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((More citations needed|date=December 2022))
((Use dmy dates|date=April 2022))
((Short description|Mountain in the English Lake District, Cumbria, England))
((Infobox mountain
| name = Clough Head
| photo = HighRigg StJohnsVale.JPG
| photo_caption = Threlkeld Knotts (left) and Clough Head (centre) showing the craggy western side of the fell
| elevation_m = 726
| prominence_m = 108
| parent_peak = [[Great Dodd]]

| location = [[Cumbria]], [[England]]
| range = [[Lake District]], [[Eastern Fells]]
| grid_ref_UK = NY333225
| topo = [[Ordnance Survey|OS]] ''Landranger'' 90, ''Explorer'' OL5
| map = United Kingdom Lake District
| map_caption = Location in Lake District, UK
| coordinates = ((coord|54.59326|N|3.03379|W|type:mountain_scale:100000|format=dms|display=inline,title))
))

'''Clough Head''' (((IPAc-en|pron|k|l|ʌ|f|_|h|ɛ|d))) (<small>meaning:</small> ''hill-top above the ravine'') is a [[fell]], or hill, in the [[England|English]] [[Lake District]]. It marks the northern end of the main ridge of the [[Helvellyn range]] and is often walked as part of the ridge walk. The fell stands south of the village of [[Threlkeld]] and the [[A66 road]], and it forms the steep eastern side of the tranquil valley of [[St John's in the Vale]].

On its western side the fell displays a dark mass of rocky crags and a deep-set rocky ravine. On the other side it has smooth grassy slopes. Beneath the north face is the steep valley or clough from which Clough Head gets its name. Also beneath the steep northern face lies the lower hill of Threlkeld Knotts, a granite hill which has been much quarried round its margin.

A number of different types of rock are found on and around Clough Head, which were formed in very different circumstances. These include deep-sea sedimentation, effusive volcanic lava flows, explosive volcanism, an intrusion of granite, mineralisation and finally glacial sculpting. To understand the geology of Clough Head is to understand much of the geology of the Lake District.

An old route known as the Old Coach Road passes beneath Clough Head. Most of the fell is [[Freedom to roam#England and Wales|Open Access]] land, which walkers can enter from either end of the Old Coach Road, or from a lane south of the village of Threlkeld. Four main routes lead to the summit.

==Topography==
With a height of 726&nbsp;m, Clough Head is the lowest summit of the Helvellyn range.

Gentle grass-covered slopes on the south and east sides of the fell drop to a broad col and to Mosedale, both of which separate Clough Head from [[Great Dodd]], its neighbour to the south. To the north of the summit the ground drops abruptly down a steep scree-covered and craggy slope which marks the northern end of the Helvellyn range. This face is called Red Screes from the colour of the rock.

Beneath Red Screes is the lower, rounded, grassy hill of Threlkeld Knotts. This hill rises gently from the valley of the River Glenderamackin, which separates the Helvellyn range of fells from [[Blencathra]] and the northern Lakeland fells. A steep valley to the east of Threlkeld Knotts, which begins immediately below Red Screes, is the clough from which Clough Head is named. In the bottom of this valley there is a sheepfold known as Clough Fold.<ref name=OS25k>Ordnance Survey 1:25,000 Explorer map</ref>

[[File:Sandbed Gill - geograph.org.uk - 116521.jpg|thumb|left|Sandbed Gill]]
Steep rocky crags guard the whole western side of the fell, rising abruptly from the green valley of St John's in the Vale. This western face of Clough Head, is steep, rough and rocky. The principal rock features are, from north to south: Buck Castle, Wanthwaite Crags and Bram Crag. South of Wanthwaite Crags is the very steep Fisher's Wife's Rake, a grassy break in the cliffs (though with scree) which allows determined fell-walkers to ascend the fell on this side. North of Bram Crag is a deep-seated rocky ravine called Sandbed Gill. This gill contains a considerable flow of water in its rocky gorge, but it often has only a dry bed by the time it gets down to valley level.<ref name=wainwright>((cite book | author = Alfred Wainwright | author-link = Alfred Wainwright | title = [[A Pictorial Guide to the Lakeland Fells]] Book 1: The Eastern Fells | publisher = Frances Lincoln | location = London | year = 2003 | orig-year = 1955 | isbn = 0711222274 ))</ref>

North-east of the summit of Clough Head is the lesser top of White Pike. From here the ridge descends and gradually broadens into the rough expanse of Thelkeld Common.

