Where is Shale found?
Shale
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Open the appShale occurs in specific geological environments. Knowing where to look, and in what kind of rock, is the difference between going home empty-handed and finding a great specimen.
Where to find Shale
Appalachian Basin, USA
Extensive shale formations, including the Marcellus Shale and Utica Shale, are significant sources of natural gas.
Western Canada Sedimentary Basin
Contains numerous shale formations, including the Montney and Duvernay shales, important for oil and gas production.
North Sea
Shale formations are common in the sedimentary sequences of the North Sea, often acting as source rocks for petroleum.
Siberian Platform, Russia
Vast shale deposits are found across Siberia, some with significant hydrocarbon potential.
China
Extensive shale gas reserves are present in various basins, particularly in the Sichuan Basin.
Australia
Shale formations are found in several sedimentary basins, including the Cooper Basin and Canning Basin.
Collecting tips
- Look for Fissility. The most distinctive feature of shale is its ability to split into thin, parallel layers. If the rock breaks into blocky fragments, it's more likely a mudstone or claystone.
- Examine Grain Size. Shale is very fine-grained. If you can see individual sand grains, it's likely a sandstone. If it feels gritty but doesn't split easily, it might be siltstone.
- Observe Color Variations. Different colors can indicate different compositions or depositional environments. Black shales often suggest anoxic conditions and high organic content.
- Check for Fossils. Shale, particularly black shale, can be rich in fossils, especially marine organisms, due to the fine-grained nature preserving delicate structures.
- Consider the Geological Context. Shale typically forms in low-energy environments. Look for it in areas that were historically deep marine, lake, or deltaic settings.
Quick Check
- Color:
- Variable (gray, black, green, red, brown)
- Luster:
- Dull to earthy
- Streak:
- White, gray, or color of the rock (if dark)
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