[caption id="attachment_175" align="alignleft" width="145" caption="Quality Business"][/caption] EastDevon.co.uk is built and operated by Westcountry Online who are accredited as a Jurassic Coast Quality Business. This award is given for successfully completing the Jurassic Coast Quality Business Scheme and demonstrating high standards of operation and a commitment to the values of the Jurassic Coast World Heritage Site.
[caption id="attachment_158" align="alignleft" width="150" caption="Seaton Tram"][/caption] Seaton is a quiet seaside holiday town that nestles one side of the mouth of the river Axe whilst on the other side of the river is Axmouth. Seaton's cliffs form part of the UNESCO World Heritage Site called the Jurassic Coast which is the pride of English Tourism and a major element in the success of the Tourism Industry along the East Devon Coast. Seaton has good road links sitting half wat between Sidmouth to the west and world famous Lyme Regis to the East. The town also boasts one of the UK's few working Tram ...
[caption id="attachment_154" align="alignleft" width="150" caption="Sidmouth"][/caption] Sidmouth is a Gateway Town to the World Heritage Site which most of us know as the Jurassic Coast even though the rocks and cliffs around Sidmouth are from the Triassic Period. Sidmouth has an excellent tourist trade and is the destination of many family holidays for many people. Lying in a geren valley with good road transport links, it has a wonderful pebble beach and plenty of rock pools for the children to explore too.
[caption id="attachment_149" align="alignleft" width="150" caption="Budleigh Salterton"][/caption] Budleigh Salterton is a small seaside village just to the East of Exmouth and has a long pebbly beach with ample parking for visitors and plenty of places to stay if you want to relax for longer. Behind the beach in areas there's the cliffs which form part of the world heritage site called the Jurassic Coast, however, the cliffs at Budleigh Salterton have pebble beds which were formed by pebbles deposited by a huge river that flowed northwards through the Triassic desert during the Triassic Period.