Top 12 Natural Monuments around Rockbeare

The red cliffs are composed of Mercia Mudstone (or Keuper Marl) and Otter Sandstone formations. Age: These rocks date back to the Triassic Period, which was approximately 252 to 201 million years ago. This makes them some of the oldest rocks exposed on this section of the Jurassic Coast. Colour Origin: The colour comes from iron oxides (ferric iron), which effectively rust the sediment. This is a signature of their original environment. Ancient Environment: When these rocks were deposited, Britain was located much closer to the equator and was part of a vast, hot, and dry desert interior. The sediments were laid down in this desert by wind-blown sand dunes and occasional flash floods from ancient river systems.

Gardens offer a superb view along Sidmouth beach. The clock tower within the gardens is perfect for great coffee, yummy cakes and even better sandwiches 😀

Connaught Gardens is a sheltered and in part walled garden of about 1.25 hectares, opened as a public park in 1934 and featuring mixed borders and municipal bedding. Rare and tender plants are also featured. Until the late C18, Sidmouth was a small fishing village at the mouth of the River Sid. In 1792 the lord of the manor, Thomas Jenkins, commissioned the architect Michael Novosielski, who had worked in London as a developer and theatre designer, to build Fortfield Terrace, a seafront crescent which was intended to provide accommodation for fashionable visitors; the scheme was never fully realised (Cherry and Pevsner 1989). By 1796 the Copper Plate Magazine commented that, 'the town is of late tolerably frequented in the bathing season', and a group of cottages ornés was constructed around the edge of the old town in the first two decades of the C19. These cottages were illustrated in Butcher and Haseler's Sidmouth Scenery published in 1816-17, and a collection of lithographs published by Rowe in 1826. A grand public mall 'railed and rolled in very good style' existed adjacent to the beach by 1810 (Cherry and Pevsner 1989), and in 1835-8 The Esplanade was constructed to designs by G H Julian. During the C19 the resort developed slowly, partly constrained by its location between cliffs to east and west and partly by the absence of the railway, which arrived only in 1874. Modest development continued into the early C20, with the resort generally catering for older visitors. In about 1820, Emmanuel Lousada of Peak House, Sidmouth, constructed a detached marine villa known as Cliff Cottage on a headland west of The Esplanade, overlooking Chit Rocks; this headland is shown on a panorama of Sidmouth painted by Hubert Cornish in 1814 (Sidmouth Museum). This house was occupied in the 1830s by the Kent family, who were followed by a succession of private owners, the last, Mr Jemmett, being eccentric and reclusive (Creeke 1992). The property, which from the late C19 was known as Sea View, was placed on the market in 1930; it was bought by Sidmouth Urban District Council for £3500 in order to create public gardens. The house, which was found to be in a dilapidated condition, was demolished, and some of its walls were incorporated into the layout for the public gardens. These were designed by the Gardens Department of Dartington Hall Ltd, which was based at Dartington Hall, Devon (qv). An illustrated publicity brochure published by the Dartington Gardens Department in 1935 (private collection) notes that it was responsible for the design, construction, and planting of the gardens. The gardens were opened on 3 November 1934 by Field Marshal HRH the Duke of Connaught, in whose honour they were named.

Quite the hike up this section after a lot of rainfall. A little tricky in places as the rain has loosened a lot of the earth, so take care going up and especially going down. Definitely the highlight of the walk, just because of the views you get at the trig point.

Ladram Bay is a secluded bay with a pebble beach. Among the most impressive sights along the Jurassic Coast are the sea stacks at Ladram Bay. The sandstones contain many vertical fractures and joints that were formed deep in the Earth's crust during past mountain building periods. The sea picked out these planes of weakness to form caves and natural arches that have since collapsed to produce sea stacks. The “Otter Sandstone” that forms the cliffs and sea stacks were deposited in a hot dry climates in the Triassic Period, about 220 million years ago. The stacks are composed of the same rock, which is relatively soft, but they have a harder band of sandstone at their base which prevents their rapid erosion by the sea. The striking red colour of the rock is caused by iron oxide, which indicate that the layers were formed in a desert. The presence of ripple marks and channels in the sandstones, together with the remains of the long-extinct plants, insects, fish, amphibians and reptiles, show that the desert was crossed by fertile river valleys.

From Sidmouth, it is a good consistent climb up to Peak Hill and it levels off for a bit before a little stairway up to High Peak Trig. Great views or tap and turn around.

Dipped in her for lunch as its nice a sheltered

High Peak is a lot steeper than we would think with lots of rubbly loose rocks so have the right footwear for getting up and down.