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A plan of the Y and Z Hole circuits at Stonehenge in relation to the central stone structure. The Y and Z Holes are two rings of concentric (though irregular) circuits of 30 and 29 near-identical pits cut around the outside of the Sarsen Circle at Stonehenge. The current view is that both circuits are contemporary.
The Station Stones are elements of the prehistoric monument of Stonehenge. Originally there were four stones, resembling the four corners of a rectangle that straddles the inner sarsen circle, set just inside Stonehenge's surrounding bank. Two stood on earth mounds at opposing corners, one corner broadly in the north of the site and one in the ...
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The word henge is a backformation from Stonehenge, the famous monument in Wiltshire. [5] Stonehenge is not a true henge, as its ditch runs outside its bank, although there is a small extant external bank as well. The term was first coined in 1932 by Thomas Kendrick, who later became the Keeper of British Antiquities at the British Museum.
Banks at the terminal ends enclose the cursus. Over fifty have been identified via aerial photography while many others have doubtless been obliterated by farming and other activities. [4] The Stonehenge Cursus is a notable example within sight of the more famous Stonehenge stone circle.
This is the first evidence for any unambiguous alignment at Stonehenge (the solstice axis). The analysis of the spacing between the Q and R array, and that of the modified (inset) portal group (Fig.3) imply a shift from an angular splay of 9 degrees (i.e. 40 settings) to 12 degrees, the same as that of the later 30 Sarsen Circle.
Many interpretations prefer an astronomical explanation for the purpose of the holes although this is by no means proved. It was formerly thought that when the Aubrey holes were first dug, the only standing feature at Stonehenge was the Heelstone, which marked the point of the midsummer sunrise, viewed from the centre of the henge.
Different structures are referred to as banks in different fields of geography. In limnology (the study of inland waters), a stream bank or river bank is the terrain alongside the bed of a river, creek, or stream. [1] The bank consists of the sides of the channel, between which the flow is confined. [1]