Ancient plant root fossils called Rhizoconcretions. These fossils are the preserved remains of plants that grew on the banks of rivers in the Triassic Period, when the area was a desert.
The fossils are mineralised molds and casts of the ancient root systems, and they show that the landscape was once hot and semi-arid. The presence of these fossils, along with some fish and amphibian remains, indicates that the Otter Sandstone dates back to the Middle Triassic

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Best routes to Triassic Fossil Roots at Otter Sandstone Cliffs

4.7

(9)

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1. Orcombe Point & Budleigh Salterton loop from Exmouth

18.3km

04:55

230m

Moderate hike. Good fitness required. Easily-accessible paths. Suitable for all skill levels.

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Moderate

5.0

(1)

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2. Exmouth sea front & Orcombe Point coastal loop from Budleigh Salterton — East Devon

17.8km

04:51

260m

Moderate hike. Good fitness required. Easily-accessible paths. Suitable for all skill levels.

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Moderate

4.8

(61)

371

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3. Otterton Ledge – Otter Estuary Nature Reserve loop from Littleham

28.2km

07:49

470m

Hard hike. Very good fitness required. Easily-accessible paths. Suitable for all skill levels.

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Hard

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Elevation 60 m

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Monday 9 February

10°C

8°C

92 %

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Max wind speed: 35.0 km/h

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Location: Budleigh Salterton, East Devon, Devon, South West England, England, United Kingdom

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Hayeswood Lane Doubletrack

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Triassic Fossil Roots at Otter Sandstone Cliffs

1. Orcombe Point & Budleigh Salterton loop from Exmouth

2. Exmouth sea front & Orcombe Point coastal loop from Budleigh Salterton — East Devon

3. Otterton Ledge – Otter Estuary Nature Reserve loop from Littleham

Other Popular Places to Check Out

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