11 a WALK in LATHKILL DALE Together in Prayer

Total Page:16

File Type:pdf, Size:1020Kb

11 a WALK in LATHKILL DALE Together in Prayer our sandwiches overlooking the village green, the only sound A WALK IN LATHKILL DALE being the excited children in the school playground. Recently on a lovely September day, my wife and I Our return journey was via the lane and across fields to One decided to try a slightly longer walk than we usually do Ash Grange, now boasting a horse riding area as well as the these days. We opted for Lathkill Dale, one of our sleeping barn. We also noticed the ancient pig pens had favourites for more than fifty years. We decided to park at undergone some repair. I wondered if they could be Over Haddon and walk to Monyash and back. When I was converted to guest sleeping quarters as many farms now driving I often parked down the road to Lathkill Lodge but branch out into the tourist industry. Of course I am wrong - my wife opted to stay in the car park at a cost of £4 - still this would not be new because the Grange was an outpost for cheaper than a seat in the "Gods" at the Lyceum. As we the monks of Roche Abbey. I am always puzzled why they passed my former parking spot, now reserved for vehicles needed to go so far afield at a time before so many houses with disabled stickers, I was reminded of probably the last occupied the land. time I drove there. We took our friends Sandy and Jenny The drop down from the farm into Cales Dale does not get from Crieff for a walk in the dale. There was a superb any easier with advancing years. Part of this ancient pathway motorcycle already parked there and Sandy had to is undergoing some archaeological and restoration work. As examine and admire it. At this point the owner returned my wife read the little notice alongside about the monks and asked Sandy if he'd like to drive it. "My word yes" going down to "wash their feet" she wondered how they said Sandy. We were relieved it wasn't a genuine offer as coped on such a rough path in sandals. She hadn't got her Sandy was then in his nineties! Later that week we took specs on and should have read "to wash their sheep". On across Cales Dale and up the steep path on the opposite them to the theatre in Chesterfield, having booked by bank, easier than it used to be now steps have been made. telephone. When I collected the tickets at the box office After a rest at the top, on to Calling Low. When we first came the young lady wanted proof of our eligibility for the this way the public path was in front of the house and through cheaper OAP rate, so Sandy had to show himself! the farmyard where drinks could be purchased. Then on to As we sat off along the concessionary path up the dale my Back Lane, down to Conksbury, though we soon left it to wife saw that the notice about the charge on the Thursday of cross the fields to Meadow Place Grange. This place always Easter week still stands at one penny ("old" money). Do seemed to have a very messy muddy entrance from this walkers on that day have to carry such coinage? There was direction. It is one of the many places we think it would be more water in the river than normal in late summer so we great to see it a couple of hundred years ago. In such a huge wondered if it would be coming out of the hill higher up the place we have rarely seen more than one person whereas dale. Before that we had a look at the remains of the aqueduct formerly it must have been a hive of activity. As we trudge which fed the Mandale Mine. The remains, now much less through the farm I saw lots of metal girders around some of than we first knew them, seem smaller each time we pass. the walls -the type used on dangerous road curves. It set me The next point of interest for us was the remains of Bateman's musing. Had they been bought second hand? Had they been House, now made accessible by a bridge across the river. I bent to shape in situ? Were they going to introduce bull first became aware of this spot in the 1940's, before we were fighting as a tourist attraction? Too fanciful of course but it married. We stayed for a week at Manor Farm in Over kept me going as the legs wearied. Onward down to the ford Haddon and walked each day. On this occasion as we passed across the Lathkill where we watched a dog enjoying himself the ruins, an attractive young lady who had been sunbathing in the river after his evening walk. Finally the climb up to the there, got up and walked down to the river. The attraction for car after some seven hours away. A lovely day but thank a young chap like me was that she was absolutely naked and goodness we hadn't attempted the similar walk we used to do, didn't try to hide it. Unfortunately I wasn't allowed to linger! parking at Alport, walking via Conksbury Bridge to Lathkill On this present visit the interest was of a different kind. A Lodge and, after the walk we did today to Back Lane, then mineshaft underneath the house has been provided with a returning through Bradford Dale instead of Meadow Place safety fence and a substantial ladder to descend underground. Grange. Unfortunately, when I went down, it was too dark to see Oh to be younger again! much. Apparently the shaft under the house had housed a Don