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Honister Slate mine is at the top of the Honister Pass in Borrowdale in the Lake District. You can watch slate being riven (or split) using processes that have changed little over the past 300 years.
Fully guided tours into the mine are available several times a day, detailing the history and spectacular features of the mine. The tour shows the current workings of the mine, and how a mixture of modern and traditional methods, is still extracting the slate which was formed some 400 million years before Tyrannosaurus Rex strode the land. Honister slate is a distinctive green slate, though Lakeland slate comes in a variety of shades and colours. It is a strong and durable material, excellant for roofs , and also for floors and walls. Slate was being exported through Piel Harbour in 1688, long before the opening of the Furness Railway in 1846. It was taken by packhorse over the western edge of Great Gable and Wasdale, for loading onto boats at Ravenglass. In the late 17th Century, it was used by Sir Christopher Wren at the Royal Hospital, Chelsea, and at Kensington Palace. Slate is a fine-grained, clayey metamorphic rock that cleaves, or splits, readily into thin slabs having great tensile strength and durability; some other rocks that occur in thin beds are improperly called slate because they can be used for roofing and similar purposes. True slates do not, as a rule, split along the bedding plane but along planes of cleavage, which may intersect the bedding plane at high angles. Slate was formed under low-grade metamorphic conditions—i.e., under relatively low temperature and pressure. The original material was a fine clay, sometimes with sand or volcanic dust, usually in the form of a sedimentary rock (e.g., a mudstone or shale). The parent rock may be only partially altered so that some of the original mineralogy and sedimentary bedding are preserved; the bedding of the sediment as originally laid down may be indicated by alternating bands, sometimes seen on the cleavage faces. Cleavage is a super-induced structure, the result of pressure acting on the rock at some time when it was deeply buried beneath the Earth’s surface. On this account, slates occur chiefly among older rocks, although some occur in regions in which comparatively recent rocks have been folded and compressed as a result of mountain-building movements. The direction of cleavage depends upon the direction of the stresses applied during metamorphism.Slates may be black, blue, purple, red, green, or gray. Dark slates usually owe their colour to carbonaceous material or to finely divided iron sulfide. Reddish and purple varieties owe their colour to the presence of hematite (iron oxide). . The principal minerals in slate are mica (in small, irregular scales), chlorite (in flakes), and quartz (in lens-shaped grains). Slates are split from quarried blocks about 7.5 cm (3 inches) thick. A chisel, placed in position against the edge of the block, is lightly tapped with a mallet; a crack appears in the direction of cleavage, and slight leverage with the chisel serves to split the block into two pieces with smooth and even surfaces. This is repeated until the original block is converted into 16 or 18 pieces, which are afterward trimmed to size either by hand or by means of machine-driven rotating knives. Slate is sometimes marketed as dimension slate and crushed slate (granules and flour). Dimension slate is used mainly for electrical panels, laboratory tabletops, roofing and flooring, and blackboards. Crushed slate is used on composition roofing, in aggregates, and as a filler. Principal production in the United States is from Pennsylvania and Vermont; northern Wales provides most of the slate used in the British Isles. The co-ordinates take you to the entrance of the slate mine. To log the cache, upload a photo of you or your GPS with the slate entrance sign to the right as you enter and answer the following questions 1) What gives Honister slate its green colour. 2) What is the slate used for. Thanks must also go to Grufftymilo who helped us to get the Earth Cache up and running
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Coordinates are in the WGS84 datum