The western slopes of Clough Head drain into St John's Beck, which flows north into the River Greta, and which in turn joins the River Derwent at Keswick. The southern and eastern slopes drain into Mosedale and Mosedale Beck, which also joins the River Greta, via the River Glenderamackin.<ref name=OS25k/>

{| style="width: 100%; height: 150px" border="1" class="wikitable"
|+ Clough Head and its Subsidiary Tops<ref>((cite web |title=Database of British and Irish Hills |url=http://www.hill-bagging.co.uk/|access-date=11 March 2016))</ref>
! Name
! Grid Reference
! Height
! Prominence
! Classification
(height and prominence)
! Classification
(authors’ listings)
|-
!Clough Head||((gbmappingsmall|NY 33394 22540))||((convert|726|m|disp=br()))||((convert|108|m|disp=br()))||[[Lists of mountains and hills in the British Isles#HuMPs|HuMP]], [[Lists of mountains and hills in the British Isles#Hewitts|Hewitt]], [[Lists of mountains and hills in the British Isles#Nuttalls|Nuttall]]||[[Lists of mountains and hills in the British Isles#Wainwrights|Wainwright]], [[Lists of mountains and hills in the British Isles#Birketts|Birkett]]
|-
!White Pike||((gbmappingsmall|NY 33900 22950))||((convert|627|m|disp=br()))||((convert|6|m|disp=br()))|| ||
|-
!Threlkeld Knotts||((gbmappingsmall|NY 33015 23023))||((convert|514|m|disp=br()))||((convert|18|m|disp=br()))|| ||[[Lists of mountains and hills in the British Isles#Birketts|Birkett]]
|-
|}

==Threlkeld Knotts==
Threlkeld Knotts (<small>meaning:</small> ''the knobbly hill above Threlkeld'') is a lower, rounded hill, nestling against and overshadowed by the steep northern face of Clough Head. Its curving summit ridge contains three small tops,<ref name=OS25k/> each of which is marked by a cairn. From Threlkeld Knotts there is a striking view of Red Screes just above, and a narrow path slants up through the crags to the west shoulder of Clough Head.

On the northern slope of Threlkeld Knotts, not far above the large quarry, are the remains of an [[Iron Age]] settlement. The documented remains include seven hut circles, five enclosures, two trackways, a field system, and some fifty cairns which probably represent field clearances.<ref>((cite web | url = http://archaeologydataservice.ac.uk/archsearch/record.jsf?rcn=LDNPHER11-1125 | title = Settlement, etc on St John's & Threlkeld Commons | website = Archaeology Data Service | access-date = 12 June 2014))</ref><ref>((Cite PastScape |mnumber=10444 |mname= | accessdate=13 June 2012))</ref> Remains of enclosure walls may still be seen, about ((convert|200|m|-1)) north of the Old Coach Road.<ref name=wainwright/>

==Old Coach Road==
An old route, marked on maps as "Old Coach Road" crosses the northern slopes of Threlkeld Knotts and skirts the eastern side of Clough Head, reaching a height of ((convert|437|m))<ref name=OS50k>Ordnance Survey 1:50,000 Landranger map</ref> as it crosses from Wanthwaite (((IPAc-en|pron|'|w|ɒ|n|.|θ|ɛ|t))<ref name=wainwright/>) in [[St John's in the Vale]] to High Row near Dockray. This has suffered from rain water erosion in recent years, but remains a useful track for walkers.<ref name=richards>((cite book | author = Mark Richards | title = Near Eastern Fells | publisher = Cicerone Press | location = Milnthorpe | year = 2008 |orig-year = 2003 | isbn = 978-1-852845414 ))</ref> Near the summit of the road is Hause Well, a spring issuing from a crevice in the rock.<ref name=wainwright/> The [[Ordnance Survey]] 1:25,000 map shows the road as an "other route with public access" and as a "traffic-free cycle route;" it does not show it as either a "[[Rights of way in England and Wales#byways open to all traffic|byway]]" or a "[[Rights of way in England and Wales#restricted byways|restricted byway]]".<ref name=OS25k/> However, official signs present on the gates at both ends of the road clearly show that access by motorised vehicles is permitted.

