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Whitley Spring EarthCache

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Hidden : 7/17/2011
Difficulty:
2 out of 5
Terrain:
2.5 out of 5

Size: Size:   not chosen (not chosen)

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Geocache Description:

This Earthcache takes you to a spring very close to the River Sowe in Whitley, Coventry.

Please take care on muddy paths.

Springs are sometimes indicated on Ordnance Survey maps as 'Issues' in reference to the occurrence of water 'issuing' from the ground to the ground surface.

Springs occur in two ways. They may issue from an opening in the ground where water may flow outwards. This could be from joints or fractures within the rock or in karstic (limestone) terrain from a channel created by the flowing water itself. These tyes of springs are known as 'Fracture', 'Fault' & 'Solution' springs.

The second way is much more common in the UK and the Midlands in which groundwater intersects with the ground surface. Typically this intersection occurs in streams and rivers where it is not visible but in some locations, such as here at Whitley it can be identified. This type of spring is known as a 'Contact' spring.

A contact spring occurs where permeable rocks overlie impermeable rocks. Permeability refers to a rocks ability to allow the transmission of water through the pore spaces between the grains or crystals with which it is comprised. No rocks can be termed completely impermeable but can have permeability rates so low as to be effectively considered impermeable.

Reference to the geological map indicates the spring at this location can be seen to coincide with the contact between the Bromsgrove Sandstone Formation (BmS) and the Mercia Mudstone Group (MMG). The boundary lies approximately north to south at this location. As the names of these formations implies this is the contact between a sandstone a mudstone. The permeability of the sandstone is greater than the mudstone as the pore spaces between the sand grains is greater than the pore space between the clay platelets. When the water contained with the sandstone flows downhill (via gravity) to the mudstone contact it is effectively 'dammed' and flows outwards depending upon the local topograpghy.

In order to claim this Earthcache you will need to visit the given coordinates and answer the following questions:

1. What is the approximate diameter of the pool which has formed at the spring?

2. Given this is the boundary between the Bromsgrove Sandstone Formation and the Mercia Mudstone Group, is there any evidence to suggest which rocks lie to the east and which lie to the west? and if so please state your conclusion.

3. Springs often occur in 'Spring lines'. Is there any evidence of a spring line at this location?

4. (Optional) Take a photo of yourself or your GPSr at the given coordinates.

Please email you answers to the questions to me before posting your log. I will attempt to verify your answers as soon as possible so you can post your discover. Please do not post your answers on your log.

Many thanks and good luck.

Additional Hints (No hints available.)