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Warden Point, Warden, Swale, Kent, England, UKi
Regional Level Types
Warden PointCoast
WardenCivil Parish
SwaleNon-metropolitan District
KentCounty
EnglandConstituent Country
UKCountry

This page kindly sponsored by Ricky Mowatt
PhotosMapsSearch
02598270017271998516115.jpg
Clay cliff face and big septarian nodule with Calcite

Warden Point, Warden, Swale, Kent, England, UK
03314270017271998546606.jpg
Ida collecting stuff on the beach

Warden Point, Warden, Swale, Kent, England, UK
02598270017271998516115.jpg
Clay cliff face and big septarian nodule with Calcite

Warden Point, Warden, Swale, Kent, England, UK
03314270017271998546606.jpg
Ida collecting stuff on the beach

Warden Point, Warden, Swale, Kent, England, UK
09514990017271998608813.jpg
Clay cliff face and big septarian nodule with Calcite

Warden Point, Warden, Swale, Kent, England, UK
Latitude & Longitude (WGS84):
51° 24' 50'' North , 0° 54' 23'' East
Latitude & Longitude (decimal):
UK National Grid Reference:
TR021724
Type:
Köppen climate type:
Mindat Locality ID:
1583
Long-form identifier:
mindat:1:2:1583:0
GUID (UUID V4):
0


Warden Point is one of the most important exposures of the Eocene London Clay Formation in the United Kingdom and has been a renowned collecting locality for over two centuries. The site is internationally recognised for its exceptionally preserved fossils, pyritised material, septarian concretions and occurrences of gypsum var. selenite.

The London Clay cliffs at Warden Point are actively eroding, with retreat estimated at approximately 3 metres per year. This continual erosion exposes fresh material onto the foreshore, making the locality exceptionally productive for collectors. However, the same process also makes the site inherently dangerous. Cliff falls are frequent and can occur without warning, and collectors should never work directly beneath unstable cliff faces.

Selenite occurs as individual crystals, crystal groups and classic fishtail (swallowtail) twins. Recent discoveries have demonstrated that Warden Point is capable of producing exceptionally large specimens, including twins exceeding 20 cm in length. Some specimens also exhibit a strong blue fluorescence and visible phosphorescence under short-wave ultraviolet illumination, with certain prismatic twin habits displaying distinct hourglass-shaped growth-sector zoning.
The foreshore is heavily influenced by tidal conditions, and visitors should be aware of tide times, weather conditions and safe exit routes before collecting.

The best crystals are found in boulders which have a brick-red outer colour. Hit with a hammer, the boulder should shatter instantly if the inside contains sizeable cracks. If it doesn't shatter immediately - move on - there will be nothing inside it, and you'll just be wasting your energy.

Select Mineral List Type

Standard Detailed Gallery Strunz Chemical Elements

Mineral List


8 valid minerals.

Rock Types Recorded


Select Rock List Type

Alphabetical List Tree Diagram

Detailed Mineral List:

ⓘ Albite
Formula: Na(AlSi3O8)
ⓘ Baryte
Formula: BaSO4
Habit: Radial crystal groups forming balls of crystal.
Colour: White, transparent, grey
Fluorescence: White LW
Description: Found in cracks in septarian nodules.
ⓘ Calcite
Formula: CaCO3
ⓘ Dolomite
Formula: CaMg(CO3)2
ⓘ Gypsum
Formula: CaSO4 · 2H2O
Fluorescence: Yellow-white in LW, White phosphorescence
ⓘ Gypsum var. Selenite
Formula: CaSO4 · 2H2O
ⓘ 'K Feldspar'
ⓘ 'Mica Group'
ⓘ Natrojarosite
Formula: NaFe3(SO4)2(OH)6
ⓘ Pyrite
Formula: FeS2
ⓘ Quartz
Formula: SiO2
ⓘ 'Smectite Group'
Formula: A0.3D2-3[T4O10]Z2 · nH2O

Gallery:

List of minerals arranged by Strunz 10th Edition classification

Group 2 - Sulphides and Sulfosalts
ⓘPyrite2.EB.05aFeS2
Group 4 - Oxides and Hydroxides
ⓘQuartz4.DA.05SiO2
Group 5 - Nitrates and Carbonates
ⓘCalcite5.AB.05CaCO3
ⓘDolomite5.AB.10CaMg(CO3)2
Group 7 - Sulphates, Chromates, Molybdates and Tungstates
ⓘBaryte7.AD.35BaSO4
ⓘNatrojarosite7.BC.10NaFe3(SO4)2(OH)6
ⓘGypsum7.CD.40CaSO4 · 2H2O
ⓘvar. Selenite7.CD.40CaSO4 · 2H2O
Group 9 - Silicates
ⓘAlbite9.FA.35Na(AlSi3O8)
Unclassified
ⓘ'Mica Group'-
ⓘ'K Feldspar'-
ⓘ'Smectite Group'-A0.3D2-3[T4O10]Z2 · nH2O

List of minerals for each chemical element

HHydrogen
Hⓘ GypsumCaSO4 · 2H2O
Hⓘ NatrojarositeNaFe3(SO4)2(OH)6
Hⓘ Gypsum var. SeleniteCaSO4 · 2H2O
Hⓘ Smectite GroupA0.3D2-3[T4O10]Z2 · nH2O
CCarbon
Cⓘ CalciteCaCO3
Cⓘ DolomiteCaMg(CO3)2
OOxygen
Oⓘ AlbiteNa(AlSi3O8)
Oⓘ BaryteBaSO4
Oⓘ CalciteCaCO3
Oⓘ DolomiteCaMg(CO3)2
Oⓘ GypsumCaSO4 · 2H2O
Oⓘ NatrojarositeNaFe3(SO4)2(OH)6
Oⓘ QuartzSiO2
Oⓘ Gypsum var. SeleniteCaSO4 · 2H2O
Oⓘ Smectite GroupA0.3D2-3[T4O10]Z2 · nH2O
NaSodium
Naⓘ AlbiteNa(AlSi3O8)
Naⓘ NatrojarositeNaFe3(SO4)2(OH)6
MgMagnesium
Mgⓘ DolomiteCaMg(CO3)2
AlAluminium
Alⓘ AlbiteNa(AlSi3O8)
SiSilicon
Siⓘ AlbiteNa(AlSi3O8)
Siⓘ QuartzSiO2
SSulfur
Sⓘ BaryteBaSO4
Sⓘ GypsumCaSO4 · 2H2O
Sⓘ NatrojarositeNaFe3(SO4)2(OH)6
Sⓘ PyriteFeS2
Sⓘ Gypsum var. SeleniteCaSO4 · 2H2O
CaCalcium
Caⓘ CalciteCaCO3
Caⓘ DolomiteCaMg(CO3)2
Caⓘ GypsumCaSO4 · 2H2O
Caⓘ Gypsum var. SeleniteCaSO4 · 2H2O
FeIron
Feⓘ NatrojarositeNaFe3(SO4)2(OH)6
Feⓘ PyriteFeS2
BaBarium
Baⓘ BaryteBaSO4

Other Regions, Features and Areas containing this locality

British and Irish IslesGroup of Islands
Eurasian PlateTectonic Plate
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.

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