==Routes==
[[File:Fisher's Wife's Rake - geograph.org.uk - 232521.jpg|thumb|left|Fisher's Wife's Rake]]
The whole of Clough Head, Threlkeld Knotts and Threlkeld Common (above the [[Wikt:intake|intake]] wall which encloses the lower agricultural land and Threlkeld Quarry) is [[Freedom to roam#England and Wales|Open Access]] land. Entry to this land can be had from three points: from either end of the Old Coach Road, or from the lane leading to Newsham Farm. This lane begins opposite Threlkeld village, or it can be joined from the disused railway line alongside the road to the quarry.<ref name=OS25k/>

'''Walkers''' may approach the summit by means of four principal routes. A narrow footpath leads from the Old Coach Road (at a point ((convert|250|m|-1)) east of Hause Well) to White Pike and then on to the summit.<ref name=wainwright/><ref name=richards/>

Another narrow path leads from Threlkeld Knotts, slanting up through the crags and scree of Red Screes to emerge on the west shoulder of Clough Head. From there one may go up gentle grassy slopes to the summit,<ref name=wainwright/><ref name=richards/> although the main path contours round to meet the track coming up from Great Dodd, which suggests that many ridge-walkers bypass the top (just as the ridge path bypasses nearly all the other tops of the range.)

From the south, the ridge track from Great Dodd leads straight up the long gentle slope to the top.<ref name=wainwright/>

Finally, Fisher's Wife's Rake is a possible route up through the crags on the west side of Clough Head for energetic and determined walkers,<ref name=richards/> but it is "''very'' steep."<ref name=wainwright/>

'''Climbers''', or scramblers with some rock-climbing experience and a rope for the more difficult pitches, can ascend the hidden recesses of Sandbed Gill.<ref>
((cite book | author = Brian Evans | year = 2005 | orig-year = 1982 | title = Scrambles in the Lake District, Vol. 2: Northern Lakes | publisher = Cicerone Press | location = Milnthorpe, Cumbria | isbn = 1852844639 ))</ref><ref name=allen>((cite book |author =  Bob Allen |date = 2005 |orig-year = 1987 |title = On High Lakeland Fells | edition = revised |publisher = Frances Lincoln |location = London |isbn = 0711225273 ))</ref> Sandbed Gill was the first new route in the Lake District to be pioneered by the brothers George and Ashley Abraham in 1890. Although George was only 18 at the time, and Ashley 14, they had already gained true rock-climbing skills elsewhere in the Lakes.<ref>((cite web | url = http://footlesscrow.blogspot.co.uk/2010/06/abraham-brothersphotographing-past.html | title = The Abraham Brothers | author = A H Griffin | date = 2010 | website = Footless Crow | access-date = 12 June 2014 ))</ref> Walkers should leave the gill well alone.<ref name=allen/>((rp|147))

Clough Head is often included as the first (or last) step of a traverse of the Helvellyn range. It may also be included in a longer version of the horseshoe walk around Deepdale which takes in the three "Dodds" to its south. This walk begins at High Row and takes advantage of the Old Coach Road.<ref>((cite book |author = John Gillham |author2 = Ronald Turnbull |name-list-style=amp|date = 2001 |title = Rambler’s Guide: Lake District |publisher = HarperCollins|location = London |isbn = 0-00-2201364 ))</ref>

==Summit==
[[File:Trig Point at Clough Head - geograph.org.uk - 232507.jpg|thumb|The summit of Clough Head and the view to the west]]
The summit is marked by an [[Ordnance Survey]] triangulation column and a wind shelter. It provides a good view of Blencathra to the north, and a wide, all-round view, broken only by Great Dodd, with glimpses of both the [[Solway Firth]] to the north and [[Morecambe Bay]] to the south.<ref name=richards/> To the south-west the vista of the high fells is "especially striking".<ref name=wainwright/>

[[Alfred Wainwright]] included a drawing of himself regarding Blencathra from this viewpoint in his ''[[Pictorial Guides to the Lakeland Fells]]''.<ref name=wainwright/> Mark Richards recommends White Pike as a better place for contemplating the view.<ref name=richards/>

==Geology==
The rocks of Clough Head belong to both the [[Skiddaw Group]] and the [[Borrowdale Volcanic Group]], both of which date from the [[Ordovician]] period.

