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Lake District historical timeline: Difference between revisions

Timeline from pre-history to present day
Content added Content deleted
(sources inside <small> tags, demolition of holy trinity church)
(glacial events added)
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{{SHORTDESC:Timeline from pre-history to present day}}
{{SHORTDESC:Timeline from pre-history to present day}}
{{Timeline styles}}<div class="plainlinks">
{{Timeline styles}}<div class="plainlinks">
==Last Glacial Period==
{| class="wikitable timeline"
|-
|'''115,000–11,700''' years ago
|Britain enters the {{w1|Last Glacial Period}}, which is part of a much larger sequence of (colder) glacial and (warmer) interglacial periods. The Last Glacial Period is known to British geologists as the Devensian glaciation.
|-
|'''22,000''' years ago
|Britain is at {{w2|Last Glacial Maximum|Glacial Maximum}}, a period of time where the ice sheets are at their greatest extent. These ice sheets cover the majority of Britain and Ireland. Lakeland is covered in its entirety under one huge ice dome. This core is so thick that maybe only the tips of the highest peaks of [[Scafell]], [[Bowfell]], and [[Great Gable]] are visible. All the [[Lakes of the Lake District|big lakes]] are excavated by the ice during this Glacial Maximum.<ref name="smith12">Smith (2012) p.12</ref>
|-
|'''13,500–10,000''' years ago
|▶The ice sheets in lakeland have retreated revealing barren glacial valleys with ice-scoured fells and lakes left impounded in the valley floors.<ref name="smith12"/>
|▶ A catastrophic rock failure causes 1000's of andesite boulders of varying sizes to cascade down from Bowder Crag in the Borrowdale Valley. The largest of these boulders is the famous [[Bowder Stone]], which lands on the lower plateau above the [[River Derwent]] in a blance-defying position on its narrowest point.<ref>Smith (2003) p.21</ref>
|-
|'''11,700''' years ago
|The {{w1|Pleistocene}} geological epoch comes to an end. This marks the beginning of the {{w1|Holocene}} (the current geological epoch) and the period of warming known to British geologists as the {{w1|Flandrian interglacial}}, which continues to present day.<ref>{{w1|Flandian interglacial}}. Wikipedia. Accessed 25 June, 2023.</ref>
|}

==1901–1950==
==1901–1950==
{| class="wikitable timeline"
{| class="wikitable timeline"
|-
|-
|'''1935'''
|'''1935'''
|▶ [[18 August]] – The last service at Holy Trinity Church in [[Mardale Green]], Westmorland, is given by the Rev. W.H. Cormack. The congregation exceeds the church's capacity of 75, and overflows to several thousand outside. Those on church grounds listen via loud speakers, attached to the church tower. The following year the church is demolished, and ancient yew trees are cut down prior to flooding the Mardale Valley for the Manchester Corporation's newly constructed [[Haweswater]] dam and reservoir.<ref>Berry, ''Mardale Revisited'', p.17</ref>
|▶ [[18 August]] – The last service at Holy Trinity Church in [[Mardale Green]], Westmorland, is given by the Rev. W.H. Cormack. The congregation exceeds the church's capacity of 75, and overflows to several thousand outside. Those on church grounds listen via loud speakers, attached to the church tower. The following year the church is demolished, and ancient yew trees are cut down prior to flooding the Mardale Valley for the Manchester Corporation's newly constructed [[Haweswater]] dam and reservoir.<ref>Berry (1984) p.17</ref>
|-
|-
|'''1936'''
|'''1936'''
|Holy Trinity Church is demolished and the bodies of those interred in the churchyard at Holy Trinity are exhumed, most of which are reburied in separate cemetery to the east of St. Michael's Church in Shap.<ref>Berry, ''Mardale Revisited'', p.19</ref>
|Holy Trinity Church is demolished and the bodies of those interred in the churchyard at Holy Trinity are exhumed, most of which are reburied in separate cemetery to the east of St. Michael's Church in Shap.<ref>Berry (1984) p.19</ref>
|-
|-
|'''1945'''
|'''1945'''
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|'''1984'''
|'''1984'''
|▶ A litter pick produces 1,000 sacks of rubbish from the valleys and fells.<ref name="robinson12"/>
|▶ A litter pick produces 1,000 sacks of rubbish from the valleys and fells.<ref name="robinson12"/>
|▶ [[23 July]] – The water level of [[Haweswater]] is over 37 feet below normal, and falling at a consistent rate of around three feet per week. Water is flowing in at less than one million gallons per day, as opposed to 80 million gallons going out. This leaves the distinctive white band of rock and shingle on the shoreline. The remains of the flooded and once picturesque hamlet of [[Mardale Green]] are visible.<ref>Berry, ''Mardale Revisited'', p.9</ref>
|▶ [[23 July]] – The water level of [[Haweswater]] is over 37 feet below normal, and falling at a consistent rate of around three feet per week. Water is flowing in at less than one million gallons per day, as opposed to 80 million gallons going out. This leaves the distinctive white band of rock and shingle on the shoreline. The remains of the flooded and once picturesque hamlet of [[Mardale Green]] are visible.<ref>Berry (1984) p.9</ref>
|}</div>
|}</div>


