테히디 우드 주변 최고의 워킹 & 하이킹 경로

Breathtaking views. Especially when combined with the blooming heather!

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It's not just the crooked beech tree that's a beautiful photo to behold. The tree a little further away, with its numerous glimpses into its trunk, is also a sight to behold!

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Very nice place to be. Have a delicious coffee with breakfast. Enjoy!

Great coast to coast route across mid Cornwall mainly off road trails and occasional quiet roads. Coffee stops, pub stops, great scenery, mining history and coastal views. There is nothing to dislike about this route.

Naturist beach with views.

Incredibly beautiful ancient beech with super helpful sign with description and history!

Top tier bench would 100% reccomend to friend or foe

Recently reopened under Lands End Coffee Co. Lots of very good cakes

Porthcadjack Cove is an oft missed beauty spot in Cornwall. There is a set of steep steps down to the beach if you have time for an explore and a spot of rock pooling.

Be sure to pause a moment to enjoy this stunning view.

The largest area of woodland in the county, Tehidy Country Park is a peaceful place for a hike, away from the busy crowds in the summer. There is a cafe and keep an eye out for the very friendly squirrels.

Beautiful beach to sit & have an ice cream👍

Portreath marks the start, or finish of the Cornwall coast to coast off road trail. There is an excellent cafe shack run by the Portreath Bakery on the seafront and lots of benches next door so you don't have to worry about getting your bike sandy to sit down with a beautiful sea view. The beach is popular with experienced surfers and families. There are public toilets and a car park closeby. Behind the harbour wall is Portreath Rock Pool, which is an excellent wild swimming spot when the sea is rough or for children. It was created by blowing a hole in the rock to create the pool and then adding a concrete dam. It is swimmable a few hours either side of low tide and is known locally as 'Rocky Pool'.

Portreath is a small village on the Cornish coast with a beautiful sandy beach. It is popular with surfers and families alike and there are plenty of cafes. restaurants and three pubs to cater for all its visitors. Public toilets are available as well as a village shop and post office.

Portreath is a a small coastal village with a very narrow harbour and sandy beach. Rather than fish, this port was used to import Welsh coal and export copper. The original loading ramp can still be seen and given the narrowness of the harbour, navigating it must have been very difficult and dangerous. There are several cafes and shops in Portreath if you are in need of refuelling and/or rehydrating.

Nice cafe on the bottom corner, sea views.

The 7.3 km long circular route takes you back to a time when Cornwall was covered by sea and then became a Europe-wide mountain range. The sedimentary rocks of this area around Portreath were deposited in a deep marine environment during the Devonian age (ca. 393 - 373 million years): Greywacken: Gray rock with fine to coarse grains (0.3 - 2 mm; 0.01 - 0.08 inch), consisting of quartz, feldspars and fragments of foreign rocks. In some cases, shiny/shimmering components can be seen (mica), the rocks form layers and banks. Siltstones: Light gray rock with fine grains (<0.063 mm; <0.002 inch) that are not visible to the naked eye. Layers can be recognized based on the color difference. Slate: Gray to black, sometimes slightly red to greenish colored rocks with very fine grains (<0.02 mm, <0.001 inch), the rocks appear foliated with very thin layers, often alternating with greywackes. The originally horizontal sedimentary layers of Cornwall were tectonically overprinted around 323 - 299 million years ago during the Variscan orogeny (mountain formation). During this time, the southern major continent Gondwana collided with the northern major continents Laurentia and Baltica as well as smaller continent fragments (terranes) such as Avalonia and Amorica. The orogeny ended approximately 270 million years ago with the formation of the supercontinent Pangea. Due to the pressure from the south, the sedimentary rocks were compressed, folded and internally transformed under increasing temperatures. This is how slates emerged from the original claystones. There are no deposits in the area for the period between the formation of the Devonian rocks until 3 million years ago. During the Ice Age 3 million years ago, the region of modern-day Cornwall lay in a tundra area south of the glaciers that covered the Northern Hemisphere. Periglacial deposits from this period can be observed on the cliffs.

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GB: Tehidy is the largest continuous forest area in the region. Many of the mining trails run through the forest. Originally, the park was privately owned by the Basset family, who are closely linked to the mining history. Since 1983, the park has been in government hands and is open to the public. EN: Tehidy is the largest contiguous forest area in the region. Many of the mining trails run through the forest. The park was originally privately owned by the Basset family, which is closely linked to the mining history. The park has been in government hands and open to the public since 1983.

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GB: The small valley with its stream was formed by tectonic processes and following weathering. A small stream cuts into the valley. In contrast to a U valley formed by glaciers, valleys formed by rivers usually show more pointed shapes (V val-ley). This is explained by the fact that the river cuts deeper and deeper into its bed. Flat areas around rivers result from meandering rivers, where the river washes out and away a wider area. These flat areas are called river terraces. At the end of the valley is a zoo with exotic and native animals. EN: The small valley with its stream was created by tectonic processes and subsequent weathering. A small stream cuts into the valley. In contrast to a U-valley formed by glaciers, valleys formed by rivers usually show more pointed shapes (V-valley). This is because the river is cutting deeper and deeper into its bed. Flat areas around rivers result from meandering river courses, where the river erodes and washes away a broader area. These flat areas are called river terraces. At the end of the valley there is a zoo with exotic and native animals.

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GB: In the surrounding area, small walls made of regional rocks, mostly greywackes and clay shales, can be found in several places. The rocks are already described in the geological overview and can be easily distinguished by the following characteristics: Layering/thickness, grain size, sorting, minerals, rock fragments and color. In addition, quartz veins occur in all rocks. These are a form of crystallization of quartz: a hard, transparent to white mineral. EN: In the following area there are small walls made of regional rocks in several places, mostly greywacke and shales. The rocks are already described in the geological overview and can be easily distinguished by the following characteristics: layering/layer thickness, grain size, sorting, minerals, rock fragments and color. In addition, quartz veins occur in all rocks. This is a crystallization form of quartz: a hard, transparent to white mineral.

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