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Winterhalter, Boris (1966): Annotated record of the detailed examination of ferromanganese concretions from the Baltic Sea [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.856723, In supplement to: Winterhalter, B (1966): Pohjanlahden ja Suomenlahden rauta-mangaani-saostumista. Summary: Iron-manganese concretions from the gulf of Bothnia and the gulf of Finland. Geoteknillisiä julkaisuja - Geotekniska meddelanden - Geotechnical publications, 69, 77 pp, https://tupa.gtk.fi/julkaisu/geoteknillinen/gt_s_069.pdf

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Coverage:
Median Latitude: 62.957535 * Median Longitude: 21.310302 * South-bound Latitude: 59.583333 * West-bound Longitude: 17.713330 * North-bound Latitude: 65.291670 * East-bound Longitude: 27.391670
Date/Time Start: 1956-01-01T00:00:00 * Date/Time End: 1963-09-07T00:00:00
Minimum DEPTH, sediment/rock: m * Maximum DEPTH, sediment/rock: m
Event(s):
WNT-2A  * Latitude: 60.615000 * Longitude: 19.051670 * Date/Time: 1956-07-07T00:00:00 * Elevation: -60.0 m * Location: Baltic Sea * Method/Device: Dredge (DRG)
WNT-3  * Latitude: 61.570000 * Longitude: 17.816670 * Date/Time: 1956-08-07T00:00:00 * Elevation: -53.0 m * Location: Baltic Sea * Method/Device: Dredge (DRG)
WNT-4  * Latitude: 61.570000 * Longitude: 18.553330 * Date/Time: 1956-08-07T00:00:00 * Elevation: -63.0 m * Location: Baltic Sea * Method/Device: Dredge (DRG)
Comment:
From 1983 until 1989 NOAA-NCEI compiled the NOAA-MMS Marine Minerals Geochemical Database from journal articles, technical reports and unpublished sources from other institutions. At the time it was the most extended data compilation on ferromanganese deposits world wide. Initially published in a proprietary format incompatible with present day standards it was jointly decided by AWI and NOAA to transcribe this legacy data into PANGAEA. This transfer is augmented by a careful checking of the original sources when available and the encoding of ancillary information (sample description, method of analysis...) not present in the NOAA-MMS database.
Parameter(s):
#NameShort NameUnitPrincipal InvestigatorMethod/DeviceComment
Event labelEventWinterhalter, Boris
Date/Time of eventDate/TimeWinterhalter, Boris
Latitude of eventLatitudeWinterhalter, Boris
Longitude of eventLongitudeWinterhalter, Boris
Elevation of eventElevationmWinterhalter, Boris
Sample IDSample IDWinterhalter, Boris
DEPTH, sediment/rockDepth sedmWinterhalter, BorisGeocode
PositionPositionWinterhalter, Boris
Deposit typeDeposit typeWinterhalter, Boris
10 ShapeShapeWinterhalter, Boris
11 Quantity of depositQuantityWinterhalter, Boris
12 SizeSizeWinterhalter, Boris
13 Substrate typeSubstrateWinterhalter, Boris
14 Sediment typeSedimentWinterhalter, Boris
15 CommentCommentGripenberg, Stina
16 DescriptionDescriptionWinterhalter, Boris
17 Uniform resource locator/link to imageURL imageWinterhalter, Boris
Size:
888 data points

Data

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Event

Date/Time

Latitude

Longitude

Elevation [m]

Sample ID

Depth sed [m]

Position

Deposit type
10 
Shape
11 
Quantity
12 
Size
13 
Substrate
14 
Sediment
15 
Comment
16 
Description
17 
URL image
WNT-B5A 1963-0664.316722.6333-58WNT-B5A-10SurfaceFe-Mn noduleFlatSeveralClayThe bottom is a brown muddy clay, with a little of sandy materialFlat concretions almost completely cover the bottom. Their bottom surface is smooth, but the top side is jagged with small botroydal shapes.