Ashford revolutionary new type of pumping engine to remove water from the mine. The roar of rushing water down the shaft was ample evidence of the problems the miners faced. Together in Prayer As we continued up the dale we came to the waterfall, much Women’s World Day of Prayer is this year organised by the more impressive than usual. Because there was so much Women of Poland. It occurs on the first Friday of March water it came over in one huge cascade instead of the usual every year and will celebrated all over the world. In Totley it four or five smaller streams. We didn't see the usual dippers will be led be Dr.Marion Jepson at Totley Rise Methodist (birds!) perhaps because we became interested in two Church, Friday 4 th March 10:00. children, just old enough to start walking. They were in the All welcome – refreshments served. charge of two young ladies, presumably their mothers. What Rosemary Belbin 236 3027 fascinated us was how they had reached this isolated spot so far from easy access. Then on past the medieval sheep wash to the Lathkill Head cave where, as anticipated, the river issued forth in quantity. Solution to Counting Camels. Having left here we then had to tackle the extremely rocky For those who didn't spot it, the fractions allocated part of the dale to get to Monyash. It was sad to see, as we to the three sons only account for seventeen exited the dale, a notice on the new toilet block that it had been vandalised. City habits spread to the country. In spite of eighteenths of the estate. Perhaps the other the above comment, Monyash was as quiet as usual as we ate eighteenth was for the harem! Don Ashford 11 .
Recommended publications
  • State of Nature in the Peak District What We Know About the Key Habitats and Species of the Peak District
    Nature Peak District State of Nature in the Peak District What we know about the key habitats and species of the Peak District Penny Anderson 2016 On behalf of the Local Nature Partnership Contents 1.1 The background .............................................................................................................................. 4 1.2 The need for a State of Nature Report in the Peak District ............................................................ 6 1.3 Data used ........................................................................................................................................ 6 1.4 The knowledge gaps ....................................................................................................................... 7 1.5 Background to nature in the Peak District....................................................................................... 8 1.6 Habitats in the Peak District .......................................................................................................... 12 1.7 Outline of the report ...................................................................................................................... 12 2 Moorlands .............................................................................................................................................. 14 2.1 Key points ..................................................................................................................................... 14 2.2 Nature and value ..........................................................................................................................
    [Show full text]
  • Reconstructing Palaeoenvironments of the White Peak Region of Derbyshire, Northern England
    THE UNIVERSITY OF HULL Reconstructing Palaeoenvironments of the White Peak Region of Derbyshire, Northern England being a Thesis submitted for the Degree of Doctor of Philosophy in the University of Hull by Simon John Kitcher MPhysGeog May 2014 Declaration I hereby declare that the work presented in this thesis is my own, except where otherwise stated, and that it has not been previously submitted in application for any other degree at any other educational institution in the United Kingdom or overseas. ii Abstract Sub-fossil pollen from Holocene tufa pool sediments is used to investigate middle – late Holocene environmental conditions in the White Peak region of the Derbyshire Peak District in northern England. The overall aim is to use pollen analysis to resolve the relative influence of climate and anthropogenic landscape disturbance on the cessation of tufa production at Lathkill Dale and Monsal Dale in the White Peak region of the Peak District using past vegetation cover as a proxy. Modern White Peak pollen – vegetation relationships are examined to aid semi- quantitative interpretation of sub-fossil pollen assemblages. Moss-polsters and vegetation surveys incorporating novel methodologies are used to produce new Relative Pollen Productivity Estimates (RPPE) for 6 tree taxa, and new association indices for 16 herb taxa. RPPE’s of Alnus, Fraxinus and Pinus were similar to those produced at other European sites; Betula values displaying similarity with other UK sites only. RPPE’s for Fagus and Corylus were significantly lower than at other European sites. Pollen taphonomy in woodland floor mosses in Derbyshire and East Yorkshire is investigated.
