Underground Waters Land Forms

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    Limestone Features

    Miss James

    Higher

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    Limestone

    Blue area

    arboniferous

    Limestone

    !or"shire

    #ales

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    Limestone consists mainly of calcium carbonate$ %here are

    several different types of limestone including hal", Jurassic

    and arboniferous$

    & %he arboniferous Limestone can be attac"ed by the'eathering process of carbonation$ %hin" aboutchemical 'eathering$ %his 'eathering contains a very

    distinctive type of landscape, 'ith both surface andunderground features$ %he most distinct landscape ofthis "ind is found in theYorkshire Dales$ Here thelimestone forms upland areas, capped by impermeableroc"s above, and separated by flat(floored and steep(sided glaciated valley)s called dales$ *laciers coveredthis area and as 'ell as sculpting the valley)s, alsoremoved loose roc" and soil to expose the limestone'hich 'as then more open to chemical 'eathering$

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    a+ - H.+ - +. / aH+.

    alcium carbonate - 2ater - arbondioxide / alcium bicarbonate

    3mpressive4

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    !or"shire #ales

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    Limestone& 5urface and rain 'ater do not flo' far on

    exposed limestone, but infiltrate rapidlyinto the roc" and soil$ 2here a 6oint or

    intersection of 6oints has been greatly

    'eathered or dissolved 'ater can passdo'n through the limestone

    arboniferous limestone is a sedimentary roc" formed in the !or"shire #alesaround 00 million years ago$ %hese roc"s 'ere laid do'n on the sea bed and

    made up of layers of ancient corals and s"eletons of sea creatures living in the

    shallo' seas at that time$

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    !or"shire

    #ales

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    Joints and Bedding 7lanes

    %his is hard grey roc", laid do'n in layers on

    the sea bed$ 3t occurs in massive bloc"s

    bordered by hori8ontal bedding planes

    and vertical joints$ %hese bedding planes

    and 6oints ma"e the roc" permeable i$e$

    'ater can pass through it$

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    lints and *ri"es

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    lints and *ri"es

    & %hese are flat areas of exposed limestone$

    5urface soil 'as probably removed by the

    glaciers$ arbonation 'eathering has

    enlarged 6oints to give 'ide gaps called

    grikes. %he stones left are called clints$

    5ome are 0$9m 'ide and .m deep$

    http:;;'''$bbc$co$u";scotland;education;int;geog;limestone;surface;their

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    5in";5'allo' holes

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    5'allo' holes

    & 3n the !or"shire #ales, streams flo' onimpermeable roc" on higher hillsides$2hen the streams reach the limestone,

    they usually only flo' for a short distancebefore disappearing underground at as'allo' hole sin" hole$ %hese developat the intersection of ma6or 6oints 'hichhave been 'idened by solution$ %his canbe seen at *aping *hyllin the !or"shire#ales$

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    *aping *hyll

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    +utcrops

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    5talagmites, stalactites = 7illars

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    5talagmites, stalactites = 7illars

    *round'ater may become saturated 'ith calcium

    bicarbonate in solution$ 2ater continually drips

    from cave ceilings$ 5ome 'ater evaporates to

    leave a thin film of calcium carbonate lime$+vertime a narro' stalactite may gro' do'n

    from the roof of the cave$ %he drip of 'ater then

    drops to the cave floor and evaporates from

    there 'hich ma"es a stalagmite$ 3f these 6oin apillar is formed$ 3n !or"shire caves stalactites

    gro' at around >$9mm per year$

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    *orges

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    arboniferous limestone areas often havenear vertical roc" cliffs along the sides of

    valley)s$ %hese cliffs are "no'n locally asscars$ %hey are susceptible to frostshattering physical 'eathering onexposed 6oints and may have screeat

    their base$ ?xtremely steep sided valley)sare called gorges$ @re formed by cavescollapsing$

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    aves

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    aves;*orges

    & #uring the melt'ater phase of the last ice

    age, underground streams eroded vast

    caverns as huge volumes of 'atertravelled through the limestone$

    5ometimes the roofs of these caverns can

    collapse exposing the Aunderground

    streamA in a very steep sided gorge$

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