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Geology and
Wildlife
The geological history of the geo-cultural region
in which the nominated Site is located begins nearly 400 million
years ago (Ma). Sand and mud settled on the floor of a
Devonian
sea, and molten rock formed submarine lavas and intrusions within
the sediments. Around 320 Ma, during
Carboniferous times,
continents collided and caused a major earth-movement. This
subjected the earlier rock formations to folding, faulting and
cleavage on a general axis with an east-north-east to
west-southwest trend. It is this alignment that accounts both for
the orientation of the granite emplacement and the main tin and
copper lodes. Mudstones became slates, which together with
subordinate bands of sandstones have long been known collectively
by the Cornish term ‘killas’.
Between 300-270 Ma, during the late Carboniferous
and
Permian periods, continental collision generated considerable
heat and pressure which melted the crust to form granite, a coarse
crystalline igneous rock formed deep in the earth. Separate
granite masses intruded into the rocks above them between 290-270
Ma. They merged to form an elongate body of granite, known to
geologists as a batholith. The intense heat also caused water to
circulate within the granite, producing the main tin, copper and
tungsten mineralisation around 270 Ma.
Around 250 Ma, during the late Permian, a mountain
chain was created during a period of considerable uplift. The
rocks which once covered the granite were then gradually removed
by deep weathering and erosion, exposing the tops of the granite
domes. Around 236 Ma, during the
Triassic, the cross-course
lead-silver-zinc mineralisation formed in a north-south structural
orientation. This alignment, perpendicular to the main tin and
copper mineralisation, was due to changes in geological stress
regimes.
Within the past 4 million years, marine erosion
created a relatively flat surface (the 130-metre planation
surface), as well as wave-cut platforms and raised beaches. It is
likely that tin placer deposits were formed within the same
period, and went on being formed until relatively recent times.
The sea level fell during the Ice Ages of the past 1 million
years, (ending around 10,000 years ago) and rose in recent times
by about 15 metres. River valleys (known as ‘rias’) were cut and
subsequently flooded by these events, including the River Tamar
and the Fal estuary.

Mining and the
Natural Environment
Mining and the natural environment have always been
inextricably linked. Geological and geomorphological processes
which took many millions of years to develop determined the
resources available for mining and the sites where they awaited
discovery and exploitation. Long ago, miners learnt the tell-tale
signs of mineralisation - the characteristic greens of secondary
copper minerals, the reds of iron-bearing rocks, the hard
resistant whiteness of quartz stringers and reefs, the local
softening and erosion of other altered rocks that signalled the
presence of valuable ores. Elsewhere they began to realise that
common plants were stunted or absent where such minerals occurred,
or that some species - indicator plants - alone thrived where
certain minerals lay not far beneath the surface. They dowsed,
tasted the water, learned the smells of pyrite and mundic -
developed a sense of geology that was instinctual long before it
was written down or scientifically analysed - picking up subtle
hints from their natural environment - clues that unerringly
guided them to what it was they sought.
In turn, their activities changed the environment. Rocks whose
weathering products were far more acidic or toxic to plant life
than those experienced in the landscape - softened and tamed by
long exposure to wind, water and bacteria - were brought from deep
beneath the earth in vast quantities, broken into fragments,
crushed to fine sands, burnt so that they turned to toxic gases,
discarded as waste and spread across its surface or spilled into
its watercourses. Across its landscape, environments were created
which had not existed in Cornwall or West Devon for tens of
millions of years. The few plants which could live there are very
specialised - pioneer species which can gain a tenuous foothold in
such dangerous habitats and after many decades create the
conditions where other, less tolerant species could, perhaps,
build on the shallow, poor soils they had painstakingly created. A
slight change in their habitat - the disturbance of the surface of
a waste dump, the spreading of a mere inch of nutrient-rich
topsoil, the removal of a mineral-rich input to a stream - can
undo the work of centuries and destroy such habitats for ever.
These are special places - rare not only in Cornwall, but
worldwide. Some are so free-draining that they resemble miniature
deserts, others are so utterly saturated with acidic water that
only the most primitive species can survive, many are rich in
freely-available toxic minerals whose closest comparisons are lava
flows. The plants and animals that survive - and in many cases
thrive here - are often unusual and find these conditions nowhere
else in a landscape which agriculture has slowly modified over
thousands of years - these are wild, primitive and important
places in our landscape - but also vulnerable places - for their
inhabitants are often small and undramatic, their value often
unrecognised until they have gone. These are the homes of rare
mosses and lichens, of stunted variants of common plants, of bare
sands and clays, exposed rocks and the insects, beetles and other
animals which are found here and which can survive nowhere else.
Many generations of such plants and animals must have lived out
their lives in islanded areas like these, utterly isolated from
contact with other such colonies, that subtle changes brought
about through specialisation and inbreeding may have occurred.
Other species rely on chains of sites like these, spread
throughout the landscape, moving from one oasis to another in what
is to them a sterile and inhospitable desert of farmland and
townscape. Remove enough of these sites, and they are trapped.
The contents of the spoil heaps, hacked as they have been from
deep below the ground, are also extremely important resources for
the geologist and mineralogist. These are types of rocks and
minerals which simply do not occur at the surface, where millions
of years of exposure to air and water chemistry, coupled with the
effects of some of the smallest, yet most abundant life forms on
the planet have changed them into the stable, familiar materials
which make up most of our environment. They provide rare and
valuable glimpses into the formation of our planet and the way it
has developed. Seventy one globally-rare species of minerals were
recorded in Cornwall up until 1992 from such sources - twelve had
never been recorded anywhere in the world before that date, and it
is certain that many more await discovery. The words
"waste" and "spoil" are often so wrongly
applied to such sites - these are treasure houses which may prove
to be as important for the knowledge of the natural world which
they provide us as the copper and tin from which they were once
separated and discarded.
For further information, try the following sites:
Cornwall Wildlife Trust,
English Nature,
Devon Wildlife Trust,
Cornwall RIGS Group,
The Russell Society,
Camborne School of Mines
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