    [Show full text]
  • Youlgreave to Lathkill Dale Circular
    Youlgreave to Lathkill Dale Let's Go Peak District II Circular Route Summary This walk is an absolute gem, starting and ending in the pretty village of Youlgreave. The route follows the crystal- clear River Bradford through shady woodland, before heading to Lathkill Dale. It then follows the River Lathkill through dramatic limestone gorges before returning to the start. Route Overview Category: Walking Length: 12.310 km / 7.69 mi Last Modified: 15th August 2019 Difficulty: Medium Rating: Unrated Surface: Moderate Date Published: 15th August 2019 Description Youlgrave Circular via Lathkill Dale Details Distance: 7.6 miles Time: 3-4 hours Terrain: Grassy footpaths, woodland trails and country lanes Accessibility: Moderate - stiles, squeeze stiles, kissing gates, steps, uneven terrain on woodland paths. Start and end grid reference: SK 21190 (Postcode DE45 1WL; /// petal.rang.plausible) Introduction This wonderful walk is an absolute gem, starting and ending in the very pretty village of Youlgreave. The route follows the crystal-clear River Bradford through shady woodland, before heading across open countryside to Lathkill Dale. It 1 / 4 then follows the course of the River Lathkill through dramatic limestone gorges before returning along field tracks and country lanes to the start point. This is a walk of 7.6 miles. There are stiles and squeeze stiles, although no terribly steep ascents. Youlgreave is well served for cafes and pubs, as well as shops to buy picnic supplies for an en-route stop. There is plenty of car parking available in Youlgreave, both in car parks (fees apply) or on the road side. Allow 3-4 hours to complete this walk at a moderate pace, more if you allow for rest stops and a lunch break.
    [Show full text]
  • Sunday 03 May 09
    What to take on a walk On Walks Drinking water Please try to be there 10 minutes before start time to allow time to put boots on & take walks Comfortable walking boots (not register. trainers) Before going on a walk please ensure that your level of fitness is adequate. Packed lunch Walk Grades Waterproof jacket and over-trousers. Leisurely (L) - This will be most evening walks. Suitable for reasonably fit people with at least a little Walking trousers (not jeans) country walking experience. Walking boots and warm, waterproof clothing are recommended. Terrain Fleece or other warm top Includes unsurfaced country paths that may be narrow, uneven, muddy or overgrown, and See http://www.lrwg.org.uk/resources/walkers obstructions such as stiles, narrow bridges, stepping for more information. stones and steps. May be hilly, with a few ascents and descents. May also include walks that would Very occasionally it is necessary to change otherwise be graded easy access or easy but are walks due to unforeseen circumstances. longer than 8km/5 miles. Pace Slow or moderate Please check the website for any changes pace; could include otherwise easy walks taken at a since this programme was printed. E&OE. moderate pace. Moderate (M) - This will be most Sunday walks around Leicestershire. Suitable for people with country walking experience and a good level of fitness. Walking boots and warm, waterproof clothing To stay in touch with LRWG socials & walks are essential. Terrain As leisurely walks, but with join our Yahoo Group on-line. It’s free, easy to some sustained climbs and perhaps some moderate join up & enables you to arrange or partake in walking on open hillsides or moorland in the warmer ad hoc socials & walks as well as request or months.
