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Damph Hill An Damh A name in Irish
(Ir. An Damh [OSI], 'the stag' or 'the ox') Donegal County, in Carn List, Psammitic schist with pebbly grit beds Bedrock

Height: 420m OS 1:50k Mapsheet: 3 Grid Reference: C43026 37042 This place has been logged as visited by 40 members. Recently by: liz50, Geo, millsd1, Wildrover, Cobhclimber, pearnett, ciarraioch, shaunkelly, melohara, Derry_Danderer, simoburn, chalky, newpark-cc, doopa, Onzy
I have visited this place: NO (You need to be a logged-in member to change this.)

Longitude: -7.325499, Latitude: 55.17866 , Easting: 243026, Northing: 437042 Prominence: 65m,  Isolation: 1.8km
ITM: 642964 937027,   GPS IDs, 6 char: Damph, 10 char: Damph
Bedrock type: Psammitic schist with pebbly grit beds, (Upper Crana Quartzite Formation)

Damph is the 845th highest place in Ireland.

Trackback: http://mountainviews.ie/summit/733/?PHPSESSID=371v7kba8j6ot2lrvruh6d4f00
COMMENTS for Damph 1 of 1
MountainViews.ie Picture about mountain Damph in area Inishowen, Ireland
Picture: Damph viewed from the NE ridge of Slieve Main.
 
Easy access over wet ground with wild views.
Short Summary created by simon3,  16 Sep 2013
An obvious way up Damph is from the road between Buncrana to Glentogher. There are a number of places to start and one place is the unfenced area opposite a dam at around C4426 3722 A.
The Fullerton Pollan dam and reservoir was completed in 1997 however as of 2013 it is not shown on the 1:50,000 OSi map though is on higher zoom levels on the OSi MapGenie layer used by this website.
The walk to the top is over rough wet ground and should not take more than 70 mins there and back.
The summit has fine views over the reservoir and of the Slieve Main to Slieve Snaght ridge. Trackback: http://mountainviews.ie/summit/733/comment/5492/
 
Started at approx. 444373 B at a small quarr .. by gerrym   (Show all for Damph)
 
Rising Damp .. by madfrankie   (Show all for Damph)
 
(End of comment section for Damph.)

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British summit data courtesy:
Database of British & Irish Hills
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"ASTER+": Hillshade and Contours
Courtesy of Tiles GIScience Research Group @ Heidelberg University More detail here
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