
Saturday, 17 March 2018
Ebenezer Place, Wick

Thursday, 15 March 2018
Clouds Hill, Dorset
Lawrence first rented Clouds Hill in 1923 and bought it in 1925, although he did not live there full-time until shortly before his death in 1935.
He died in a motorcycle accident near Bovington Camp when he swerved to avoid two boys on bicycles and was thrown off. The cottage at Clouds Hill is now preserved exactly as Lawrence left it, even down to the absence of electric light.
Chislehurst Caves, Kent
The caves at Chislehurst (Kent, England) are not as well-known as those at Cheddar in Somerset, but they are certainly worth a visit. They are within Greater London and therefore offer an alternative to the usual “sights” that tourists normally flock to see.
The caves are man-made, having been created
as mines for chalk and flint in the Middle Ages. They were last used
commercially in the 1830s but saw service as weapons stores during World War
One and air-raid shelters in World War Two.
The complex of tunnels extends for more than 20 miles under the North Downs, but today’s visitors are limited to what they are shown during a 50-minute tour by experienced and knowledgeable guides, armed with oil lamps.
The features to be seen include wall carvings and the Cave Church that was established for Londoners who sheltered here during air raids.
The caves are privately owned, but the charge for admission is reasonable.
Burns' Cottage, Alloway, Ayrshire
He was born on 25th January 1759 in a modest three-room thatched cottage in Alloway, Ayrshire. His father, a gardener, had built it himself two years previously. However, Robert was the first of seven children and as the family grew the cottage clearly became impractical as a family home. They therefore moved away when Robert was only seven years old.
The cottage was owned by many other people throughout the years, and was at one time a village pub. However, the association with Robert Burns became known as his fame spread and visitors from far and wide came to see the place where Scotland’s National poet had started his life.
Robert Burns was only 37 years old when he died in on 21st July 1796. On the fifth anniversary of his death a group of friends met at the cottage to celebrate his life by holding a supper in his honour. The tradition of an annual “Burns Supper” has been maintained ever since, although the date has been moved to that of the poet’s birth, namely 25th January. Burns Suppers are held throughout Scotland and in many other parts of the world.
The cottage has been fully restored and is now the centerpiece of the Robert Burns Birthplace Museum and the Burns National Heritage Park, under the overall management of the National Trust for Scotland. The presentation of the cottage’s interior was been done as authentically as possible, so that the visitor can see where young Robert Burns would have ate, slept, and had his first lessons in reading and writing from his father.
Visitors will be able to appreciate the humble background from which he came, as well enjoying some of his poems displayed on the walls and presented in audio form.
As well as the cottage, visitors can immerse themselves in “Burnsiana” by following the path to the main Museum, walking across the Brig o’Doon and visiting ruined Auld Kirk, both of which feature in his poem Tam O’Shanter.
© John Welford
Bedruthan Steps, Cornwall
Batholiths: volcanoes that never were
A batholith is a massive upwelling of molten magma that has risen from deep in the Earth’s crust and cooled very slowly before it could reach the surface.
Batholiths are associated with mountain building and are often found within mountain chains. They can be very large, such as the one beneath the Andes of Peru that covers an area covering 1600 by 190 kilometres. After a batholith has cooled and solidified, the overburden of pre-existing rock may be eroded to revel the batholith which often takes the form of a granite dome – this is the origin of outcrops in Cornwall that now form Dartmoor, Bodmin Moor and the Land’s End peninsula.
The magma may not always form a solid mass as it rises. Magma can intrude into faults and weaknesses in the overburden and create sills and dykes (horizontal and vertical intrusions respectively) or subsidiary masses called laccoliths.
Other coarse-grained igneous rocks that originate in batholiths, besides granite, include gabbro and syenite. It is still possible for heat to rise through a batholith millions of years after it has solidified, and some of this can be the result of radioactive decay. If this heat becomes trapped it could be a potential source of energy if it can be accessed.
(The photo is of Hay Tor on Dartmoor)
Monday, 4 December 2017
Must-see items at London's British Museum
The sculptures are housed in the Duveen Gallery (Room 18), which is on the extreme “left” of the building from the main entrance. The visitor with little time will therefore have to avoid the temptation to look at all the other treasures he or she will pass on the way!