    [Show full text]
  • March 2021 Youlgrave, Alport and Middleton Set to Lose out in District Council Boundary Shake-Up
    - 1 - The Bugle A chance to blow your trumpet for the villagers of Alport, Middleton and Youlgrave No. 233 March 2021 Youlgrave, Alport and Middleton set to lose out in District Council boundary shake-up The future of Youlgrave’s distinct and independent representation on the District Council is under threat, following BAKEWELL WARD controversial proposals unveiled by the Boundary Commission. They recommend that Alport Youlgrave should be amalgamated into Youlgrave Bakewell ward, while Middleton Middleton would be absorbed into a new Proposed Boundary changes would see Lathkill & Bradford Bonsall & Winster ward. ward disappear and Youlgrave swallowed up by Bakewell. The electoral review proposes reducing the overall number Bakewell, which will be represented by of Derbyshire Dales District Council three councillors. Meanwhile, Middleton wards from 39 to 34 and is intended to & Smerrill, despite being neighbouring even up the number of voters in each parishes in the same valley, will be put ward. The Commission also says that into Bonsall & Winster ward. ward boundaries should “reflect the Youlgrave has been represented by an interests and identities of local Independent District Councillor for many communities, as well as promoting decades. effective local government”. Youlgrave Parish Council is firmly However, the proposals put out for opposed to the plans, arguing that public consultation recommend that villages like Youlgrave have completely Youlgrave’s Lathkill & Bradford ward is different interests from those of a town abolished and instead Alport and such as Bakewell and need separate Youlgrave will be incorporated into Continued on page 7 - 2 - Missing Element Mortgage Services Ltd We have been helping people financing their homes for 30 years.
    [Show full text]
  • Lathkill Dale
    Hydromorphological Appraisal of the Use of Large Woody Debris in the Restoration of the River Lathkill, Derbyshire John M. E. Cowx & Ian B. Drew Adapted from Gordon et al., 2004 Focus on Hydromorphology – but recognising the link with ecology Raven et al., (2002) - the importance of the physical (hydromorphological) dimension as a supporting element in the ecological restoration of rivers is profound. Chessman et al., (2006) indicate that rehabilitation of geomorphic condition can be critical for the improving the biodiversity. Clarke et al., (2002) argues that both morphological and ecological components of a river system are inherently linked and that ecological goals can only be achieved through geomorphic improvements. Successful river restoration can only be achieved by a multidisciplinary approach, fully understanding ecological, hydrological and geomorphological process and form Lathkill Dale 1 of 5 valleys comprising the Derbyshire Dales National Nature Reserve managed by Natural England Historical channel modification by human intervention 18th and 19th century lead mining was associated with channelisation and the excavation of drainage soughs. Diagrammatic profile through the edge of the Derbyshire plateau, showing a sough cut to drain the limestone for deeper mining access (Ford and Rieuwerts, 2007). Note: contrary to this diagram the sough at Lathkill Dale was driven in below the level of the river. The drainage provided by the sough combined with the permeable limestone geology has causes surface flow to dry up in summer months. Environment Agency daily discharge data for the River Lathkill (1997-2009) (data provided courtesy of Professor John Gunn). The River Lathkill indicating the perennial and intermittent springs.
    [Show full text]
  • Lathkill Dale Fieldwork Activities
    Name: Stop 1- Q3, 4 & 5 Tutor Group: During walk- Q1 Stop 2 – Q7, 8, 9 & 10 Geography Group: Stop 3 – Q2, 6, 11 & 12 Lathkill Dale Activities 1/ During your walk, mark on your map, where the river first appears from the valley sides. Label source of river 2/ For the following 6 photographs (numbered 1 to 6) match them to the letters A-F on the map. Label the letter next to the photo. Photos 3 and 4 have been done. Photo 1 geography.org.uk Photo 2 Photo 3 F geography.org.uk Photo 4 D Photo 5 geography.org.uk Photo 6 geography.org.uk 3/ On your walk, you will see the rocks in the photo below. Use evidence from the map to work out where these rocks have come from a/ deposited by a glacier 20,000 years ago b/ mined material from the caves c/ waste or spoil from Ricklow Quarry geography.org.uk 4/ You will see this place on your walk. What is the arrow on the photograph pointing to? What is this ? a/ a quarry waste slope b/ a scree slope c/ a ski slope 5/ How has the slope in the above photograph formed ? a/ people have tipped waste from the quarry here b/ freeze thaw weathering of the rocks above c/ the soil has been washed away by the rain; leaving these rocks geography.org.uk 6/ This valley was mined for lead in the 19th century. The lead formed 100 million years ago, after the limestone valley had formed.
