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Louzeiras de Canelas quarry, Canelas e Espiunca, Arouca, Aveiro, Portugali
| Regional Level Types | |
|---|---|
| Louzeiras de Canelas quarry | Quarry |
| Canelas e Espiunca | Civil Parish |
| Arouca | Municipality |
| Aveiro | District |
| Portugal | Country |
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Latitude & Longitude (WGS84):
40° 57' 44'' North , 8° 12' 56'' West
Latitude & Longitude (decimal):
Type:
Köppen climate type:
Nearest Settlements:
| Place | Population | Distance |
|---|---|---|
| Alpendurada | 8,485 (2018) | 14.3km |
| Rio Mau | 1,407 (2018) | 16.5km |
| Macieira de Cambra | 4,909 (2018) | 17.5km |
| Moreira | 11,336 (2018) | 17.9km |
| Vale de Cambra | 7,649 (2014) | 19.5km |
Other/historical names associated with this locality:
Valério quarry
Name(s) in local language(s):
Louzeiras de Canelas (também conhecida como Pedreira do Valério - Pedreira Nº 5221), Canelase Espiunca, Arouca, Distrito de Aveiro, Portugal
Active slate quarry very rich in fossils: http://www.ardosiasvf.com.pt/en/fosseis.html
"Almost two centuries have gone by since slate was first extracted in Canelas. The tradition of extracting slate has continued in the region, with only brief interruptions, and numerous fossil invertebrates have been found, particularly Trilobites.
The fossil contents of this slate were first studied by Décio Thadeu in 1956. The foundation of the company “Ardósias Valério & Figueiredo, Lda” in 1990 led to exploitation of the slate on an industrial scale, with a view to the production of roofing, flooring, façade coverings, and other materials. Thanks to excavations in “Pedreira do Valério” quarry and the cooperation of its concession company, an extraordinary paleontological collection of international importance has been put together.
Most of the collection, including the specimens of greatest scientific interest, can be found in Canelas and have inspired the creation of the Canelas Geological Interpretation Centre. The aims of this Centre include to organise Paleontological research and to disseminate this heritage in schools and universities and to the general public."
A jazida fossilífera da Pedreira do Valério é internacionalmente reconhecida como uma jazida Konservat-Lagerstätten, pela excepcionalidade da conservação dos fósseis encontrados nas ardósias. Nestes materiais da Formação Valongo, com cerca de 465 milhões de anos (Darriwiliano - Ordovícico Médio) tem sido encontrada uma fauna de invertebrados fósseis constituída por trilobites, bivalves, rostroconchas, gastrópodes, cefalópodes, braquiópodes, crinóides, cistóides, hiolítidos, conulárias, ostracodos, graptólitos e icnofósseis. Entre estes merecem particular destaque as trilobites, correspondendo muitas delas aos maiores exemplares do mundo, tanto em termos genéricos como em termos específicos para diversas espécies.
Este local assume uma importância significativa nos domínios da paleontologia, tafonomia, paleogeografia, paleoecologia, estratigrafia, sedimentologia e tectónica.
In: http://geossitios.progeo.pt/geositecontent.php?menuID=3&geositeID=967
Select Mineral List Type
Standard Detailed Gallery Strunz Chemical ElementsMineral List
3 valid minerals.
Rock Types Recorded
Note: data is currently VERY limited. Please bear with us while we work towards adding this information!
Select Rock List Type
Alphabetical List Tree DiagramDetailed Mineral List:
| ⓘ 'Chlorite Group' |
| ⓘ Muscovite Formula: KAl2(AlSi3O10)(OH)2 |
| ⓘ Muscovite var. Sericite Formula: KAl2(AlSi3O10)(OH)2 |
| ⓘ Pyrite Formula: FeS2 References: |
| ⓘ Quartz Formula: SiO2 |
Gallery:
List of minerals arranged by Strunz 10th Edition classification
| Group 2 - Sulphides and Sulfosalts | |||
|---|---|---|---|
| ⓘ | Pyrite | 2.EB.05a | FeS2 |
| Group 4 - Oxides and Hydroxides | |||
| ⓘ | Quartz | 4.DA.05 | SiO2 |
| Group 9 - Silicates | |||
| ⓘ | Muscovite | 9.EC.15 | KAl2(AlSi3O10)(OH)2 |
| ⓘ | var. Sericite | 9.EC.15 | KAl2(AlSi3O10)(OH)2 |
| Unclassified | |||
| ⓘ | 'Chlorite Group' | - | |
List of minerals for each chemical element
| H | Hydrogen | |
|---|---|---|
| H | ⓘ Muscovite | KAl2(AlSi3O10)(OH)2 |
| H | ⓘ Muscovite var. Sericite | KAl2(AlSi3O10)(OH)2 |
| O | Oxygen | |
| O | ⓘ Muscovite | KAl2(AlSi3O10)(OH)2 |
| O | ⓘ Quartz | SiO2 |
| O | ⓘ Muscovite var. Sericite | KAl2(AlSi3O10)(OH)2 |
| Al | Aluminium | |
| Al | ⓘ Muscovite | KAl2(AlSi3O10)(OH)2 |
| Al | ⓘ Muscovite var. Sericite | KAl2(AlSi3O10)(OH)2 |
| Si | Silicon | |
| Si | ⓘ Muscovite | KAl2(AlSi3O10)(OH)2 |
| Si | ⓘ Quartz | SiO2 |
| Si | ⓘ Muscovite var. Sericite | KAl2(AlSi3O10)(OH)2 |
| S | Sulfur | |
| S | ⓘ Pyrite | FeS2 |
| K | Potassium | |
| K | ⓘ Muscovite | KAl2(AlSi3O10)(OH)2 |
| K | ⓘ Muscovite var. Sericite | KAl2(AlSi3O10)(OH)2 |
| Fe | Iron | |
| Fe | ⓘ Pyrite | FeS2 |
Other Regions, Features and Areas containing this locality
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Louzeiras de Canelas quarry, Canelas e Espiunca, Arouca, Aveiro, Portugal