LIMESTONE / GRANITE LANDSCAPES

Come here because of the Education Guardian Best of the Web article from 13th December 2005 ? Welcome - why not explore THE SITE more....


In the 'AS' exam, a requirement is to know an example of either LIMESTONE or GRANITE landscape. This page will help you learn more about these distinctive landscapes.


Suggested areas:

LIMESTONE: Yorkshire Dales - classic Malham round, Burren in Republic of Ireland, White Peak area of Peak District - we now have some great MEMORY MAP software to help us teach this area and go through the physical features. The LIMESTONE section of this website has a range of other links. We also use an excellent PHOTO JAM created by V. Vannet - a search on FLICKR or similar photo-sharing sites would provide plenty of suitable fodder.

A dry valley in the White Peak. Picture taken by Mister P. Notice classic valley shape, but absence of stream (that's a dry stone wall running down the middle) 

GRANITE: Dartmoor (some excellent stuff from the National Park site), Isle of Arran: go HERE for a useful summary of the Igneous geology of the island, with some dramatic photographs. Also plenty of granite in the SW Peninsula, which is essentially one large granite feature known as a batholith.


ARRAN

There are some classic features on the island: glacial ones too. A useful place for fieldwork too.

Arran has a whole host of important Geological / Geographical case studies that can be used. Try a search for some useful sites.


LIMESTONE: THE YORKSHIRE DALES

OS 1: 25000 Map of Malham area including the classic Malham round, this is well featured in many textbooks, including David Waugh's 'Key Geography for GCSE', and also a GeoActive document on the walk. Also featured in 'Essential Mapskills' spiral bound book mentioned elsewhere on the site. (Once had an interview for a job at Malham Tarn Field Centre, but that's another story..) We have this on the ANQUET MAPS and MEMORY MAP platforms to allow us to see a 3D landscape.

Terrain forming on limestone is known as KARST TOPOGRAPHY. There are various types of limestone, but it is the Carboniferous limestone that we shall be considering.

Rock is permeable, but also soluble in rainwater due to formation of weak carbonic acid as rainwater falls through polluted air. Pure water can dissolve 1 part per 30,000, but as carbonic acid, dissolves 1 part per 7000.

Development of karstic topography depends largely on 4 factors:

a) Solubility: depends on amount of Calcium carbonate. Dolomitic limestone is less soluble than carboniferous or oolitic.

b) Type of permeability:

2 types: rock may be porous throughout, permitting mass permeation through its body, leading to formation of underground channels

or, rock may be dense but has well defined joints and bedding planes through which the transport of water is concentrated (the case with carboniferous limestone) - solution and corrasion form cave systems underground

c) Relief. If the limestone is close to base level, there may only be slight features formed by phreatic water (below the water table)

Where the limestone is higher up, rainwater is able to disappear underground and leave some of the typical features of the Dales, with very little surface drainage. Forms shallow cave systems (vadose) i.e. usually above the water table (below is phreatic - remember VIP...)

d) Rainfall: this is the erosive agent, so more rainfall means more erosion.

Carbonation enlarging cracks in limestone above Malham Cove, Yorkshire Dales. Picture taken by Mister P.

Watlowes Dry Valley, above Malham Tarn. Picture by Mister P.

A good article in the September 2002 issue of 'Geography Review', written by David Atkinson covers a lot of the issues relating to limestone weathering and scenery, and would be well worth reading for those with an interest.

Recently got sent a very nice CD-ROM postcard. Has good information and a VIRTUAL TOUR of the main Malham round. This is well worth buying if you ever go to the area. Wonder if it's available online ?

LIMESTONE PAGE: now with new images of the area thanks to Val Vannet

GRANITE: DARTMOOR AND ITS TORS

For more on Granite landscapes, I recommend Issue 436 of Geofile Online (published January 2003) - this has some excellent information and case study material and a read of this should set up most 'AS' students nicely for the exam.

We have also used a programme from 27 years ago! Called 'The Land' it looks at different areas. Presented by Bill Grundy, the programme on Dartmoor features some good flared trousers and Vauxhall Victors. It has details on the basic features of the landscape:

- 'Moor and Tor' landscape

- Thin acidic soils

- Poor drainage leading to peat formation, blanket bog and standing water

- Usage of the area as military training ground, also a desolate location for prison.

- High rainfall and frequent mist in the area

- Absence of trees in many areas, although there are a few areas of ancient woodland e.g Wistman's Wood, which I remember visiting on an undergraduate fieldtrip.

- Granular disintegration and kaolinisation (hydrolysis) of granite is explored. Chemical weathering. Expansion of joints.

- Mining of china clay around the area: aureole - area surrounding the granite intrusion where rocks are metamorphic.

From the top of Hay Tor looking across to more Tors.

Recently visited the Dartmoor Visitor Centre at Princetown, which is the location of Dartmoor Prison, which you can buy postcards of (cue 'Wish you were here' jokes....) There is a 40 mph speed limit throughout the moor which is a good idea with so many livestock free to wander. Bought a couple of useful resources here. Ranger Ralph is the vehicle used to help teach younger people about the moor. I bought his guide to the moor. Spoke to one of the people in a Tourist Information centre who said that the Moor Care Less Wear had been introduced because of some money that had been made available to fund the project.

One of the best sites on Dartmoor is that produced by Richard Knight, which is linked to from HERE. He has a website featuring walks around Dartmoor, which also has lots of useful information on the moor, as well as the TORS. There are a series of panoramas as well. He has kindly given permission for them to be used for educational purposes. Please contact him via the site if you want to use the image.

The new Coasts series on BBC in November 2006 featured china clay in the programme featuring Devon and Cornwall. It covered Carlyon Bay and its quartz beach, china clay and its uses. Radio Times contains about a third china clay by weight.

For 1 tonne of china clay extracted there are 9 tonnes of waste, which were piled up into hills called the Cornish Alps.

These have been landscaped, and there is a link here with the Eden Project.

Beach at Carlyon Bay is likely to disappear.

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