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==References==
==References==
<small>
{{reflist|25em}}
{{reflist|25em}}
</small>

==Sources==
==Sources==
<small>
<small>
*Berry, Geoffrey (1984). ''Mardale Revisited: The Story of Haweswater''. Kendal: Westmorland Gazette.
*Berry, Geoffrey (1984). ''Mardale Revisited: The Story of Haweswater''. Kendal: Westmorland Gazette.
*Robinson, Jeremy Rowan. ''Managing the Lake District National Park: The first 60 years''. Kendal: Lake District National Park.
*Robinson, Jeremy Rowan. ''Managing the Lake District National Park: The first 60 years''. Kendal: Lake District National Park.
*Smith, Alan (2003). ''The Story of the Bowder Stone''. The Landscapes of Cumbria. Keswick: Rigg Side Publications.
*Smith, Alan (2012). ''The Big Lakes of Lakeland''. The Landscapes of Cumbria No.5. Keswick: Rigg Side Publications
*Smith, Alan (2014). ''The Smaller Lakes and Tarns of Lakeland''. The Landscapes of Cumbria No.6. Keswick: Rigg Side Publications
</small>
</small>
<noinclude>
<noinclude>

Revision as of 17:20, 25 June 2023

1997–to date

(Lake District National Park Authority)

2021 9 May – The Lake District National Park celebrates its 70th anniversary since its original designation. The open spaces and natural beauty of Lakeland are appreciated with increasing enthusiasm due to the restrictions of the Covid-19 Pandemic. Celebrations continue through to August, which marks the National Park Authority's 70 years since it was founded (13 August, 1951). People are invited to mark the anniversary by sharing their favourite Lake District memories on various social media, using #LakeDistrict70 and tagging Lake District National Park. Chief Executive, Richard Leafe says: "This last year has shown us how much people value this protected, national landscape and how important it has been for everyone’s wellbeing," and that this "anniversary is a chance to reflect on highlights from the last seven decades, and to look ahead too."[10]

References

  1. 1.0 1.1 Smith (2012) p.12
  2. Smith (2003) p.21
  3. Flandian interglacial. Wikipedia. Accessed 25 June, 2023.
  4. Berry (1984) p.17
  5. Berry (1984) p.19
  6. Robinson, p.11
  7. 7.0 7.1 7.2 7.3 Robinson, p.12
  8. 8.0 8.1 Robinson, p.13
  9. Berry (1984) p.9
  10. 70 Years of the Lake District National Park Lake District National Park. Accessed 24 June, 2023.

Sources

  • Berry, Geoffrey (1984). Mardale Revisited: The Story of Haweswater. Kendal: Westmorland Gazette.
  • Robinson, Jeremy Rowan. Managing the Lake District National Park: The first 60 years. Kendal: Lake District National Park.
  • Smith, Alan (2003). The Story of the Bowder Stone. The Landscapes of Cumbria. Keswick: Rigg Side Publications.
  • Smith, Alan (2012). The Big Lakes of Lakeland. The Landscapes of Cumbria No.5. Keswick: Rigg Side Publications
  • Smith, Alan (2014). The Smaller Lakes and Tarns of Lakeland. The Landscapes of Cumbria No.6. Keswick: Rigg Side Publications

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