WNT-B6 1963-0464.191722.1000-54WNT-B6-10SurfaceFe-Mn noduleRoundSeveralSmallSandA sandy bottom with large stonesSmall round concretions appear on top.
WNT-CI 1963-0564.416722.9167-80WNT-CI-10SurfaceFe-Mn noduleDiscSeveralSandy clayThe bottom is a homogeneous clay, with a pair of centimeters thick sand-rich clay layer at the topOn top appear disc-like flat concretions.
WNT-CIII 1963-0664.700023.0833-74WNT-CIII-10SurfaceFe-Mn noduleRoundSeveralUp to 1.5 cmSandy clayThe bottom is clay, on top of which is a thin sand-sand layerRound concretions, of which the largest diameter is approx. 1,5 cm, are formed in a concentric layers. A second sample at a depth of 82 m contained only round concretions.
WNT-CIII1963-0664.700023.0833-74WNT-CIII-20SurfaceFe-Mn noduleFlatSeveral0.5-1.0 cm thickSandy clayThe bottom is clay, on top of which is a thin sand-sand layerFlat concretions, 0.5-1 cm in thickness.
WNT-CIV-A 1963-0664.850023.1583-78WNT-CIV-A-10SurfaceFe-Mn noduleRoundManyLargeSandy clayThe bottom is brown clay with a cm of sandy material at the topThe haul is rich in large round concretions
WNT-CIV-A1963-0664.850023.1583-78WNT-CIV-A-20SurfaceFe-Mn noduleFlatSeveralFragmentSandy clayThe bottom is brown clay with a cm of sandy material at the topSome fragments of flat concretions.
WNT-CIV-B 1963-0664.850023.1583-65WNT-CIV-B-10SurfaceFe-Mn noduleRoundFewSandy clayThe bottom is brown clay with a cm of sandy material at the topFew round concretions
WNT-CIV-B1963-0664.850023.1583-65WNT-CIV-B-20SurfaceFe-Mn noduleFlatManySandy clayThe bottom is brown clay with a cm of sandy material at the topAbundant flat crusty concretions
WNT-CV 1963-0565.000023.2500-90WNT-CV-10SurfaceFe-Mn noduleRoundManyLargeSandy clayThe bottom is clay with sand at the topA high concentration of large round concretions.
WNT-F10 1963-0664.733321.5500-67WNT-F10-10SurfaceFe-Mn noduleRoundSeveralSmallMuddy clayThe bottom is muddy clay with a few stones. The surface layer contains sand (in oxidizing state)Some small round (grain-like) concretions.
WNT-F10A 1963-0664.900021.6333-60WNT-F10A-10SurfaceFe-Mn noduleDiscSeveralSmallSandy clayThin bluish clay, sandy materialThe top layer contains small disc shaped concretions (in oxidizing state)
WNT-F12A 1963-0664.933322.3000-72WNT-F12A-10SurfaceFe-Mn noduleRoundSeveralSmallClayThe bottom is muddy claySmall round (grain-like) concretions mixed with sandy clay
WNT-F12A1963-0664.933322.3000-72WNT-F12A-20SurfaceFe-Mn noduleDiscFewClayThe bottom is muddy clayIn some places single plate-like concretions. Inside (core) is very dark in color and soft.
