Scintillating Beauty

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Scintillating Beauty Nature is awesome architecture!!!
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"๐‘๐Ž๐‚๐Š๐’ ๐‘๐„๐Œ๐„๐Œ๐๐„๐‘"

แด›สœษชs แด˜แด€ษขแด‡ แดœแด˜แด…แด€แด›แด‡s ษชแดแด€ษขแด‡s แดา“ sแดแดแด‡ sแด„ษชษดแด›ษชสŸสŸแด€แด›ษชษดษข ษขแด‡แดสŸแดษขษชแด„แด€สŸ สŸแด€ษดแด…า“แดส€แดs แด€ษดแด… า“แด‡แด€แด›แดœส€แด‡s แดแด„แด„แดœส€ษชษดษข แด€สŸสŸ แด€ส€แดแดœษดแด… แด›สœแด‡ ษขสŸแดส™แด‡, แด€สŸแดษดษข แดกษชแด›สœ แดแด‡แด›ษชแด„แดœสŸแดแดœsสŸส ส™ส€ษชแด‡า“แด‡แด… ษขแด‡แดสŸแดษขษชแด„แด€สŸ ษชษดา“แดส€แดแด€แด›ษชแดษด แดา“ แด›สœแด‡ sแด€แดแด‡. โœจโ˜„๏ธ

แด€แด…แด…ษชแด›ษชแดษดแด€สŸสŸส: sแดแดแด‡ ษดแด€แด›แดœส€แด‡'s แด„แด€แด˜แด›แดœส€แด‡ ๐ŸŒฟ It offers us to see it's massive beauty and wonders made by it...Our page ...tries it's best to provide u some best clicks of the moments of the nature.....๏ฟฝ

๐‹๐€๐Œ๐ˆ๐๐€๐“๐„๐ƒ ๐๐‡๐˜๐‹๐‹๐ˆ๐“๐„ ๐Ÿ˜โคโš’๏ธ๐‘๐‰, ๐ˆ๐๐ƒ๐ˆ๐€ ๐Ÿ‡ฎ๐Ÿ‡ณ๐ƒ๐„๐’๐‚๐‘๐: โฌ‡๏ธThis is a photo of carbonaceous phyllite in an outcrop of the Alwar Formati...
07/10/2026

๐‹๐€๐Œ๐ˆ๐๐€๐“๐„๐ƒ ๐๐‡๐˜๐‹๐‹๐ˆ๐“๐„ ๐Ÿ˜โคโš’๏ธ

๐‘๐‰, ๐ˆ๐๐ƒ๐ˆ๐€ ๐Ÿ‡ฎ๐Ÿ‡ณ

๐ƒ๐„๐’๐‚๐‘๐: โฌ‡๏ธ
This is a photo of carbonaceous phyllite in an outcrop of the Alwar Formation taken near Rajgarh, RJ, India ๐Ÿ‡ฎ๐Ÿ‡ณ. It shows the foliation and lamination of the rock in cross-sectional view. It also shows one of the whitish commonly seen on the surface of altered/carbonated phyllite.

๐ƒ๐Ž๐‹๐Ž๐Œ๐ˆ๐“๐„ ๐Ÿ˜โคโš’๏ธ๐‘๐š๐ฃ๐š๐ฌ๐ญ๐ก๐š๐ง, ๐ˆ๐ง๐๐ข๐š ๐Ÿ‡ฎ๐Ÿ‡ณThis photo shows a rolled rockmass of dolomite which is bedded in nature. The aforementi...
05/10/2026

๐ƒ๐Ž๐‹๐Ž๐Œ๐ˆ๐“๐„ ๐Ÿ˜โคโš’๏ธ

๐‘๐š๐ฃ๐š๐ฌ๐ญ๐ก๐š๐ง, ๐ˆ๐ง๐๐ข๐š ๐Ÿ‡ฎ๐Ÿ‡ณ

This photo shows a rolled rockmass of dolomite which is bedded in nature. The aforementioned bedded nature appears due to uneven erosion of the rock comprising materials of alike competency.

