CROSS CURRICULAR STUDIES - THREE |
The nature of the different stone
used by Andy Goldsworthy and the wallers in constructing his cones
and folds can lead to an understanding of the GEOGRAPHY and GEOLOGY
of Cumbria and link to studies in SCIENCE.
'The Lake District ... contains
a surprising number of different rock types and
corresponding styles of walling. Starting with the oldest formations,
the Skiddaw Slates of the northern peaks, one finds walls of dark
or occasionally greenish fissile slates and flags ... Between
Keswick and Ambleside, in a broad zone which includes the most
rugged part of the district, the Borrowdale Volcanics form a varied
group of erosion-resistant massive lavas and tuffs. The granite
and granophytes of Ennerdale and Eskdale produce walls of similar
type but a warm mottled pink. The volcanic walls are generally
similar in design to those of slate but are generally coarser
and more massive ...
The southern part of the Lake
District is made up of Silurian slates, which include shales and
flags as well as true slates. These resemble the Skiddaw slates
... which produce slabs for walling. Where the Coniston and Brathay
flags occur at the boundary of the Silurian slates and Borrowdale
volcanics, roughly quarried slates are sometimes used upright
to make stone fences. Many examples can be found around Coniston,
Hawkshead and Ambleside.
Around the edges of the Cumbrian dome other newer rocks occur
which connect Lake District walls with those of the Pennines and
the Carlisle area. Carboniferous limestone around Furness, in
the area south of Kendal and elsewhere is used to build silvery-grey
walls, quite similar to those farther east in Yorkshire. New Red
Sandstones occur on the coast around St. Bees and in the tongue
of the Eden Valley, where the walls are rusty red and often of
shaped and wellbedded blocks, while between here and the
limestone area is a narrow belt of Coal Measure gritstone walls.'
(5)
Dry stone walls, sheepfolds, limestone
kilns and field barns are also habitats for a wide range of flora
and fauna and present the possibility of studying many species
of flowers, grasses, mosses, lichens, animals, birds and insects
as part of the SCIENCE curriculum. (6)
The Sheepfolds project can give
rise to work in MATHEMATICS, looking at pattern and tessellation
in wall building. The shape, area, dimensions and proportions
of the folds were often based on careful calculations.
'To minimise snow deposit within
the stell, the height of a circumference wall in relation to diameter
is crucial: thus for stells up to 15 yards [about 15 metres] in
diameter this height should be 6 feet [about 2 metres]. Most stells
were 8 to 15 yards [approx. 8 to 15 metres] in diameter, depending
on the size of their heft'. (7)
(A stell is a sheepfold that provides
shelter for sheep and a heft is the area of fell land grazed by
a particular flock of sheep.)
Andy Goldsworthy's cones too are
built to careful measurements, where the size of the base, the
maximum width and the final height are in ratio 3: 5: 7. He has
found that these proportions form the strongest structure to allow
the weight of the stone to curve out and then in. The cones completed
at Raisbeck, Outhgill, Brough and Bolton are approximately 2 metres
high, have about 25 courses and, altogether, contain 3-4 tons
of stone in each cone.
Each time Andy Goldsworthy builds
a fold, Dick Capel, the Sheepfolds Commissions Manager, has an
interesting mathematical problem in calculating the amount of
stone required to build a fold. If it is approximately two metres
high and three metres in diameter he must calculate the circumference
to find how many tons will be needed. Approximately one ton of
stone is used per metre of wall.