The Lithology Of Stonehenge
Weatherworn and overgrown by lichen, it is not possible at the present
day to see clearly the nature of the stones which go to make up
Stonehenge. For that reason only the barest outline of the monument as
it appears to the unknowing eye has been given, in order that the
original plan may be grasped thoroughly before entering into those
important issues which help to solve the enigma of its origin. Careful
investigatio
reveals the fact that the stones vary very much in
material, and that, further, just as the stones are placed in
systematic order, so, too, has the same care been exercised in the
selection of the material from which each circle or horseshoe has been
built. Moreover, just as the stones can be divided into groups of
uprights and imposts, or Trilithons, and simple uprights, so, too,
has it been found that while all the Trilithons are composed of a
local stone, known generally as Sarsen; all the simple uprights
are of foreign stone, sometimes classed together roughly as
Syenite. This latter term must be understood in a very comprehensive
sense since the simple uprights show considerable variation in
quality, but one and all are foreign to the county of Wiltshire;
whereas the larger Sarsen blocks are to be found in considerable
numbers scattered over the Wiltshire Downs. This difference in
material seems to present a considerable difficulty; and the question
naturally arises, How did the foreign stones come to Salisbury Plain?
This point will be considered later, as it is one involving other
matters, such as the ethnology of the builders and the probable region
from which they obtained these unusual materials. But the Sarsens
present no problem, and so may be considered first of all, for
familiar as they are their story is full of interest.