Talk:Black Hill (Herefordshire)

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Geology[edit]

I have added an external link on the local geology since a previous editor seems not to appreciate the local landslips, or the Old Red Sandstone structure. 31.52.9.44 (talk) 06:43, 20 September 2015 (UTC)[reply]

I have also added further details of the ridge walk, and local parallels, such as the ridge walk on the [Skirrid]] a few miles away to the south, and composed of similar Old red Sandstone rocks. Other topographical features such as the Hatterall ridge, could be improved in a similar way. (talk) —Preceding undated comment added 12:01, 20 September 2015 (UTC)[reply]

That 'other editor' - me - has left a message on your talk page about some of this, User 31.52.9.44 It's not about 'appreciating' the landslips, it's about providing a reference for them. cheers Geopersona (talk) 12:57, 20 September 2015 (UTC)[reply]
User 31.52.9.44 - you have added this : Such landslips were probably formed at the end of the last Ice age when meltwater undermined the strata. - where is the evidence for this statement? ie a reference from a book or the web that can be included in a references section in this article. You may think that this explanation is the case, indeed that may be the reason that some landslips have occurred but I suspect not in the case of landslips high on these hills - more likely is that slopes were over-steepened by glacial action. I don't have the evidence for my statement either so haven't added it - it remains speculation. Unsupported material entered into articles is likely to be removed as per Wikipedia policy. Please contribute to the expansion of these articles but not with material that cannot be backed up. thanks Geopersona (talk) 03:42, 22 September 2015 (UTC)[reply]

External links modified[edit]

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