An east-west geological [[fault (geology)|fault]] just north of the summit has brought these two rather different rock groups side by side. To the north, including White Pike, much of Threlkeld Common and the margins of Threlkeld Knotts are rocks of the '''Buttermere Formation''', part of the Skiddaw Group.<ref name=BGSmap>((cite map |publisher= [[British Geological Survey]]|title= Sheet E029, Keswick (Solid) |map= 1:50,000 Geological Maps | date = 1999|isbn= 0751832294)) - may be viewed on the ((cite web |url= http://www.bgs.ac.uk/discoveringGeology/geologyOfBritain/viewer.html|title= Geology of Britain viewer|author=<!--Staff writer(s); no by-line.--> | website= British Geological Survey)) or on the BGS's iGeology smartphone app</ref> Mudstones, siltstones and sandstones which had been deposited in deep water on the northern margin of an ancient continent ([[Avalonia]]) in the early Ordovician Period were chaotically disrupted by a huge undersea avalanche to form an [[olistostrome]] deposit in which blocks of rock are now embedded in a matrix of mudstone, and intensely deformed by minor folds, slumps and shears. This event can be dated to about 460 million years ago.<ref name=stone>((cite book |author=P. Stone |date=2010 |title=British Regional Geology: Northern England | publisher = British Geological Society| location = Nottingham |isbn = 978-0852726525|display-authors=etal))</ref>

The deep sea deposits of the Skiddaw Group were raised above sea level by the [[subduction]] of ocean crust from the north beneath the continent to the south. This uplift was followed by a brief (about 5 million years) period of intense volcanic activity, up to about 450 million years ago.<ref name=stone/>((rp|9, 35))

To the south of the fault on Clough Head are rocks of the '''Birker Fell Andesite Formation'''. These rocks are among the earliest of the volcanic rocks of the Borrowdale Volcanic Group, and are part of a thick succession of [[andesite]] sheets which now outcrop in a wide band around the western and northern sides of the Lake District.<ref name=BGSmap/> These sheets were formed by successive eruptions of mobile andesitic lava from shallow-sided volcanoes. The composition of the erupting magma varied from time to time, and the geological map shows an area of [[basaltic andesite]] along the crags on the western side of the fell, and areas of [[dacite]] higher on the fell.<ref name=BGSmap/> Individual lava flows may be separated by beds of volcaniclastic sandstone, that is, sedimentary deposits formed from the erosion of the volcanic rocks and deposited by streams, floods and possibly wind.<ref name=stone/>((rp|46)) The geological map shows a number of areas of volcaniclastic sandstone on the crags on the west side, as well as a larger area surrounding the summit, into which an andesite [[sill (geology)|sill]] was intruded.<ref name=BGSmap/>

After the eruptions of the Birker Fell Formation, the composition of the erupting magma changed from largely andesitic to predominantly [[dacite|dacitic]], and as a result the nature of the volcanism became more explosive.<ref name=woodhall>((cite book |author = D. G. Woodhall |date= 2000 |title = Geology of the Keswick District (Sheet Explanation of BGS Sheet E029) | publisher = British Geological Survey |location = Nottingham ))</ref>

In the area to the north of [[Sticks Pass]] the Birker Fell andesites are overlain by the '''Lincomb Tarns Tuff Formation'''. This [[formation (stratigraphy)|formation]] is one of the most widespread of the volcanic rocks of the Lake District; it seems that the whole district was buried beneath at least 150&nbsp;m of densely welded [[ignimbrite]], a rock formed from a [[pyroclastic flow]] of very hot gas and rock. This formation must represent a series of eruptions of truly exceptional magnitude, accompanying the formation of a volcanic [[caldera]] probably in the area around what is now Helvellyn.<ref name=stone/>((rp|55))

On Clough Head a small sheet of the '''Thirlmere Tuff Member''' covers the summit of the fell, a [[Geological unit#member|member]] of the Lincomb Tarns Formation. This rock is a [[rhyolite|rhyolitic]] [[Lapilli|lapilli-tuff]] in which the individual pieces of semi-molten lava were flattened under the weight of deposits above them.<ref name=BGSmap/>

Towards the end of, or after the cessation of the volcanic activity a large granite [[batholith]] was emplaced in stages beneath the volcanic rocks of the Lake District.<ref name=stone/> Threlkeld Knotts consists largely of an intrusion of micro-granite, known as the '''Threlkeld Intrusion''',<ref name=BGSmap/> a part of the larger batholith. The granite was intruded into rocks of the Skiddaw Group and the base of the Borrowdale Volcanic Group. [[Uranium-lead dating]] has established an age of 451±1.1 million years for this intrusion.<ref name=stone/>

