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Crazy Lace Agate Cut!
Thundereggs?
Chalcedony & Crazy Lace Cut!
Plume w/CrazyLace cut!
Thought it would be three thundereggs!?!?
Plume botryoidal chalcedony nugget!
Plume slice!
Botryoidal slice!
Plume agate inspection!
Plume flow!
Botryoidal Chalcedony Nugget!
Botryoidal Glow!
Square geode!
It's curved!
Botryoidal formations!
Jasper, Chalcedony, Opal & ???
Nodule with crystals!
Chalcedony or Opal!?
Chalcedony!
Carmel Chalcedony Nugget!
Clear/White Banding!
Looking for colors!
Love the orange/yellow!
Some botryoidal goins' on!
One 4 cuttin'!
Green & White Chalcedony!
Chalcedony or Opal?
Botryoidal chalcedony!
White botryoidal chalcedony?
Agate w/Orange Chalcedony!
Smooth Shard!
White Chalcedony Inside!
More Cut White Chalcedony!
Glow Shard!
Nice Glow!
Opal or Chalcedony?
Chalcedony & Jasper!
White/Yellow Chalcedony!
Botryoidal chalcedony!
Yellow & White Chalcedony!
Agate Nodule w/Chalcedony!
Sandwich o' Chalcedony!
Chalcedony Sqared!
Chalcedony Blob!
Pretty Red Jasper!
Beautiful Colors!
Chalcedony?
Chalcedony!
Quartz or Chalcedony!?!?
Chalcedony from a Thunderegg!
Chalcedony!
Chalcedony!
Thought it would be three thundereggs!?!?
Based on the visual characteristics of the rock in the image, it appears to be an iron-rich sedimentary rock, possibly an ironstone or banded iron formation (BIF). Here are some key observations:
Color: The rock has a reddish-brown hue, which is typical of iron oxides like hematite (Fe₂O₃) or goethite (FeO(OH)).
Texture: The rock shows a layered or banded structure with a mix of different shades of red, brown, and some lighter minerals, which suggests it might be a sedimentary rock formed in layers over time.
Luster: The wet appearance gives it a glossy look, which can sometimes help in identifying minerals by enhancing their color and luster.
Composition: The presence of small white or light-colored inclusions could be quartz, calcite, or other minerals commonly found in iron-rich sedimentary environments.
Ironstones are often formed in ancient marine or lake environments where iron was precipitated out of the water and deposited in layers. Banded iron formations are particularly notable for their distinct layers of iron oxides and silica, formed under specific chemical conditions in the Earth's early history.
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