| Locality type: | Quarry |
| Classification |
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| Species: | Calcite |
| Formula: | CaCO3 |
| Confirmation |
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| Validity: | Believed Valid |
| Data |
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| Mineral Data: | Click here to view Calcite data |
| Locality Data: | Click here to view Level 300m, Karikás Hill quarry (Kalapos Hill), Prága Hill, Bazsi, Sümeg District, Veszprém County, Hungary |
| Data Identifiers |
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| Mindat Occurrence Record ID: | 529933 |
| Long-form Identifier: | 1:3:529933:1 |
| GUID (UUID V4): | afc98ae4-0b7c-4f35-90ae-2547391b4104 |
| Nearest other occurrences of Calcite |
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| 0.2km (0.1 miles) | ⓘKarikás Hill quarry (Kalapos Hill), Prága Hill, Bazsi, Sümeg District, Veszprém County, Hungary |
| 1.3km (0.8 miles) | ⓘTátika Hill, Zalaszántó, Keszthely district, Zala County, Hungary |
| 2.2km (1.4 miles) | ⓘSarvaly Hill quarry, Sümeg, Sümeg District, Veszprém County, Hungary |
| 3.5km (2.2 miles) | ⓘHemán-tó Hill, Zalaszántó, Keszthely district, Zala County, Hungary |
| 4.4km (2.7 miles) | ⓘSzántói Hill, Zalaszántó, Keszthely district, Zala County, Hungary |
| 5.2km (3.3 miles) | ⓘLáz Hill mine, Uzsa, Tapolca District, Veszprém County, Hungary |
| 6.8km (4.2 miles) | ⓘKovácsi Hill, Zalaszántó, Keszthely district, Zala County, Hungary |
| 6.9km (4.3 miles) | ⓘVárvölgy quarry, Várvölgy, Keszthely district, Zala County, Hungary |
| 10.3km (6.4 miles) | ⓘNyírespuszta, Nyirád, Ajka District, Veszprém County, Hungary |
| 12.3km (7.6 miles) | ⓘPilikáni Quarry, Keszthely, Keszthely district, Zala County, Hungary |
| References |
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| Reference Search (possible matching items) |
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 | | Book (volume) | | present day, a history of mining activity in the district and suggestions as to localities where the amateur...(1:21 120) map: Engineering geology of the Belfast district Institute of Geological Sciences, London A.... CONTENTS VOLUME ONE Part One Geology of the district 2 6 11 Part Two Chapter1 Introduction Geological...from the air 21 Columnar basalt, Ballynastraid Quarry Spheroidal weathering of basalt 32 Relict spheroids...of Larry Bane Head 106 34 Larry Bane Head and Quarry from the air 35 Boheeshane Bay cliffs from the |  | | Report (chapter) | | at Conoco's Borehole Test Facility (CBTF) in Kay County, Oklahoma. This work was focused on developing...Kay County, north-central Oklahoma, on the Nemeha Ridge, a tectonic feature which, in Kay County, consists...are parallel to fractures mapped in detail in a quarry exposure 5k east-northeast of the CBTF (Fig. 4)...Hinge Elevation °°m Fort Riley-RedEa91e sea level ~ -300m E:oooo lO00m Fig. 3. W N W - E S E section...pattern in the Fort Riley Limestone in an abandoned quarry at Vap's Pass located 5 km east-northeast of the |  | | Journal (article/letter/editorial) | | GoldDeposit:An Examplefromthe MouskaGoldMine, Bousquet District,Canada ABDELHAY BELKABIR AND CLAUDE HUBERT...1990),wellrepresented bydeposits of theBousquet district, consists of both sulfidieand quartzvein orebodies...protoliths, whichare part of the the Bousquet district(Fig. 1). Because of a lesspervasive Dumagamistructural...sulfidiedeposits golddeposits of the Bousquet district(seeEliopoulos, 1983; andthe effectsof reworking...strikenortheast-southwest to east-xvest anddip steeply epidote,calcite,biotite,ehlorite,serieite, magnetite-ilmenite, |  | | Book | | 01242 714600 A GEOLOGY OF IRELAND Gweedore, County Donegal in September, looking towards the ‘Poisoned...Palaeozoic rocks: the coastline of the Burren in County Clare* in Lower Carboniferous limestones, the famed...in Old Red Sandstone; and so on. An exception is County Antrim with its Giant’s Causeway in columnar basalts...stratigraphy Table 1. Geological time scale. Fig. 3. County map of Ireland. Provinces are also indicated. The...the data for Donegal. Fig. 4. Cliffs of Moher, County Clare, looking towards O’Brien’s Tower. These steep |  | | Report (issue) | | siltstones (Zechsteinformatior,). The natural water level was at 135 m below surface. Within this interval...stress direction in the northern part of the Kanto district is ENE-WSW, which is attributed to the interaction...the Kanto district and the west-side of Suruga bay (southeastern part of the Tokai district) is NW-SE...earthquake. The relatively high differential stress level at these two sites may suggest high potential for...Surv. Inst., 1980. Horizontal strain in the Kanto district. Rep. Coordinating Committee Earthq. Predic., |
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