베레 레지스‬에서 가장 멋진 ‪14‬개의 천연기념물

Bacon Hole is a semi-circular bay located east of Lulworth Cove and slightly west of Mupe Bay. It's often described as a smaller version of Lulworth Cove. Geology: Bacon Hole exposes steeply inclined strata of the Purbeck Group of rocks. The basal Purbeck section, including the Mupe Member (part of the Lulworth Formation), can be seen here. The Purbeck Group is known for its alternating layers of hard limestone and soft mudstone, which have been significantly folded by immense geological pressures. This area also exhibits a conspicuous conglomeratic oil sand. Mupe Rocks are a series of sea stacks and inter-tidal ledges located at the mouth of Bacon Hole, extending eastward into the sea. Formation: These distinctive rock formations are part of the Purbeck Group strata, which are steeply dipping in this area due to significant folding. They are essentially remnants of more resistant rock that have withstood marine erosion.

185 Million Years of Earth's History: The 95-mile stretch of coastline, from Orcombe Point in Exmouth to Old Harry Rocks near Swanage, exposes a continuous sequence of rocks spanning the Triassic, Jurassic, and Cretaceous periods of the Mesozoic Era. This makes it the only place on Earth where such a vast and sequential record of geological time is easily accessible.

This early Iron Age hillfort, taken over by the Romans when they invaded, has double and triple ramparts. The parallel double ramparts on the east and west flanks are connected along the northern border and are unmistakably visible. Because the cliff face acted as defence, it is probable that there were never ramparts along the southern end. Hut circles are visible within the interior of the fort. During a minor excavation in 1939 fragments of Iron Age pottery, as well as sling-stones and bones were found in a pit near the western entrance. Subsequent landslides have revealed the floor of the hillfort. The continual ground disturbances at the southern fringe increase the possibility of further archaeological finds. However, the twin hazards of the cliff erosion and the possibility of unexploded military shells from the Lulworth Ranges command extreme caution.

Worbarrow Bay is a large broad and shallow bay just to the east of Lulworth Cove. The residents of Worbarrow were required to leave their homes in 1943, including the Miller family who had lived at Worbarrow for many generations. Little evidence now remains of the eight cottages and coastguard station (disbanded in 1910) that once stood close to the bay. The area is only accessible when the ranges are closed.

Trig pillar ‘Woolsbarrow Camp’

Once you're at this well-known junction, also known as the Dorsetshire Gap, it doesn't matter which direction you head because the landscape in this area is breathtaking.

The Dorsetshire Gap is a very atmospheric location, very easy to imagine Medieval traders passing through it. Be aware that the bridleways too and from it are tough, the tracks marked on the maps may not exist on the ground, cycling can be hard an slow, Still worth a visit.

Woolsbarrow Hillfort is located in a clearing in the forests of Bloxworth Heath. The nearest town is Bere Regis, about 3+1⁄4 miles (5.2 km) to the west-northwest of the hillfort. The heath is a popular walking area and the site can be reached by public footpath. Woolsbarrow is a slight univallate hillfort on a flat-topped knoll on the plateau of Bloxworth Heath, which separates the rivers Sherford to the east and Piddle to the west. The hillfort is marked by a single rampart about 20 feet (6.1 m) below the top of the gravel knoll and covers an area of around 2+1⁄4 acres (0.91 ha). The eastern part of the hillfort has been damaged by sand and gravel extraction, but much of it survives well and has the potential for further archaeological evidence to be uncovered. It is one of only about 150 slight univallate hillforts nationally and is of national importance.