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Natural world · La Société Guernesiaise

The reef that became a cliff-top plateau

Pleinmont, Torteval, Guernsey · 49° 26′ N · 2° 40′ W

A high, surprisingly level headland records an ancient marine erosion surface that local geological interpretation describes as a largely submerged warm-water reef around 10 million years ago.

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CategoryNatural world
DatasetLa Société Guernesiaise
Coordinates49° 26′ N · 2° 40′ W
EvidenceSource linked

Field note

Pleinmont compresses several geological timescales into one walk: ancient metasediments and granite form the headland, later seas planed its upper surface, and much younger coastal erosion cut the cliffs seen today. The published coordinate is a safe trail-access reference on National Trust land, not a fossil collecting point.

Why it is unusual

The place exposes a geological, ecological or atmospheric process in a form that can be read in the landscape.

When to go

April–June and September–October are useful shoulder-season starting points.

JFMAMJJASOND
Green: favourableAmber: check conditionsRed: more challenging

Evidence and practical context

Torteval’s Geology field guide. The dataset supports discovery and context; inspect the original record for its full description, boundaries and status.

Before you go: Conditions and appearance may change seasonally; confirm local restrictions.

Place intelligence v2

What the surrounding data reveals

99Rarity / 99
Oddness / 99
6Oddities within 25 km
11Oddities within 50 km

settlement relative to mapped settlements · access signal: generally accessible · evidence confidence 75/100.

Nearest cross-dataset oddities

Distances are straight-line approximations. Rarity is measured within MapTheOdd’s current catalogue.

MapTheOdd data passport

What this page adds

Nearest mapped settlementTorteval · 1 km
Administrative contextTorteval, Guernsey
Settlement population65,228
TimezoneEurope/Guernsey
Isolation signalWithin a settlement
Page quality100/100 · Indexable

Evidence ledger

This separates source facts, editorial interpretation and computed context so they are not presented as equivalent claims.

CoordinateParsed from the published place recordHigh
Place identityThe reef that became a cliff-top plateauMedium–high
InterpretationPleinmont compresses several geological timescales into one walk: ancient metasediments and granite form the headland, later seas planed its upper surface, and much younger coastal erosion cut the cliffs seen today. The published coordinate is a safe trail-access reference on National Trust land, not a fossil collecting point.Medium
Local contextTorteval, Torteval; 1 km awayComputed
AccessConditions and appearance may change seasonally; confirm local restrictions.Requires live checking

Reuse the record

Download the structured place record, computed geographic context and provenance used by this page. This makes the page inspectable rather than a closed editorial summary.

Generated from source data checked August 2026. Computed relationships are reproducible approximations, not claims about legal access or current operating status.

Corrected and evidence-checked

A record with enough depth to use

Feature typeAncient marine erosion platform
Interpreted marine phaseAbout 10 million years ago
Older bedrockL’Erée granite and Pleinmont metasediment
Coordinate meaningPublished trail-access point
Walking formatCliff-top and headland paths
SamplingDo not collect rock without permission

What is actually here

The unusual feature is not an exposed bed of reef fossils. La Société Guernesiaise describes the level high ground at Torteval as an ancient marine erosion surface: during a period of much higher sea level roughly 10 million years ago, today’s cliff tops were largely submerged and probably formed a warm-water reef. Later uplift, falling sea levels and erosion left that former marine surface high above the modern coast.

The deeper geological story

The landscape is far older than the marine platform. The local field guide places Pleinmont metasediment formation roughly between 1,000 and 700 million years ago and gives an age of about 646 million years for the nearby L’Erée granite. Contacts, dykes and erosion-resistant differences between these rocks help explain the gullies, rock pools, narrow coupfées and offshore reefs visible around the headland.

What to look for

Read the broad, level skyline first: that shape is the large-scale clue to the former marine surface. From the official path, compare pinker granite around La Grosse Rocque with darker metasedimentary cliffs, look for narrow grass-covered rock necks being cut by erosion, and use binoculars for inaccessible exposures. This is landscape interpretation rather than fossil hunting.

Getting there and walking

The National Trust publishes a Pleinmont access reference at 49.434207, -2.664403. Parking is available at Portelet; its guide also lists bus routes 91 and 92. Lower levels are described as mobility and pedestrian friendly, while other coastal trails are hilly. Routes can be extended beyond a mile depending on the chosen loop.

Safety and responsible access

Stay on established headland and cliff paths. La Société warns that steep geological exposures can be dangerous and inaccessible without appropriate equipment. Cliff edges, wet rock, wind and rapidly changing coastal weather require care. Geological interest does not imply permission to collect samples; some Guernsey sites are protected or becoming protected.

Nearby layers worth combining

The same outing can connect geological interpretation with Les Hanois lighthouse views, Pleinmont’s Second World War naval observation tower, the Table des Pions or “Fairy Ring”, National Trust land at Le Vaux de Monel and the wider southwest-coast path network. These overlapping natural, industrial and cultural layers are what make the record useful.

Sources and further checking

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