Locality type: | Quarry |
Classification |
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Species: | Baryte |
Formula: | BaSO4 |
Confirmation |
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Validity: | Believed Valid |
Data |
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Mineral Data: | Click here to view Baryte data |
Locality Data: | Click here to view Point 8.0, Borstein, Reichenbach, Lautertal (Odenwald), Bergstraße, Darmstadt, Hesse, Germany |
Data Identifiers |
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Mindat Occurrence Record ID: | 165084 |
Long-form Identifier: | 1:3:165084:6 |
GUID (UUID V4): | 32c21404-a94e-43a9-85ff-c7365d80de3d |
Nearest other occurrences of Baryte |
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0.1km (0.1 miles) | ⓘPoint 9.0, Borstein, Reichenbach, Lautertal (Odenwald), Bergstraße, Darmstadt, Hesse, Germany |
0.4km (0.2 miles) | ⓘPoint 5.0, Borstein, Reichenbach, Lautertal (Odenwald), Bergstraße, Darmstadt, Hesse, Germany |
0.6km (0.4 miles) | ⓘPoint 3.0, Borstein, Reichenbach, Lautertal (Odenwald), Bergstraße, Darmstadt, Hesse, Germany |
0.9km (0.6 miles) | ⓘPoint 2.0, Teufelsstein, Reichenbach, Lautertal (Odenwald), Bergstraße, Darmstadt, Hesse, Germany |
1.6km (1.0 miles) | ⓘBangertshöhe, Hochstädten, Bensheim, Bergstraße, Darmstadt, Hesse, Germany |
1.7km (1.1 miles) | ⓘSeemann quarry, Hochstädten, Bensheim, Bergstraße, Darmstadt, Hesse, Germany |
1.8km (1.1 miles) | ⓘPoint 14.0, Hohenstein, Reichenbach, Lautertal (Odenwald), Bergstraße, Darmstadt, Hesse, Germany |
2.5km (1.5 miles) | ⓘLinck marble works, Auerbach, Bensheim, Bergstraße, Darmstadt, Hesse, Germany |
3.2km (2.0 miles) | ⓘPoint 20.0, Katzenstein, Raidelbach, Lautertal (Odenwald), Bergstraße, Darmstadt, Hesse, Germany |
3.7km (2.3 miles) | ⓘBergweg, Gadernheim, Lautertal (Odenwald), Bergstraße, Darmstadt, Hesse, Germany |
References |
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Reference Search (possible matching items) |
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| | Book | veins in Westphalian strata of the Ruhr, West Germany. W. K/au 693 BIOGRAPHICAL NOTES 701 LOCALITY...represented in the Limerick Province by the Ballymartin Point Formation, a name which replaces the lower division... Within the Limerick Province, the Ballymartin Point Formation is succeeded by the Ballysteen Limestone...widely in the north Midlands west of Navan. The same point can be illustrated by comparing the high sandstone...transcurrent movement at Silvermines. The important point to stress is that the termination of even small |
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