WNT-L19 1959-0164.983322.0500-49WNT-L19-10SurfaceFe-Mn noduleRoundSeveralSmallSandSmall grain-like (shot-like) concretions mixed with sand
WNT-L22 1959-0164.825023.1667-80WNT-L22-10SurfaceFe-Mn noduleRoundSeveralClayThe bottom is muddy clayRound concretions
WNT-L221959-0164.825023.1667-80WNT-L22-20SurfaceFe-Mn noduleDiscSeveralClayThe bottom is muddy clayDisc-shaped concretions
WNT-L24 1959-0164.733323.7000-43WNT-L24-10In sedimentFe-Mn noduleSeveralSiltSilty sedimentSilty sediment rich in Fe-Mn precipitates
WNT-L32 1959-0164.850022.9983-80WNT-L32-10SurfaceFe-Mn noduleRoundSeveralClayMuddy clay bottomSignificant number of round concretions
WNT-L34 1959-0164.700022.3417-80WNT-L34-10SurfaceFe-Mn noduleRoundSeveralRound grain-like pellets
WNT-L341959-0164.700022.3417-80WNT-L34-20SurfaceFe-Mn noduleFlatSeveralFlat slabs
WNT-L341959-0164.700022.3417-80WNT-L34-30SurfaceFe-Mn noduleRingSeveralStoneRing aggretations around stones
WNT-L36 1959-0164.513321.6883-36WNT-L36-10SurfaceFe-Mn noduleFlatSeveralClayThe bottom is firm clayPlate-shaped concretions
WNT-L37 1959-0164.475021.8667-80WNT-L37-10SurfaceFe-Mn noduleDiscSeveralBottom almost entirely covered with plate-shaped flat concretions
WNT-P7A 1958-0764.141722.7917-85WNT-P7A-10SurfaceFe-Mn noduleFlatSeveral0.5 thickThe bottom is covered by about half a centimeter thick flat concretions
WNT-P9 1958-0164.633322.9167-79WNT-P9-10SurfaceFe-Mn noduleRoundMany2.5 cmClayPlenty of round concretions (diam. <2.5 cm)
WNT-P91958-0164.633322.9167-79WNT-P9-20SurfaceFe-Mn noduleAgglomerateFewClayAs a rare phenomenon some shells are sometimes sticked together to form larger agglomerates
WNT-P91958-0164.633322.9167-79WNT-P9-30SurfaceFe-Mn noduleDiscSeveralFragmentClayFragments of flat plate-like concretions
WNT-P20 1958-0765.066723.3500-85WNT-P20-10SurfaceFe-Mn noduleRoundManyUp to 2.0 cmClayThe ground is clay, with some sandPlenty of reddish round grain-like (shot-like) concretions, the largest being 2 cm in diameter
WNT-R6A 1963-0664.975023.4667-83WNT-R6A-10SurfaceFe-Mn noduleRoundManySmallSandy clayOn the top of a brown muddy clay, a thin silty and sandy bottom.A large number of small round concretions among the small rocks
WNT-S2 1963-0163.900022.1500-58WNT-S2-10SurfaceFe-Mn noduleDisc1SmallSandSandy bottomA small plate-shaped concretion
WNT-S3 1963-0363.958321.7500-70WNT-S3-10SurfaceFe-Mn noduleFlatManySandy claySandy clay bottomPlenty of irregularly-shaped flatconcretions. Signs of corrosion and regrowth on the concretions.
WNT-S31963-0363.958321.7500-70WNT-S3-20SurfaceFe-Mn noduleRingSeveralStoneSandy claySandy clay bottomRing-shaped concretions
WNT-S4 1963-0364.066721.4417-105WNT-S4-10SurfaceFe-Mn noduleFlatSeveral0.3 cm thickClayMuddy clay bottomFlat, reddish-brown, earthy, approx. 3 mm thick flat concretions (see. fig. 14, p. 37)
WNT-A3 1963-0664.850022.3000-59WNT-A3-10SurfaceFe-Mn noduleFlatSeveralMoraine tillFlat round concretions on moraine bottom
WNT-A31963-0664.850022.3000-59WNT-A3-20SurfaceFe-Mn noduleRingSeveralRockMoraine tillLarge rocks immediately above the bottom level ringed by Fe-Mn precipitate
WNT-A5 1963-0664.875022.4500-66WNT-A5-10SurfaceFe-Mn noduleFlatSeveralThinMoraine tillA thin plate concretion
WNT-A51963-0664.875022.4500-66WNT-A5-20SurfaceFe-Mn noduleRingSeveralFragmentStoneMoraine tillBits and pieces of ore that formed around the stones (ring ore).