๐‰๐€๐’๐๐„๐‘ ๐Š๐๐Ž๐: ๐๐ˆ๐… ๐Ÿ˜โš’๏ธโค๐‰๐š๐ฌ๐ฉ๐ž๐ซ ๐Š๐ง๐จ๐›, ๐ˆ๐ฌ๐ก๐ฉ๐ž๐ฆ๐ข๐ง๐ , ๐”๐’๐€ ๐Ÿ‡บ๐Ÿ‡ธ๐ƒ๐„๐’๐‚๐‘๐ˆ๐๐“๐ˆ๐Ž๐:โฌ‡๏ธThe picture showing a famous BIF unit is the 1.874 or 2...
02/10/2026

๐‰๐€๐’๐๐„๐‘ ๐Š๐๐Ž๐: ๐๐ˆ๐… ๐Ÿ˜โš’๏ธโค

๐‰๐š๐ฌ๐ฉ๐ž๐ซ ๐Š๐ง๐จ๐›, ๐ˆ๐ฌ๐ก๐ฉ๐ž๐ฆ๐ข๐ง๐ , ๐”๐’๐€ ๐Ÿ‡บ๐Ÿ‡ธ

๐ƒ๐„๐’๐‚๐‘๐ˆ๐๐“๐ˆ๐Ž๐:โฌ‡๏ธ
The picture showing a famous BIF unit is the 1.874 or 2.11 billion year old Negaunee Iron-Formation, which outcrops in the Marquette Iron Range of Michiganโ€™s Upper Peninsula (UP), USA.

The Negaunee Fe-Fm. has been metamorphosed to varying degrees and contains many specific lithologies, including jaspilites, taconites, specularites, ferruginous quartzites, ferruginous cherts, and ferruginous slates. The Negaunee Fe-Fm. has economic concentrations of iron and much of the unit in the Marquette Iron Range has been mined away.

The best remaining, easily-accessible outcrop is Jasper K**b in the town of Ishpeming, Michigan. Earthโ€™s oldest known macrofossils, Grypania spiralis, occur in this unit.

๐Ÿ“ท:ยฉ James St. John (via Wikimedia Commons)

๐˜พ๐™ค๐™‡๐™ช๐™ข๐™‰๐™–๐™ ๐˜ฝ๐™–๐™Ž๐™–๐™‡๐™ ๐Ÿ˜โš’๏ธ๐Ÿ’๐—–๐—ผ๐˜‚๐—ป๐˜๐˜† ๐—”๐—ป๐˜๐—ฟ๐—ถ๐—บ, ๐—ก๐—ผ๐—ฟ๐˜๐—ต๐—ฒ๐—ฟ๐—ป ๐—œ๐—ฟ๐—ฒ๐—น๐—ฎ๐—ป๐—ฑ, ๐—จ๐—ž  ๐Ÿ‡ฎ๐Ÿ‡ช๐Ÿ‡ฌ๐Ÿ‡ง55ยฐ 14โ€ฒ 25โ€ณ N, 6ยฐ 30โ€ฒ 37.3โ€ณ W๐˜ฟ๐™€๐™Ž๐˜พ๐™๐™„๐™‹๐™๐™„๐™Š๐™‰: ๐—ง๐—ต๐—ฒ ๐—š๐—ถ๐—ฎ๐—ป๐˜'๐˜€ ๐—–๐—ฎ๐˜‚๐˜€๐—ฒ...
01/10/2026

๐˜พ๐™ค๐™‡๐™ช๐™ข๐™‰๐™–๐™ ๐˜ฝ๐™–๐™Ž๐™–๐™‡๐™ ๐Ÿ˜โš’๏ธ๐Ÿ’

