and the particular name of the deposits.

2. Estimate the weight of the visible portion of the closest stone to the co-ordinates, assuming sarcen stone weighs "154 lbs per cubic foot". Stones of Stonehenge By E. Herbert Stone

3. Walk north east along The Avenue away from the co-ordinates, and email me the co-ordinates you are at when the stones are no longer visible to you.

Although Stonehenge is in the stewardship of English Heritage, there is no need to enter the fenced compound (and pay the entrance fee) to complete this earthcache. Cache location has been approved by representatives of Wiltshire County Council.



I WILL be checking answers. If you don't want to take the effort to do the cache, or don't have the time because you're on a coach trip - don't expect to be given a smiley just for sending some Googled, but incorrect, answers. And don't complain if your logs are deleted and the reasons given on this page!
And if English isn't your first language, please note that The Avenue is not the road....

Additional Hints (No hints available.)