Everything Totally Explained


Ask & we'll explain, totally!
Seat Sandal
Totally Explained


  NEW! All the latest news in the worlds of computer gaming, entertainment, the environment,  
finance, health, politics, science, stocks & shares, technology and much, much, more.  


View this entry using RSS

Everything about Seat Sandal totally explained

Seat Sandal is a fell in the English Lake District, it's situated four kilometres north of the village of Grasmere from where it's very well seen. Nevertheless, it tends to be overshadowed by its more illustrious neighbours in the Eastern Fells, Helvellyn and Fairfield.

Topography

The fells western flanks above Dunmail Raise are grassy and smooth while its eastern slopes are steep and craggy as they fall away towards Grisedale Hause which at 537 m (1,761 ft) contains Lakeland's highest substantial tarn, Grisedale Tarn. The fell reaches a height of 736 m (2,415 ft) and just scrapes into the list of Marilyns by being given prominence of "around" 150 metres from the higher fell of Fairfield, however this must be a borderline case as there's no Ordnance Survey surveyed height for the top of Grisedale Hause. Alfred Wainwright gives it a height of 1929 feet (588 metres) giving Seat Sandal a topographic prominence of only 148 metres (two metres short of Marilyn qualification). The hills unusual name comes from the Norse language, meaning “Sandulf’s Hill Pasture”, Sandulf being being a Nordic personal name.
   Seat Sandal is distinctive in that its drainage reaches the sea at more widely spread points than any other Lakeland Fell. with Raise Beck going through Thirlmere and Derwent Water to reach the Irish Sea at Workington, Tongue Beck going through Grasmere and Windermere to reach Morecambe Bay and Grisedale Beck draining into Ullswater and then to the sea at the Solway Firth. The fell's main topographic attraction is Gavel Crag on its eastern side, which is connected to the main body of the fell by a fine rock arete.
   Dunmail Raise provides the topographical connection between the Eastern and Central Fells, Steel Fell rising on the other side of the pass.

Geology

A ill of andesite lava forms the summit, the rocks beneath being the dacitic lapilli-tuffs of the Lincomb Tarns Formation.

Ascents

The fell can be ascended from Grasmere or Dunmail Raise although a start from Patterdale is quite feasible. The Grasmere or Patterdale starts use the old packhorse route that links the two places; this is now part of Wainwright’s Coast to Coast Walk. When Grisedale Hause is reached it's a steep climb to the summit following a broken wall. The ascent from Dunmail Raise follows the bed of Raise Beck until it peters out at a height of 580 m (1,900 ft), it's then a walk south up easy slopes to reach the summit.

View

The view from the top is limited by the nearby Helvellyn and Fairfield ranges although there's a good view of Lakeland to the west, the Solway Firth and Criffel are viewed on a good day as is Morecambe Bay to the south.

Further Information

Get more info on 'Seat Sandal'.


External Link Exchanges

Do you know how hard it is to get a link from a large encyclopaedia? Well we're different and will prove it. To get a link from us just add the following HTML to your site on a relevant page:

    <a href="http://seat_sandal.totallyexplained.com">Seat Sandal Totally Explained</a>

Then simply click through this link from your web page. Our crawlers will verify your link, extract the title of your web page and instantly add a link back to it. If you like you can remove the words Totally Explained and embed the link in article text.
   As long as your link remains in place, we'll keep our link to you right here. Please play fair - our crawlers are watching. Your site must be closely related to this one's topic. Any kind of spamming, dubious practises or removing the link will result in your link from us being dropped and, potentially, your whole site being banned.



Copyright © 2007-8 totallyexplained.com | Licensed under the GNU Free Documentation License | Site Map
This article contains text from the Wikipedia article Seat Sandal (History) and is released under the GFDL | RSS Version