Seven quarries around the western side of Threlkeld Knotts have worked the microgranite. In addition to the large Threlkeld Quarry there are smaller workings at Birkett Bank, Hilltop Quarries and Bramcrag Quarry.<ref name=OS25k/> Threlkeld Quarry was opened in 1870 to supply railway ballast for the Crewe to Carlisle railway line. Production increased in the 1890s with material for [[Thirlmere|Thirlmere Reservoir]] and for roadstone.<ref>((Cite PastScape |mnumber=1466061 |mname=Threlkeld Granite Quarry | accessdate=13 June 2012))</ref> The quarry closed in the 1980s and now houses the Threlkeld Quarry and Mining Museum.<ref>[http://www.threlkeldquarryandminingmuseum.co.uk Threlkeld Quarry and Mining Museum] retrieved 14 June 2014</ref>

'''Mineral veins''' have been formed in many Lake District rocks by [[hydrothermal]] circulation of groundwater though geological [[fault (geology)|faults]] and are often associated with the granite batholith.<ref name=stone/>((rp|189)) [[Vein (geology)|Veins]] containing lead and copper ores were found on Wanthwaite Crag where there are several old mineral workings, some very old. The most recent lease was taken out in 1887 by the short-lived and unsuccessful Wanthwaite Crag Mining Company.<ref name=adams>((cite book | author = John Adams | title = Mines of the Lake District Fells | publisher = Dalesman | location = Skipton | year = 1995 | isbn = 0852069316 ))</ref>

The lower promontory of Threlkeld Knotts north of Clough Head is scarred and flanked by 'rock slope failure' fractures and landslips, and views from the A66 and Blencathra could suggest that the whole mass of the Knotts has descended from the concavity in the north face, which is not a true glacial cirque (Lakeland combe), but this remains debatable.<ref>Jarman D and Wilson PW (2015): Clough Head - Threlkeld Knotts: a perplexing RSF complex. In McDougall DA and Evans DJA (eds), The Quaternary of the Lake District - Field Guide. Quaternary Research Association, London, 153-173.</ref> Rock slope failure also patterns White Pike with antiscarps (uphill-facing scarplets), which could formerly have extended across the Clough Head cavity.

==Names==
'''Clough Head''' was called ''Threlkeld Fell'' in [[Thomas West (priest)|Thomas West's]] 1778 guide book.<ref>((cite book | author = Thomas West | date = 1821 | orig-year = 1778 | title = A Guide to the Lakes in Cumberland, Westmorland and Lancashire |  edition = 11th |publisher = W Pennington |location = Kendal |page = 85 )) - available online at [http://www.geog.port.ac.uk/webmap/thelakes/html/lakemenu.htm www.geog.port.ac.uk]. Accessed 10 June 2014</ref> Its present name, Clough Head, was first recorded by the [[Ordnance Survey]] in 1867. Clough is a dialect word from the [[Old English]] ''clōh'', a ravine. This appears to be a reference to a steep valley just below Red Screes, and which contains a sheepfold called Clough Fold.<ref name=OS25k/> Thus Clough Head is "the hill-top above the ravine."<ref name=whaley>Diana Whaley, ''A Dictionary of Lake District Place-Names'', English Place-Name Society 2006, ((ISBN|0-904889-72-6))</ref>

'''White Pike''' is "the pale summit," recorded since 1774, probably named from its pale-coloured rock, and perhaps in contrast to the reddish colour of Red Screes beneath the main summit.<ref name=whaley/>

'''Threlkeld Knotts''' was first recorded by the [[Ordnance Survey]] in 1900. Knott is a dialect word from the [[Old Norse]] ''knǫttr'', 'ball, hard round mass' used of compact or craggy hills. Hence Threlkeld Knotts is "the knobbly hill above Threlkeld", a place-name recorded from as early as 1197 and meaning "the slaves' spring" from the Old Norse ''þræla'', 'thrall, slave,' and Old Norse ''kelda'', 'a spring.'<ref name=whaley/> 'Thrall' may have been the word used by the Norse settlers to refer to the native Britons.<ref name=gambles>
((cite book | author = Robert Gambles | title = Lake District Place Names | publisher = Hayloft Publishing Ltd. | location = Kirkby Stephen, Cumbria | year = 2013 | isbn = 1-904524-92-3 ))</ref>