๐—–๐—ผ๐˜‚๐—ป๐˜๐˜† ๐—”๐—ป๐˜๐—ฟ๐—ถ๐—บ, ๐—ก๐—ผ๐—ฟ๐˜๐—ต๐—ฒ๐—ฟ๐—ป ๐—œ๐—ฟ๐—ฒ๐—น๐—ฎ๐—ป๐—ฑ, ๐—จ๐—ž ๐Ÿ‡ฎ๐Ÿ‡ช๐Ÿ‡ฌ๐Ÿ‡ง
55ยฐ 14โ€ฒ 25โ€ณ N, 6ยฐ 30โ€ฒ 37.3โ€ณ W

๐˜ฟ๐™€๐™Ž๐˜พ๐™๐™„๐™‹๐™๐™„๐™Š๐™‰:
๐—ง๐—ต๐—ฒ ๐—š๐—ถ๐—ฎ๐—ป๐˜'๐˜€ ๐—–๐—ฎ๐˜‚๐˜€๐—ฒ๐˜„๐—ฎ๐˜† is ๐—ผ๐—ป๐—ฒ of the ๐—ฏ๐—ฒ๐˜€๐˜ ๐—ฒ๐˜…๐—ฎ๐—บ๐—ฝ๐—น๐—ฒ๐˜€ of ๐—–๐—ผ๐—น๐˜‚๐—บ๐—ป๐—ฎ๐—ฟ ๐—•๐—ฎ๐˜€๐—ฎ๐—น๐˜ in the ๐˜„๐—ผ๐—ฟ๐—น๐—ฑ. The Giantโ€™s ๐—–๐—ฎ๐˜‚๐˜€๐—ฒ๐˜„๐—ฎ๐˜† is made up of ๐˜€๐—ผ๐—บ๐—ฒ ๐Ÿฐ๐Ÿฌ,๐Ÿฌ๐Ÿฌ๐Ÿฌ columns of ๐˜๐—ต๐—ผ๐—น๐—ฒ๐—ถ๐—ถ๐˜๐—ถ๐—ฐ ๐—ฏ๐—ฎ๐˜€๐—ฎ๐—น๐˜ that extend out into the ๐—”๐˜๐—น๐—ฎ๐—ป๐˜๐—ถ๐—ฐ ๐—ข๐—ฐ๐—ฒ๐—ฎ๐—ป like a pavement. The basalt columns at the Giantโ€™s Causeway provided the ๐—ฒ๐˜ƒ๐—ถ๐—ฑ๐—ฒ๐—ป๐—ฐ๐—ฒ to ๐˜€๐˜‚๐—ฝ๐—ฝ๐—ผ๐—ฟ๐˜ the โ€œ๐—ฉ๐˜‚๐—น๐—ฐ๐—ฎ๐—ป๐—ถ๐˜€๐˜โ€ ๐˜๐—ต๐—ฒ๐—ผ๐—ฟ๐˜† for the ๐—ผ๐—ฟ๐—ถ๐—ด๐—ถ๐—ป of ๐—ฒ๐˜…๐˜๐—ฟ๐˜‚๐˜€๐—ถ๐˜ƒ๐—ฒ ๐—ถ๐—ด๐—ป๐—ฒ๐—ผ๐˜‚๐˜€ ๐—ฟ๐—ผ๐—ฐ๐—ธ๐˜€ ๐—ฑ๐—ถ๐˜€๐—ฐ๐—ฎ๐—ฟ๐—ฑ๐—ถ๐—ป๐—ด the "๐—ก๐—ฒ๐—ฝ๐˜๐˜‚๐—ป๐—ถ๐˜€๐˜๐˜€" ๐˜๐—ต๐—ฒ๐—ผ๐—ฟ๐˜† that argued that ๐—ฏ๐—ฎ๐˜€๐—ฎ๐—น๐˜ ๐—ฝ๐—ฟ๐—ฒ๐—ฐ๐—ถ๐—ฝ๐—ถ๐˜๐—ฎ๐˜๐—ฒ๐—ฑ ๐—ณ๐—ฟ๐—ผ๐—บ ๐˜€๐—ฒ๐—ฎ๐˜„๐—ฎ๐˜๐—ฒ๐—ฟ.