WNT-A6 1963-0664.858322.6167-78WNT-A6-10SurfaceFe-Mn noduleDiscSeveral2.0 cm thickGlacigenicGlacial deposit surface has little sand and gravelDisc-shape concretions. The thicker plates (approx. 2 cm) are made primarily of oxihydrates mixed with clay. The concretions are covered with a thin hard crust.
WNT-A7 1963-0664.858322.7833-78WNT-A7-10SurfaceFe-Mn noduleRoundSeveralUp to 2.0 cmSandy clayThe bottom is of brown clay covered with sandy materialPlenty of round concretions. The largest grain-like (shot-like) pellets have a diameter of more than 2 cm.hdl:10013/epic.46576.d005
WNT-A8 1963-0664.850023.0000-80WNT-A8-10SurfaceFe-Mn noduleFlatSeveralFlat concretions sometimes broken with regrowth in concentric rings
WNT-A81963-0664.850023.0000-80WNT-A8-20SurfaceFe-Mn noduleRoundManyLargePlenty of large grain-like (shot-like) concretions.
WNT-A9 1963-0664.858323.2167-91WNT-A9-10SurfaceFe-Mn noduleRoundManyPlenty of round concretions
WNT-A91963-0664.858323.2167-91WNT-A9-20SurfaceFe-Mn noduleDiscFewThinSmall number of thin plate concretions
WNT-A10 1963-0664.975023.4667-83WNT-A10-10SurfaceFe-Mn noduleRingSeveralStoneClayBrown muddy clay with some gravelRing concretions formed around stones
WNT-A101963-0664.975023.4667-83WNT-A10-20SurfaceFe-Mn noduleDisc1ThickClayBrown muddy clay with some gravelA thick plate concretion
WNT-A11 1963-0664.783323.2000-82WNT-A11-10SurfaceFe-Mn noduleFlatSeveralSandBrown sandy bottomMany flat concretions mixed with small gravel.
WNT-A12 1963-0664.675023.1000-70WNT-A12-10SurfaceFe-Mn noduleFlatFewSandThe sample includes a little bit of sand mixed a few flat concretions.
WNT-15A 1956-1263.996722.1917-54WNT-15A-10SurfaceFe-Mn noduleFlatSeveralThinThin flat concretions
WNT-15A1956-1263.996722.1917-54WNT-15A-20SurfaceFe-Mn noduleRingSeveralFragment of concretionSometimes broken pieces of flat concretions are mixed together to form the core of ring concretions
WNT-24 1956-0763.758321.4500-55WNT-24-10SurfaceFe-Mn noduleRingManyRockSandy clayClay mixed with sand bottomPlenty of ring concretions formed around rocks
WNT-241956-0763.758321.4500-55WNT-24-20SurfaceFe-Mn noduleFlatSeveral1.0 cm thickSandy clayClay mixed with sand bottomSeparate flat plates.
WNT-4/61 1961-0165.291723.4333-78WNT-4/61-10SurfaceFe-Mn noduleDiscSeveralLargeClayClay bottom with gravelLarge plate concretions
WNT-9/61 1961-0164.183322.9167-33WNT-9/61-10SurfaceFe-Mn noduleDiscSeveralSandDisc shaped concretions on sand
WNT-14/61 1961-0164.391721.8833-85WNT-14/61-10SurfaceFe-Mn noduleRoundManyUp to 1.5 cmPlenty of round concretions of different sizes ( <1.5 cm)
WNT-14/611961-0164.391721.8833-85WNT-14/61-20SurfaceFe-Mn noduleDiscFewA few small disc-shaped concretions
WNT-2A 1956-0760.615019.0517-60WNT-2A-10SurfaceFe-Mn noduleDiscSeveralClayMainly clay rich plate (disc-shaped) concretions
WNT-3 1956-0861.570017.8167-53WNT-3-10SurfaceFe-Mn noduleSlabSeveralPartly corroded and dissolved plate concretions. Their core is clay. They present a typical layered structure.
