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United Kingdom
England
South West England
Portreath

Basset's Cove – View of Navax Point loop from Portreath

Routes
Hiking trails & Routes
United Kingdom
England
South West England
Portreath

Basset's Cove – View of Navax Point loop from Portreath

Moderate

4.5

(6)

63

hikers

Basset's Cove – View of Navax Point loop from Portreath

03:08

11.4km

190m

Hiking

Moderate hike. Good fitness required. Easily-accessible paths. Suitable for all skill levels. The starting point of the route is accessible with public transport.

Last updated: April 19, 2026

Tips

Your route passes through protected areas

Please check local regulations for:

Cornwall National Landscape

Waypoints

A

Start point

Bus stop

Get Directions

1

1.26 km

Ralph's Cupboard

Highlight (Segment) • Gorge

To the west of this bay, a rock wall protrudes into the bay and divides it. This wall is the result of long-term erosion, which led to the collapse of a former cave. The name Ralph’s Cupboard comes from a legend that the giant Ralph lived in this bay. This giant attacked the incoming ships and stored the recovered treasures in the cave, his closet.
The eastern side of the bay shows a typical cliff with dark gray shales and greywackes at the lower end and periglacial deposits at the upper part of the cliff.

Translated by Google •

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2

2.01 km

Porthcadjack Cove and Waterfall

Highlight • Waterfall

Lying beneath the striking North Cliffs, Porthcadjack Cove is a little-visited beach on the Cornish coast. Accessible from the Coast Path via a steep and narrow path, the isolated nature of this beach makes it a serene spot and a real hidden gem.

Tip by

3

2.53 km

Basset's Cove Beach

Highlight • Beach

4

2.58 km

Mirrose Well Cove

Highlight (Segment) • Viewpoint

GB: In the lower Mirrose Well Cove one finds deposits with repeated sequences. In each sequence, a gradation of the layers can be observed, with the grain size decreasing from the bottom to the top. In the case of Mirrose Well Cove, coarser greywackes were deposited first, turning into fine greywackes, and followed by clayey layers. Altogether, the deposits reach a thickness of six to ten feet (2-3 m). This type of deposit is caused by turbidites (massive mud flows). To trigger a turbidite, minimal vibrations or the deposition of further sediment grains are enough. The sediments then flow down the slope in a turbulent stream along the water current - a slope inclination of 2-3° is enough here - and spread out into the deep sea in the form of a fan. In this way, sediments with a thickness of several dozens of feet can form within a few hours.

EN: Lower Mirrose Well Cove contains deposits with repeated sequences. In each sequence, a gradation of the layers can be observed, with the grain size decreasing from bottom to top. In the case of Mirrose Well Cove, coarser greywackes were first deposited, which transitioned into fine greywackes, followed by clayey layers. Overall, the deposits reach a thickness of two to three meters. These types of deposits are due to turbidites (powerful turbidity currents). To trigger a turbidite, minimal vibrations or the deposition of further sediment grains are sufficient. The sediments then flow down the slope in a turbulent stream with the water current - here a slope of 2-3° is sufficient - and spread out in the deep sea in the form of a fan. In this way, deposits several tens of meters thick can form within a few hours.

Translated by Google •

Tip by

5

2.97 km

Basset's Cove

Highlight • Natural Monument

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.

Translated by Google •

Tip by

6

4.06 km

View of Navax Point

Highlight • Viewpoint

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

Tip by

7.12 km

Tehidy Wood

Forest

8

7.74 km

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

Tip by

9

9.11 km

Tehidy Country Park

Highlight • Historical Site

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.

Translated by Google •

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B

11.4 km

End point

Bus stop

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Way Types & Surfaces

Way Types

7.09 km

2.13 km

1.27 km

500 m

387 m

Surfaces

6.36 km

2.48 km

1.37 km

923 m

206 m

< 100 m

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Elevation

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Highest point (90 m)

Lowest point (10 m)

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Weather

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Wednesday 8 July

24°C

14°C

0 %

Additional weather tips

Max wind speed: 16.0 km/h

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