    [Show full text]
  • Review of Tufa Deposition and Palaeohydrological Conditions in the White Peak, Derbyshire, UK: Implications for Quaternary Landscape Evolution
    CORE Metadata, citation and similar papers at core.ac.uk Provided by NERC Open Research Archive Review of tufa deposition and palaeohydrological conditions in the White Peak, Derbyshire, UK: implications for Quaternary landscape evolution. Vanessa J. Banks1,2*, Peter F. Jones2, David J. Lowe1, Jonathan R. Lee1, Jeremy Rushton1, and Michael A. Ellis1. 1 British Geological Survey, Kingsley Dunham Centre, Nicker Hill, Keyworth, Nottingham NG12 5GG 2 University of Derby, Geographical, Earth and Environmental Sciences, Kedleston Road, Derby, DE22 1GB * Corresponding author. E‐mail address: [email protected] Abstract. This review considers the geological and geomorphological context of tufa barrages that occupy buried valley settings in the Wye catchment, Derbyshire. It describes the potential relationship of the tufa with locations of hypothesised river captures and inception horizon‐guided groundwater flow paths. Tufa barrage development is associated with steps in the bedrock, which may be related to knick‐point recession during river capture. Broad estimates of valley incision have been calculated from previously dated deposits. These support current interpretations of particularly significant effective base‐level lowering during the Anglian and Devensian stages of the Quaternary and have the potential to add to the knowledge of regional uplift histories. Key words: tufa, Quaternary hydrogeology, inception horizons, incision, landscape evolution. 1. Introduction. Tufa is a terrestrial freshwater accumulation of calcium carbonate (Viles, 2004) that is commonly found in limestone terrain. Also referred to as travertine by some authors (Pentecost, 1999), it is precipitated when water that is saturated with calcium carbonate becomes supersaturated due to degassing of carbon dioxide. This can be caused by: atmospheric absorption of carbon dioxide, increase in temperature, decrease in pressure, physical agitation, aquatic plant photosynthesis (Lorah and Herman, 1988), or microbial processes (Pedley and Rogerson, 2010).
    [Show full text]
  • Markerstones for the Millennium Parish of Middleton and Smerrill
    markerstones for the millennium markerstones for the millennium Parish of Middleton and Smerrill CELEBRATING LANDSCAPE - DEVELOPING IDENTITY www.sitesofmeaning.org.uk markerstones for the millennium markerstones for the millennium About Sites of Meaning Sites of Meaning is a millennium project of Middleton and Smerrill in the Derbyshire Peak. It marks the seventeen entrances to its parish with boundary stones each inscribed with a text chosen by members of the parish. A public manifestation of private thoughts and feelings at the start of a new century. Started in 1999 and fi nished in 2006,Sites of Meaning was run by a team of parishioners who raised funds, Middleton by Youlgrave collected text for the inscriptions, commissioned stones from artists and masons, and installed the fi nished boundary markers. Over two hundred people took part in Sites of Meaning, including the local community and primary school, schools and colleges throughout the region, local and national artists and other professionals. At fi rst funding was raised more or less on a stone to stone basis. But as the project gathered momentum and the team gained experience and confi dence, larger funds were sought as projects were designed Longdale to involve more of the surrounding community. The Sculpture Residency in 2002 saw Amanda Wray carve a stone for site 8 in the village playground. Other Stones – Other Meanings explored local history and archaeology, and generated poetry through Youlgrave Primary School. InscribeNOW completed Sites of Meaning with a photographic residency and workshops, the generation of publicity and educational material, and a fi nal celebration re-uniting all those who have worked on Sites of Meaning.