WNT-4 1956-0861.570018.5533-63WNT-4-10SurfaceFe-Mn noduleDiscSeveralThinGravelGravle bottomA thin disc-shaped concretion
WNT-5 1956-0762.336719.0917-91WNT-5-10SurfaceFe-Mn noduleRoundManyUp to 0.6 cmAbundance of small (<6 mm) round grain-like (shot-like) concretions
WNT-6 1956-0861.570020.0000-110WNT-6-10SurfaceFe-Mn noduleRoundManyUp to 1.0 cmPlenty of round grain-like (shot-like) concretions of different sizes ( <1 cm). Some concretions have a smooth surface, while others are mamillated.
WNT-8 1956-0161.998321.0633-35WNT-8-10SurfaceFe-Mn noduleDisc1Moraine tillMoraine bottomBetween the rocks a disc-shaped (plate) concretion.
WNT-11A 1956-1062.986720.2100-65WNT-11A-10SurfaceFe-Mn noduleDiscSeveralLargeLarge disc-shaped (plate) concretions with a clayey core covered by a hard Fe-Mn shell a couple of millimeters thick.
WNT-12A 1956-1062.678320.6700-32WNT-12A-10SurfaceFe-Mn noduleSlab1GravelCoarse gravelA corroded disc-shaped (plate) concretion
WNT-28B 1956-0762.723318.6383-88WNT-28B-10SurfaceFe-Mn noduleSlab1LargeGravelLarge, corroded disc-shaped (plate) concretions among the gravel.
WNT-36 1956-0760.983320.0817-116WNT-36-10SurfaceFe-Mn noduleDiscSeveralDisc-shaped (plate) concretions with a clayey core
WNT-17/61 1961-0162.133317.8833-68WNT-17/61-10SurfaceFe-Mn noduleFlatSeveralClayMuddy clay covered with sandRather thin flat concretions.
WNT-19/61 1961-0161.916719.1000-92WNT-19/61-10SurfaceFe-Mn noduleFlatManyLoamSilty loam bottomMany flat concretions.
WNT-23/61 1961-0161.833319.6000-126WNT-23/61-10SurfaceFe-Mn noduleFlatSeveralThinLoamBluish-gray silty loamThin flat concretions.
WNT-BII 1963-0161.466719.8000-98WNT-BII-10SurfaceFe-Mn noduleRoundManySandy clayBluish-gray clay covered by a sandy layer (1-2 cm)Plenty of round grain-like (shot-like) concretions
WNT-BIII 1963-0161.616719.7833-89WNT-BIII-10SurfaceFe-Mn noduleRoundSeveralGlacigenicGlacial deposit type bottom with coarser mineral componentsRound grain-like (shot-like) concretions
WNT-BIV 1963-0161.750019.7500-86WNT-BIV-10SurfaceFe-Mn noduleFlatSeveralLargeGlacigenicGlacial deposit type bottomLarge flat concretions
WNT-BV 1963-0161.900019.7333-81WNT-BV-10SurfaceFe-Mn noduleFewFragmentClayFew fragments of Fe-Mn concretions
WNT-BVI 1963-0161.900019.4167-61WNT-BVI-10SurfaceFe-Mn noduleFewFragmentClayFew fragments of Fe-Mn concretions
WNT-F19A 1963-0162.963319.9167-100WNT-F19A-10SurfaceFe-Mn noduleDiscSeveralSmallA small disc-shaped concretion
WNT-F23-B 1963-0162.650019.5167-125WNT-F23-B-10SurfaceFe-Mn noduleDiscFewLargeA few large disc shaped concretions. Revisiting Gripenberg F23 (1925) Station
WNT-F23-C 1963-0162.650019.5167-130WNT-F23-C-10SurfaceFe-Mn noduleRoundManySandy clayThe bottom is sand mixed with clay. The surface portion holds coarser material, brown (ocher) in color due to oxidizing conditionsA lot of small round grain-like (shot-like) concretions. Revisiting Gripenberg F23 (1925) Station