๐™‚๐™€๐™Š๐™‡๐™Š๐™‚๐™”:
The ๐—ฝ๐—ฟ๐—ถ๐˜€๐—บ๐—ฎ๐˜๐—ถ๐—ฐ ๐—ฐ๐—ผ๐—น๐˜‚๐—บ๐—ป๐˜€ ๐—ณ๐—ผ๐—ฟ๐—บ๐—ฒ๐—ฑ due to ๐˜€๐—น๐—ผ๐˜„ ๐—ฐ๐—ผ๐—ผ๐—น๐—ถ๐—ป๐—ด of ๐—น๐—ฎ๐˜ƒ๐—ฎ that had ๐—ฝ๐—ผ๐—ป๐—ฑ๐—ฒ๐—ฑ in a ๐—ฝ๐—ฎ๐—น๐—ฒ๐—ผ ๐˜ƒ๐—ฎ๐—น๐—น๐—ฒ๐˜†. The ๐—”๐—ป๐˜๐—ฟ๐—ถ๐—บ ๐—ฏ๐—ฎ๐˜€๐—ฎ๐—น๐˜๐˜€ extend through much of ๐—ป๐—ผ๐—ฟ๐˜๐—ต-๐—ฒ๐—ฎ๐˜€๐˜ ๐—œ๐—ฟ๐—ฒ๐—น๐—ฎ๐—ป๐—ฑ and are the western extent of the ๐—•๐—ฟ๐—ถ๐˜๐—ถ๐˜€๐—ต and ๐—œ๐—ฟ๐—ถ๐˜€๐—ต ๐—œ๐—ด๐—ป๐—ฒ๐—ผ๐˜‚๐˜€ ๐—ฃ๐—ฟ๐—ผ๐˜ƒ๐—ฒ๐—ป๐—ฐ๐—ฒ formed ๐—ฑ๐˜‚๐—ฟ๐—ถ๐—ป๐—ด the ๐—ผ๐—ฝ๐—ฒ๐—ป๐—ถ๐—ป๐—ด of the ๐—ก๐—ผ๐—ฟ๐˜๐—ต ๐—”๐˜๐—น๐—ฎ๐—ป๐˜๐—ถ๐—ฐ ๐—ข๐—ฐ๐—ฒ๐—ฎ๐—ป ๐—ฎ๐—ฝ๐—ฝ๐—ฟ๐—ผ๐˜…๐—ถ๐—บ๐—ฎ๐˜๐—ฒ๐—น๐˜† ๐Ÿฑ๐Ÿฌ ๐—บ๐—ถ๐—น๐—น๐—ถ๐—ผ๐—ป ๐˜†๐—ฒ๐—ฎ๐—ฟ๐˜€ ๐—ฎ๐—ด๐—ผ. ๐——๐—ถ๐˜€๐˜๐—ฟ๐—ถ๐—ฏ๐˜‚๐˜๐—ฒ๐—ฑ within the basalts is a ๐—ฑ๐—ถ๐˜ƒ๐—ฒ๐—ฟ๐˜€๐—ฒ ๐—ฎ๐˜€๐˜€๐—ฒ๐—บ๐—ฏ๐—น๐—ฎ๐—ด๐—ฒ of ๐˜‡๐—ฒ๐—ผ๐—น๐—ถ๐˜๐—ฒ ๐—บ๐—ถ๐—ป๐—ฒ๐—ฟ๐—ฎ๐—น๐˜€ that ๐—ฟ๐—ฒ๐—ณ๐—น๐—ฒ๐—ฐ๐˜๐˜€ a ๐˜๐—ฒ๐—บ๐—ฝ๐—ฒ๐—ฟ๐—ฎ๐˜๐—ฒ ๐—ด๐—ฟ๐—ฎ๐—ฑ๐—ถ๐—ฒ๐—ป๐˜ ๐—ฝ๐—ฟ๐—ฒ๐˜€๐—ฒ๐—ป๐˜ during their ๐—ณ๐—ผ๐—ฟ๐—บ๐—ฎ๐˜๐—ถ๐—ผ๐—ป.

