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Lode Quarry, Liepa Parish, Cēsis Municipality, Vidzeme Region, Latviai
Regional Level Types
Lode QuarryQuarry
Liepa ParishParish
Cēsis MunicipalityMunicipality
Vidzeme RegionRegion
LatviaCountry

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Latitude & Longitude (WGS84):
57° 23' 30'' North , 25° 24' 22'' East
Latitude & Longitude (decimal):
Type:
Deposit first discovered:
1953
Age:
393.3 ± 1.2 to 382.7 ± 1.6 Ma
Geologic Time:
Nearest Settlements:
PlacePopulationDistance
Priekuļi2,532 (2016)8.9km
Cēsis18,198 (2016)11.9km
Valmiera26,963 (2017)16.7km
Līgatne1,433 (2016)28.1km
Smiltene6,108 (2016)29.9km
Mindat Locality ID:
374238
Long-form identifier:
mindat:1:2:374238:2
GUID (UUID V4):
7871d691-6ba1-4927-9823-4051bba6fa91


Lode (Liepa) Clay Quarry is a Middle Devonian (Gauja suite, Lode Member) clay deposit located in the Liepa Parish territory (Cēsis Municipality). It is the biggest active clay quarry in Latvia. Almost all active clay quarries in the country consist of Quaternary Period rocks, only in the Lode quarry, Devonian clays are mined.

The Lode deposit was discovered in 1953 by the geologist J. Slienis. Ten years later industrial extraction of clay for brick-making was started. The clay-pit became world-famous in 1970 when Latvian geologist V.Kuršs discovered well-preserved fossils of Upper Devonian armoured fish and Strunius kurshi fish for the first time in history. Nowhere else fish fossils in such good condition have been discovered; part of the fossils can be viewed in the Latvian Museum of Natural History. The Lode armoured fish deposit, which is located in the southern part of the quarry is a protected natural monument. Some clay layers of the Gauja suite with rich fossil content are a geological object of world importance.

Nowadays clay is extracted by the company „Lode“ which produces finishing, oven-chimney, and construction bricks, as well as other clay items.

Clay fractions in the quarry rocks mainly consist of illite 80-85% and kaolinite 15-20%. Minor aleurite and sand fractions contain quartz, feldspar, mica (mainly muscovite) and carbonates (dolomite, calcite).

Select Mineral List Type

Standard Detailed Gallery Strunz Chemical Elements

Mineral List


3 valid minerals.

List of minerals arranged by Strunz 10th Edition classification

Group 2 - Sulphides and Sulfosalts
Jordisite2.EA.30MoS2
Group 4 - Oxides and Hydroxides
Goethite4.00.α-Fe3+O(OH)
Group 8 - Phosphates, Arsenates and Vanadates
Hydroxylapatite8.BN.05Ca5(PO4)3(OH)
Unclassified Minerals, Rocks, etc.
'Psilomelane'-

List of minerals for each chemical element

HHydrogen
H HydroxylapatiteCa5(PO4)3(OH)
H Goethiteα-Fe3+O(OH)
OOxygen
O HydroxylapatiteCa5(PO4)3(OH)
O Goethiteα-Fe3+O(OH)
PPhosphorus
P HydroxylapatiteCa5(PO4)3(OH)
SSulfur
S JordisiteMoS2
CaCalcium
Ca HydroxylapatiteCa5(PO4)3(OH)
FeIron
Fe Goethiteα-Fe3+O(OH)
MoMolybdenum
Mo JordisiteMoS2

Other Regions, Features and Areas containing this locality

Eurasian PlateTectonic Plate
EuropeContinent

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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