'''Fisher's Wife's Rake''' is "Mrs Fisher's Path." Rake is a dialect word of unknown origin which refers to a narrow path on a hill.<ref name=whaley/>((rp|415)) Mark Richards claims that the name comes from the Fisher family of Rake How across the valley. He says the husband cut [[peat]] on the col above and his wife hauled it down by sled, but he gives no indication of the source of this information.<ref name=richards/>

==Notes and references==
'''Notes'''
((Reflist|group=note))
'''References'''
((Reflist))

((Eastern Fells))
* [[List of hills in the Lake District]]
* [[List of fells in the Lake District]]

[[Category:Fells of the Lake District]]
[[Category:Hewitts of England]]
[[Category:Nuttalls]]

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Module:Citation/CS1/Date validation (view source) (protected)
Module:Citation/CS1/Identifiers (view source) (protected)
Module:Citation/CS1/Utilities (view source) (protected)
Module:Citation/CS1/Whitelist (view source) (protected)
Module:Citation/CS1/styles.css (view source) (protected)
Module:Convert (view source) (template editor protected)
Module:Convert/data (view source) (template editor protected)
Module:Convert/text (view source) (template editor protected)
Module:Coordinates (view source) (protected)
Module:Coordinates/styles.css (view source) (protected)
Module:DecodeEncode (view source) (template editor protected)
Module:Disambiguation/templates (view source) (protected)
Module:Find sources (view source) (template editor protected)
Module:Find sources/config (view source) (template editor protected)
Module:Find sources/links (view source) (template editor protected)
Module:Find sources/templates/Find sources mainspace (view source) (template editor protected)
Module:Footnotes (view source) (template editor protected)
Module:GetParameters (view source) (template editor protected)
Module:IPAc-en (view source) (template editor protected)
Module:IPAc-en/data (view source) (template editor protected)
Module:IPAc-en/phonemes (view source) (template editor protected)
Module:IPAc-en/pronunciation (view source) (template editor protected)
Module:If empty (view source) (protected)
Module:Infobox (view source) (template editor protected)
Module:Infobox/styles.css (view source) (template editor protected)
Module:InfoboxImage (view source) (template editor protected)
Module:Lang (view source) (template editor protected)
Module:Lang/ISO 639 synonyms (view source) (template editor protected)
Module:Lang/data (view source) (template editor protected)
Module:Language/data/iana languages (view source) (template editor protected)
Module:Language/data/iana regions (view source) (template editor protected)
Module:Language/data/iana scripts (view source) (template editor protected)
Module:Language/data/iana suppressed scripts (view source) (template editor protected)
Module:Language/data/iana variants (view source) (template editor protected)
Module:Location map (view source) (template editor protected)
Module:Location map/data/United Kingdom Lake District (view source) (semi-protected)
Module:Location map/styles.css (view source) (template editor protected)
Module:Math (view source) (protected)
Module:Message box (view source) (protected)
Module:Message box/ambox.css (view source) (protected)
Module:Message box/configuration (view source) (protected)
Module:Namespace detect/config (view source) (protected)
Module:Namespace detect/data (view source) (protected)
Module:Native name (view source) (template editor protected)
Module:Navbar (view source) (protected)
Module:Navbar/configuration (view source) (protected)
Module:Navbar/styles.css (view source) (protected)
Module:Navbox (view source) (template editor protected)
Module:Navbox/configuration (view source) (template editor protected)
Module:Navbox/styles.css (view source) (template editor protected)
Module:Ns has subpages (view source) (protected)
Module:Ordnance Survey coordinates (view source) (template editor protected)
Module:Pagetype (view source) (protected)
Module:Pagetype/config (view source) (protected)
Module:Pagetype/disambiguation (view source) (protected)
Module:Pagetype/setindex (view source) (protected)
Module:Pagetype/softredirect (view source) (protected)
Module:ParameterCount (view source) (template editor protected)
Module:Plain text (view source) (template editor protected)
Module:SDcat (view source) (protected)
Module:Separated entries (view source) (protected)
Module:String (view source) (protected)
Module:String2 (view source) (template editor protected)
Module:TableTools (view source) (protected)
Module:Unicode data (view source) (template editor protected)
Module:Unsubst (view source) (protected)
Module:WikidataIB (view source) (template editor protected)
Module:WikidataIB/nolinks (view source) (template editor protected)
Module:WikidataIB/titleformats (view source) (template editor protected)
Module:Wikitext Parsing (view source) (protected)
Module:Yesno (view source) (protected)

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