Gravestone Photographic Resource

How and why grave monuments become illegible

The gravestone photographic resource project is an attempt to provide a record of grave monuments for future generations. This is important because over time many momuments deteriorate and become unreadable.

There are many reasons for this deterioration including:

early photo of grave at Hove, Sussex (20)

A good example of how grave monuments gradually become less readable over time are these two photos of the same monument but taken years apart:

Notice in particular how water/frost damage has lifted off part of the bottom right of the monument. Once this type of damage starts it usually progresses quite quickly until none of the original surface is left and the monument is completely unreadable.

This is a major reason why the Gravestone Photographs Resource is so important and why it needs more volunteers!

later (2006) photo of grave at Hove, Sussex (20)
wind errosion

Wind errosion

Wind errosion of gravestone monuments is often a very gradual process and is greatly influenced by the type of stone and its position relative to the prevailing wind.

The most likely type of stone to suffer wind errosion are those made from sandstone. Other much harder stones such as granite and slate are the least effected by wind errosion.

wind errosion at Little Common, Sussex (1101)
Example of wind errosion

wind errosion at Little Common, Sussex (1095)
Example of wind errosion

water errosion

Water errosion

water errosion at Castleton, Derbyshire (6841)
Example of water errosion

Like wind errosion, water errosion of gravestone monuments is often a very gradual process and is often greatly influenced by the type of stone and its position relative to the prevailing wind.

The most likely type of stone to suffer wind errosion are those made from sandstone. Other much harder stones such as granite and slate are the least effected by water errosion.

frost errosion

Frost damage

Like wind and water errosion, frost damage to gravestone monuments is greatly influenced by the type of stone. Unlike wind and water errosion, once it starts it can very quickly make a monument completely illegible.

The most likely type of stone to suffer frost damage are those made from soft layered stone such as sandstone. Other much harder stones such as granite are the least effected by frost damage. However occasionally slate which is a very hard but layered stone can be damaged by frost.

Besides actually damaging the stone itself, frost can also cause damage to those stones which have inlayed lettering. When water gets behind inlayed lettering a freezes then the lettering drops out of place.

frost damage at Campsea Ashe, Suffolk (1742)
Example of frost damage

frost damage at Castleton, Derbyshire (6713)
Example of frost damage

frost damage at Campsea Ashe, Suffolk (1736)
Example of frost damage that has caused lettering to fall out.

frost damage at Castleton, Derbyshire (6827)
Example of frost damage

lichen and moss damage

Lichen and moss damage

lichen damage at Barrowby, Lincolnshire (5908)
Example of lichen damage

Unlike wind, water and frost damage to gravestone monuments, it is not so greatly influenced by the type of stone. It is however related to the location and direction the monument is facing as well as the amount of polution in the air.

Moss is most likely to be a problem in the more shaded parts of a cemetery especially where the monument is facing north. It is more common in rural cemeteries where there is little polution.

Lichen damage is much more likely on older stones as it is much slower groing than moss. It is also more likely in rural churchyards where there is little polution. In town cemeteries where there will be more polution, lichen is not such a problem as the polution kills it off before it can do any real damage.

ivy damage

Ivy damage

Ivy can very quickly make a grave monument completely illegible by smothering it with growth. Often this growth can be removed without damage to the underlying stone. However if the monument is made of a soft stone then the roots of the ivy may penetrate it and then eventually remove the top legible layer.

Ivy damage is most often a problem in neglected rural churchyards.

ivy damage at Castleton, Derbyshire (6818)
Example of ivy damage. In this example much of the ivy has been bemoved from the main part of the monument. Although the damage to this monument is not great it clearly shows have the roots do begin to penetrate the soft stone.

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