WNT-F23-C1963-0162.650019.5167-130WNT-F23-C-20SurfaceFe-Mn noduleDiscFewLargeSandy clayThe bottom is sand mixed with clay. The surface portion holds coarser material, brown (ocher) in color due to oxidizing conditionsA few large disc shaped concretions. Revisiting Gripenberg F23 (1925) Station
WNT-F23E 1963-0162.750019.1833-172WNT-F23E-10SurfaceFe-Mn noduleRoundSeveralSmallGlacigenicGlacial deposit type bottomSome small sized grain-like (shot-like) concretions
WNT-L65-A 1959-0162.700019.7167-95WNT-L65-A-10SurfaceFe-Mn noduleFlat1LargeGlacigenicGlacial deposit type bottomA large flat concretion
WNT-L65-B 1959-0162.700019.7167-120WNT-L65-B-10SurfaceFe-Mn noduleManyGlacigenicMany concretions
WNT-L67 1959-0162.566720.1667-83WNT-L67-10SurfaceFe-Mn noduleRoundManyClayMany grain-like (shot-like) concretions
WNT-L68 1959-0162.516720.3000-65WNT-L68-10SurfaceFe-Mn noduleDiscSeveralGlacigenicClay, sand and gravelDisc-shaped concretions
WNT-L70 1959-0162.575019.2833-125WNT-L70-10SurfaceFe-Mn noduleRoundSeveralClayGrain-like (shot-like) round concretions
WNT-L71 1959-0162.608318.7167-98WNT-L71-10SurfaceFe-Mn noduleDiscSeveralLargeClayA little clay materialLarge plate concretions
WNT-L73 1959-0162.633318.2167-98WNT-L73-10SurfaceFe-Mn noduleDiscSeveralLargeClayA little clay materialLarge plate concretions
WNT-L83 1959-0162.000017.8500-67WNT-L83-10SurfaceFe-Mn noduleFewFragmentClayA few pieces of Fe-Mn concretions
WNT-L89 1959-0162.000019.3383-61WNT-L89-10SurfaceFe-Mn noduleFlatFewGlacigenicClay, sand and gravelA few flat concretions
WNT-L91 1959-0162.000020.1417-135WNT-L91-10SurfaceFe-Mn noduleDiscSeveralHard groundRock materialDisc-shaped concretions and rock material.
WNT-L92 1959-0162.000020.5667-85WNT-L92-10SurfaceFe-Mn noduleDiscSeveralClayDisc-shaped concretions
WNT-L95 1959-0161.891721.0583-44WNT-L95-10SurfaceFe-Mn noduleDiscSeveralClayDisc-shaped concretions
WNT-L100 1959-0161.600019.9750-110WNT-L100-10SurfaceFe-Mn noduleRoundManyGlacigenicGlacial deposit type bottomMany grain-like (shot-like) concretions
WNT-L103 1959-0161.600019.0833-53WNT-L103-10SurfaceFe-Mn noduleFlatSeveralClayClay with little gravelFlat concretions
WNT-L110 1959-0161.600017.7133-55WNT-L110-10SurfaceFe-Mn noduleFlatSeveralGlacigenicClay, sand and gravel bottomFlat concretions
WNT-L115 1959-0161.150017.7833-58WNT-L115-10SurfaceFe-Mn noduleFewGlacigenicSand, gravel, clay and rocksSome Fe-Mn concretions
WNT-L154 1959-0161.066719.9417-102WNT-L154-10SurfaceFe-Mn noduleDiscSeveralClayClay and soft gravelDisc-shaped concretions.
WNT-L162 1959-0161.391721.0583-48WNT-L162-10SurfaceFe-Mn noduleDisc1SandIron-rich sandA disc-shaped concretion.
WNT-P4 1959-0162.480020.1917-15WNT-P4-10SurfaceFe-Mn noduleDiscSeveralThe sample contains almost exclusively disc-shaped concretions.
