周辺のスポット/アトラクション・トップ20

Just to confirm what Ian said above - don't get caught out! Same friendly service, just a new location. Very satisfied with a recent comprehensive service (approaching a refurbishment!) of my gravel bike. Runs like new again.

This is the old location. Kelsall Cycles are now at : Rose Farm, John St, Tarporley CW6 0LP, which is to the south east of the old location.

From English Heritage : “These two massive Saxon stone crosses dominate the cobbled market square of Sandbach. They are elaborately carved with animals and Biblical scenes including the Nativity of Christ and the Crucifixion, and probably date from the 9th century. They were originally painted as well as carved, and they are among the finest surviving examples of Anglo-Saxon high crosses.”

English Heritage says “These two massive Saxon stone crosses dominate the cobbled market square of Sandbach. They are elaborately carved with animals and Biblical scenes including the Nativity of Christ and the Crucifixion, and probably date from the 9th century. They were originally painted as well as carved, and they are among the finest surviving examples of Anglo-Saxon high crosses.”

The plaque says “This is part of the ninth-century cross that was erected in 1578 to mark a charter granting Sandbach a weekly market. This piece survived Protestant extremists' attempts to destroy it and helped inspire the restoration of the crosses in 1810.”

Beeston Castle is a former Royal castle in Beeston, Cheshire, England, perched on a rocky sandstone crag 350 feet above the Cheshire Plain. It was built in the 1220s by Ranulf de Blondeville, 6th Earl of Chester, on his return from the Crusades.

Nestled within captivating surroundings, Winterley Pool emerges as a favoured fishing lake, offering a tranquil haven for both anglers and nature enthusiasts alike. An idea spot to pause and immerse oneself in the breathtaking scenery. Abundant in wildlife, the pool is graced by a resident flock of mute swans.

Blakemere Moss at Delamere Forest is a reclaimed wetland area. The Moss was originally formed from two kettle holes (water filled hollows formed by a detached mass of glacial ice melted in situ towards the end of the last ice age). Delamere Forest is made up of more than 100 peatland basins and includes several sites of rare 'quaking' bogland, a phenomenon in which sphagnum mosses form a carpet above peaty water that appears to tremble when trodden on. The area was drained from the 1800's, supposedly by prisoners from the Napoleonic Wars and planted with trees, (mainly oak and Scot's Pine) between 1793-1815 to provide timber for shipbuilding. The Forestry Commission planted the moss with pine and western hemlock during the 1940s, which proved uneconomic. In the late 1990's the Commission allowed the area to re-flood again naturally.