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Peppercombe, Parkham, Torridge, Devon, England, UKi
Regional Level Types
PeppercombeCliff
ParkhamCivil Parish
TorridgeDistrict
DevonCounty
EnglandConstituent Country
UKCountry

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PhotosMapsSearch
Latitude & Longitude (WGS84):
50° 59' 43'' North , 4° 18' 27'' West
Latitude & Longitude (decimal):
UK National Grid Reference:
SS381243
Type:
Köppen climate type:
Nearest Settlements:
PlacePopulationDistance
Woolfardisworthy783 (2018)5.9km
Bideford28,672 (2018)7.3km
Northam7,668 (2018)7.6km
Appledore2,161 (2018)9.7km
Instow706 (2018)11.1km
Mindat Locality ID:
294151
Long-form identifier:
mindat:1:2:294151:9
GUID (UUID V4):
cc5676ad-fe3b-40f7-a8f8-d01809e62b0b


A cliff line cutting through an outlier of the Permo-Triassic red beds (New Red Sandstone) which lie unconformably on the Carboniferous beds of the Bude Formation, and preserved as two half-graben.

This location yields views of the Peppercombe and Portledge faults, as well as a fine exposure of the Variscan Unconformity which separates the gently-dipping New Red Sandstone form the heavily folded Carboniferous beds below.
The red beds are faulted against the Carbonferous beds at both fault lines.
The hematite-stained cliffs contain a number of interesting features, including calcite-replaced plant fossils; pure, pigment grade, limonite pebbles, occasional mineral crusts and black concretionary nodules associated with iron-reduction patches similar to those of Budleigh Salterton, which are approximately coeval.

The black, concretionary nodules show slightly elevated radioactivity, and a variety of mineral crusts on drying after collection.

The exposure runs for approximately 500m eastward from the beach access path and the wave cut platform may give tantalising glimpses of the red beds at low tide.

This is a public beach with unrestricted access via public footpaths across National Trust land. Both access and walking the beach require some care due to poor footing.

PLEASE NOTE:
The area to the west of Giffard's Jump (the high point adjacent to the Peppercombe fault) and to the north-east of Portledge Mouth (the Portledge Fault) are designated Sites of Special Scientific Interest (SSSI), and collecting/damage to the cliffs is prohibited. The main part of the exposure, however, is not so designated (DEFRA May 2017 - see online references)

Select Mineral List Type

Standard Detailed Gallery Strunz Chemical Elements

Mineral List


5 valid minerals.

Rock Types Recorded

Note: data is currently VERY limited. Please bear with us while we work towards adding this information!

Select Rock List Type

Alphabetical List Tree Diagram

Detailed Mineral List:

Calcite
Formula: CaCO3
Habit: massive, intergrown
Colour: transparent, white, cream, red
Description: Calcite forms the basis of many of the nodules and th rhizo-concretions at this location. May be pseudomorphous after gypsum/anhydrite in places.
Erythrite ?
Formula: Co3(AsO4)2 · 8H2O
Habit: earthy, encrusting
Colour: pink
Description: Minute, pinkish crusts on black nodules after allowing to dry out thoroughly have been tentatively identified as erythrite as being comparable to the material seen on the similar nodules from Budleigh Salterton.
'Limonite'
Habit: massive
Colour: ochre yellow
Description: Well-rounded pebbles of pure sulphide minerals have given rise to pure, pigment grade limonite. Analysis is probably close to pure hydrated Fe(III) hydroxide. The presence of limonite is significant as all other iron oxides have been converted to nano-particles of hematite as part of the deposition process.
Metatyuyamunite ?
Formula: Ca(UO2)2(VO4)2 · 3H2O
Habit: bladed, earthy
Colour: yellow
Description: Seen as minute, yellowish crusts of tiny crystals on the surface of black nodules. Tentatively identified through similarity with the mineral as seen on the Budleigh Salterton nodules.
Metavivianite ?
Formula: Fe2+Fe3+2(PO4)2(OH)2 · 6H2O
Habit: botryoidal, encrusting
Colour: bottle green to greenish-black
Description: Seen as bottle-green to greenish-black encrustations on surfaces and within fractures. Tentatively identified as metavivianite through inference from understood local chemistry and similarity to other occurrances.
Quartz
Formula: SiO2
Habit: Massive, prismatic
Colour: white, yellowish
Description: Many of the clasts comprising the basal conglomerate and subsequent breccias are composed of broken quartz veins. Isolated crystal ponts may occasionally be found in the breccias.

Gallery:

List of minerals arranged by Strunz 10th Edition classification

Group 4 - Oxides and Hydroxides
Quartz4.DA.05SiO2
Metatyuyamunite ?4.HB.25Ca(UO2)2(VO4)2 · 3H2O
Group 5 - Nitrates and Carbonates
Calcite5.AB.05CaCO3
Group 8 - Phosphates, Arsenates and Vanadates
Erythrite ?8.CE.40Co3(AsO4)2 · 8H2O
Metavivianite ?8.DC.25Fe2+Fe3+2(PO4)2(OH)2 · 6H2O
Unclassified
'Limonite'-

List of minerals for each chemical element

HHydrogen
H ErythriteCo3(AsO4)2 · 8H2O
H MetatyuyamuniteCa(UO2)2(VO4)2 · 3H2O
H MetavivianiteFe2+Fe23+(PO4)2(OH)2 · 6H2O
CCarbon
C CalciteCaCO3
OOxygen
O CalciteCaCO3
O ErythriteCo3(AsO4)2 · 8H2O
O MetatyuyamuniteCa(UO2)2(VO4)2 · 3H2O
O MetavivianiteFe2+Fe23+(PO4)2(OH)2 · 6H2O
O QuartzSiO2
SiSilicon
Si QuartzSiO2
PPhosphorus
P MetavivianiteFe2+Fe23+(PO4)2(OH)2 · 6H2O
CaCalcium
Ca CalciteCaCO3
Ca MetatyuyamuniteCa(UO2)2(VO4)2 · 3H2O
VVanadium
V MetatyuyamuniteCa(UO2)2(VO4)2 · 3H2O
FeIron
Fe MetavivianiteFe2+Fe23+(PO4)2(OH)2 · 6H2O
CoCobalt
Co ErythriteCo3(AsO4)2 · 8H2O
AsArsenic
As ErythriteCo3(AsO4)2 · 8H2O
UUranium
U MetatyuyamuniteCa(UO2)2(VO4)2 · 3H2O

Other Regions, Features and Areas containing this locality

British and Irish IslesGroup of Islands
Eurasian PlateTectonic Plate
EuropeContinent
UK

This page contains all mineral locality references listed on mindat.org. This does not claim to be a complete list. If you know of more minerals from this site, please register so you can add to our database. This locality information is for reference purposes only. You should never attempt to visit any sites listed in mindat.org without first ensuring that you have the permission of the land and/or mineral rights holders for access and that you are aware of all safety precautions necessary.

References

 
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