๐—š๐—ฒ๐—ผ๐—น๐—ผ๐—ด๐—ถ๐—ฐ๐—ฎ๐—น ๐—ฃ๐—ฒ๐—ฟ๐—ถ๐—ผ๐—ฑ: Paleogene

๐— ๐—ฎ๐—ถ๐—ป ๐—š๐—ฒ๐—ผ๐—น๐—ผ๐—ด๐—ถ๐—ฐ๐—ฎ๐—น ๐—œ๐—ป๐˜๐—ฒ๐—ฟ๐—ฒ๐˜€๐˜: History of Geoscience & Volcanology

๐—”๐—ฟ๐—ผ๐˜‚๐—ป๐—ฑ ๐Ÿฑ๐Ÿฌ to ๐Ÿฒ๐Ÿฌ ๐—บ๐—ถ๐—น๐—น๐—ถ๐—ผ๐—ป ๐˜†๐—ฒ๐—ฎ๐—ฟ๐˜€ ๐—ฎ๐—ด๐—ผ, during the ๐—ฃ๐—ฎ๐—น๐—ฒ๐—ผ๐—ฐ๐—ฒ๐—ป๐—ฒ ๐—˜๐—ฝ๐—ผ๐—ฐ๐—ต, Antrim was subject to ๐—ถ๐—ป๐˜๐—ฒ๐—ป๐˜€๐—ฒ ๐˜ƒ๐—ผ๐—น๐—ฐ๐—ฎ๐—ป๐—ถ๐—ฐ ๐—ฎ๐—ฐ๐˜๐—ถ๐˜ƒ๐—ถ๐˜๐˜†, when highly fluid ๐—บ๐—ผ๐—น๐˜๐—ฒ๐—ป ๐—ฏ๐—ฎ๐˜€๐—ฎ๐—น๐˜ ๐—ถ๐—ป๐˜๐—ฟ๐˜‚๐—ฑ๐—ฒ๐—ฑ through ๐—ฐ๐—ต๐—ฎ๐—น๐—ธ ๐—ฏ๐—ฒ๐—ฑ๐˜€ to form an ๐—ฒ๐˜…๐˜๐—ฒ๐—ป๐˜€๐—ถ๐˜ƒ๐—ฒ ๐˜ƒ๐—ผ๐—น๐—ฐ๐—ฎ๐—ป๐—ถ๐—ฐ ๐—ฝ๐—น๐—ฎ๐˜๐—ฒ๐—ฎ๐˜‚. As the lava ๐—ฐ๐—ผ๐—ผ๐—น๐—ฒ๐—ฑ, ๐—ฐ๐—ผ๐—ป๐˜๐—ฟ๐—ฎ๐—ฐ๐˜๐—ถ๐—ผ๐—ป occurred. ๐—›๐—ผ๐—ฟ๐—ถ๐˜‡๐—ผ๐—ป๐˜๐—ฎ๐—น ๐—ฐ๐—ผ๐—ป๐˜๐—ฟ๐—ฎ๐—ฐ๐˜๐—ถ๐—ผ๐—ป ๐—ณ๐—ฟ๐—ฎ๐—ฐ๐˜๐˜‚๐—ฟ๐—ฒ๐—ฑ in a similar way to ๐—ฑ๐—ฟ๐˜†๐—ถ๐—ป๐—ด ๐—บ๐˜‚๐—ฑ, with the cracks propagating down as the mass cooled, leaving ๐—ฝ๐—ถ๐—น๐—น๐—ฎ๐—ฟ-๐—น๐—ถ๐—ธ๐—ฒ ๐˜€๐˜๐—ฟ๐˜‚๐—ฐ๐˜๐˜‚๐—ฟ๐—ฒ๐˜€.