WNT-To3 1963-0560.788320.2117-62WNT-To3-10SurfaceFe-Mn noduleDisc1FragmentA fragment of disc-shaped concretion from an area suspected to be rich of this type of deposit
WNT-A18 1963-0663.241720.9050-19WNT-A18-10SurfaceFe-Mn noduleSlabSeveralUp to 50.0 cmx10.0 cmSandMixed gravel and sandExceptionaly large plate concretions, the largest being 50 cm in length and about 10 cm in thickness. The inner part was generally made of pale and clay or sand with an outer dark brown crust.
WNT-A19 1963-0663.216720.8500-24WNT-A19-10SurfaceFe-Mn noduleSlabSeveralUp to 50.0 cmx10.0 cmSandMixed gravel and sandExceptionaly large plate concretions, the largest being 50 cm in length and about 10 cm in thickness. The inner part was generally made of pale and clay or sand with an outer dark brown crust.
WNT-A22 1963-0663.191720.8167-24WNT-A22-10SurfaceFe-Mn noduleManyClayMuddy clay covered with a thin layer of coarser materialObserved diving behind a large rock and protected from the bottom streams there are many Fe-Mn concretions
WNT-A23 1963-0561.333320.9500-54WNT-A23-10SurfaceFe-Mn noduleDiscSeveralGlacigenicGlacial deposit type bottom with a bit of gravel and stonesDisc-shaped concretions with corroded surface.
WNT-A24B 1963-0561.308321.1417-30WNT-A24B-10SurfaceFe-Mn noduleFlatSeveralSmallGlacigenicGlacial deposit type bottom topped by a little sand, clay and scatteredSmall flat concretions especially downstream from large stones. The observations were carried out by diving.
WNT-N4 1963-0860.136721.2367-30WNT-N4-10SurfaceFe-Mn noduleFlatSeveralGlacigenicGlacial till reworked in sand and gravel without finer materialThe observations were carried out by diving. Flat concretions appearing strongly corroded.
WNT-N1 1963-0460.153325.1783-17WNT-N1-10SurfaceFe-Mn noduleFlatSeveralGlacigenicSand and gravel on a flat bottom with larger rocks in placesFe-Mn concretions do have a distinct flat shape.
WNT-N2 1963-0460.143325.1433-20WNT-N2-10SurfaceFe-Mn noduleRingSeveralGravelSmooth gravel bottom with some rocksThe Fe-Mn deposit forms rings around the small stones.
WNT-N3 1963-0659.795023.1983-20WNT-N3-10SurfaceFe-Mn noduleRingMany2.0-4.0 cm wideGravelSand and gravel bottomCovered at 70% by many ring-shaped concretions. The Fe-Mn deposit ring has a diameter of 2 to 4 cm around small to large stones.hdl:10013/epic.46576.d006
WNT-R/62 1962-0160.431726.9633-18WNT-R/62-10SurfaceFe-Mn noduleRingManyClayThe bottom is covered with a thin layer of clay containing sand and gravelA significant proportion of the surface is covered by Fe-Mn concretions formed as rings around small stones.
WNT-Z705 1963-0959.816724.7500-64WNT-Z705-10SurfaceFe-Mn noduleRoundSeveralGlacigenicBrown glacial deposit type bottom layer topped by a sand layer 0.5-1 cm thick sand-containing layerSmall grain-like (shot-like) round concretions.
WNT-A31 1963-0760.425027.3917-18WNT-A31-10SurfaceFe-Mn noduleRingSeveralThe bottom is covered ring-shaped concretions largely mostly circular. They are similar to those found in Finnish lakes.
WNT-F58A 1963-0159.583322.9667-18WNT-F58A-10SurfaceFe-Mn noduleRoundSeveral0.3 cmRound concretions (grains with diam. 3 mm)
WNT-14RR4 64.883322.8000-74WNT-14RR4-10SurfaceFe-Mn noduleRoundManyRound concretionshdl:10013/epic.46576.d001