account, from Portland. Probably the confusion arose through the
original reporter using the term "the Island." Natives would know that
the definite article could only refer to their own locality! The stone
is an effect of denudation and is similar to other isolated sandstone
rocks scattered about the south of England, e.g., the "Toad" Rock at
Tunbridge Wells and "Great upon Little" near West Heathly in Sussex. A
short distance away is a smaller mass called the "Puckstone." The
derivation of the larger rock is probably Haligstane--Holy Stone. So
difficult is it to contemplate the ages through which gradual
weathering would bring these stones to their present shape that
scientists, as recently as the middle of the last century, were at
variance as to their natural or artificial origin.

A by-road, a little over five miles long, runs under the face of Nine
Barrows Down and Brenscombe Hill to Corfe. It is a picturesque route
and has some good views, but a much finer way, and but little longer,
is along the top of the Downs themselves culminating at Challow Hill
in a sudden sight of Corfe, backed by the imposing Knowle Hill. This
walk is even surpassed by that along the hills westwards from Corfe.
In this direction a similar by-road also runs under the long line of
the Purbeck Hills, here so called, but on the south side of the range
through Church Knowle which has an old cruciform church pulled about
by "restorers" as far back as the early eighteenth century and several
times since. The village is pleasant in itself and beautifully
situated. A short distance farther is an ancient manor house dating
from the fourteenth century. Its name--Barneston--is said to
perpetuate a Saxon landholder, Berne, so that the foundations of the
house are far older than this period. Over three miles from Corfe is
the small church hamlet of Steeple; here a road bears upward to the
right, and if the hill top has not been followed all the way from