    [Show full text]
  • Derbyshire Dales
    Welcome to Derbyshire Dales The story begins… solidified forming mineral veins. One Nature Reserve of the most common minerals found The rocks in the Reserve were formed within Lathkill dale today is lead ore or Galena (lead sulphide), which has been The Derbyshire Dales National Nature around 350 million years ago when the extensively mined. Reserve is made up of five superb Peak District lay near to the equator, under dales: Lathkill; Cressbrook; Hay; Long; a tropical ocean which supported a vast During the last Ice Age, 20,000 years ago, and Monk’s Dale. Carefully managed array of marine life. Shells, corals and mud the ground in Derbyshire was frozen by Natural England, they form one of built up on the ocean floor in layers, until (known as permafrost). At the end of the Ice England’s finest sites for wildlife and the weight of the sediment compressed Age the ice sheets began to melt, forming geology, providing an opportunity to these layers, eventually forming the fast-flowing rivers which wore away experience nature at its very best. You limestone of the White Peak. Some shells the cracks and fissures in the limestone, can access the dales all year. Come in survived and are preserved today as fossils. creating the deep valleys we see today. early spring to see woodland, wildflowers Since the glaciers have melted, water levels and birds, or in early summer to see the 100 million years ago, volcanic activity across the area have dropped and many internationally-renowned grassland forced hot solutions carrying minerals ancient river valleys are now dry, such as in flowers and insects.
    [Show full text]
  • Bolehill Farm with Woodland on Your Left
    riverbank for a short distance then leaves it to cross the field to a entrance to the left. 52 Towards the top of the valley there is a gate into Holme Lane. 33 Turn left and walk down the lane, with steep little climb by a cave entrance on the left, before you reach glimpses of Holme Hall and its gardens ahead and to your right. a gate into fields at the top of the wood. 53 Walk up the valley then six country walks from 34 At the junction after Holme Grange and before Lumford Cot- go through a squeeze-stile to the left of a gate and walk out to the tages, turn left over Holme Bridge, a narrow packhorse bridge with road, passing to the left of Sheldon’s small water treatment works. cutwaters. 35 On reaching the A6, turn right and follow the near 54 On reaching the road, turn right past Lower Farm on your right pavement for 700 yards, passing the entrance to Riverside Business and Woodbine Farm on your left. 55 At the beginning of the village Park on your right partway along. 36 Just after the entrance to houses, before a barn conversion called “The Byre”, turn left along Deepdale Business Park on your left, go through a gap in the wall a track with a public footpath finger-post. 56 Pass a small stone by a gate on your right and follow the path beyond. 37 This leads barn on the right and follow the wall ahead; climb a stile with a sign via a gate and a narrow path to a road with houses on either side.
    [Show full text]
  • Elcome... to the Derbyshire Dales in the Peak District
    SWIM Hathersage & GYM... erbyshire Get fit and enjoy a swim at the superb state-of-the-art Arc Leisure Centre at Matlock. Or if it’s a nice summer’s day try the lido at Hathersage, an open-air heated pool where you can take a picnic to enjoy after your swim. For opening times and details contact: ales Ashbourne 01335 343712 Matlock 01629 581322 Bakewell 01629 814205 Wirksworth 01629 824717 Hathersage (outdoor) 01433 650843 www.derbyshiredales.gov.uk/leisurecentres Visitor Guide 2015 Find a place to stay… Search for availability and book online at www.visitpeakdistrict.com at a great range of accommodation – from luxury hotels to cosy cottages and away-from-it-all campsites. www.visitpeakdistrict.com www.derbyshiredales.gov.uk Or browse through the Peak District Visitor Guide, available online or from a Visitor Centre. Front cover photos: Parwich village (main) by Karen Frenkel; Longstone well dressing; Cycling on the Monsal Trail; Haddon Hall. Published by Regeneration & Policy, Derbyshire Dales District Council, Town Hall, Matlock, Derbyshire, DE4 3NN E: [email protected] T: 01629 761145 Whilst every effort has been taken compiling this publication and the information it contains, the Council cannot accept responsibility for the services and events shown. Design by pmgd www.paulmcleangraphicdesign.co.uk April 2015 Follow us on Facebook & Twitter @derbyshiredales www.derbyshiredales.gov.uk/tourism elcome...Stanage Edge et back to nature... Woodland walks to the Derbyshire Dales in the Peak District Water, woodland and wildflowers… The name Derbyshire Dales takes its name from the many dales (valleys) often carrying crystal clear Picturesque villages and bustling historic rivers or streams.
    [Show full text]