๐——๐—ฒ๐—ณ๐—ผ๐—ฟ๐—บ๐—ฎ๐˜๐—ถ๐—ผ๐—ป that ๐—ฎ๐—ฐ๐—ฐ๐—ผ๐—บ๐—ฝ๐—ฎ๐—ป๐—ถ๐—ฒ๐˜€ the ๐—ฐ๐—ผ๐—ผ๐—น๐—ถ๐—ป๐—ด of ๐—ฐ๐—ฒ๐—ฟ๐˜๐—ฎ๐—ถ๐—ป ๐—ฏ๐—ฎ๐˜€๐—ฎ๐—น๐˜ ๐—ณ๐—น๐—ผ๐˜„๐˜€ yields ๐˜€๐—ฝ๐—ฒ๐—ฐ๐˜๐—ฎ๐—ฐ๐˜‚๐—น๐—ฎ๐—ฟ ๐—ฒ๐˜…๐—ฎ๐—บ๐—ฝ๐—น๐—ฒ๐˜€ of "๐˜๐—ต๐—ฒ๐—ฟ๐—บ๐—ฎ๐—น ๐—น๐—ผ๐—ฎ๐—ฑ๐—ถ๐—ป๐—ด". The cooling causes uniform ๐˜€๐—ต๐—ฟ๐—ถ๐—ป๐—ธ๐—ฎ๐—ด๐—ฒ and contraction expressed in columnar jointing of ๐—ต๐—ฒ๐˜…๐—ฎ๐—ด๐—ผ๐—ป๐—ฎ๐—น ๐—ฐ๐—ต๐—ฎ๐—ฟ๐—ฎ๐—ฐ๐˜๐—ฒ๐—ฟ.

๐—ง๐—ต๐—ฒ๐—ฟ๐—บ๐—ฎ๐—น ๐—น๐—ผ๐—ฎ๐—ฑ๐—ถ๐—ป๐—ด is one ๐—ถ๐—ป๐˜๐—ฒ๐—ฟ๐—ฝ๐—ฟ๐—ฒ๐˜๐—ฎ๐˜๐—ถ๐—ผ๐—ป of the ๐—ณ๐—ผ๐—ฟ๐—บ๐—ฎ๐˜๐—ถ๐—ผ๐—ป of ๐—ฐ๐—ผ๐—น๐˜‚๐—บ๐—ป๐—ฎ๐—ฟ basalt at ๐—š๐—ถ๐—ฎ๐—ป๐˜'๐˜€ ๐—ฐ๐—ฎ๐˜‚๐˜€๐—ฒ๐˜„๐—ฎ๐˜†.

๐—œ๐˜€๐—ป'๐˜ ๐˜๐—ต๐—ถ๐˜€ ๐—ด๐—ฒ๐—ผ๐—บ๐—ผ๐—ฟ๐—ฝ๐—ต๐—ผ๐—น๐—ผ๐—ด๐˜†/๐—ด๐—ฒ๐—ผ๐—น๐—ผ๐—ด๐—ถ๐—ฐ๐—ฎ๐—น ๐—น๐—ฎ๐—ป๐—ฑ๐—ณ๐—ผ๐—ฟ๐—บ ๐—ฆ๐—–๐—œ๐—ก๐—ง๐—œ๐—Ÿ๐—Ÿ๐—”๐—ง๐—œ๐—ก๐—š? ๐Ÿ˜๐Ÿคฉ

๐™€๐™ญ๐™–๐™ข๐™ฅ๐™ก๐™š๐™จ:

1. Devils Postpile National Monument (California, USA) ๐Ÿ‡บ๐Ÿ‡ธ
2. Devils Tower National Monument (Wyoming, USA)
3. Fort Davis National Historic Site (Texas, USA)
4. Grand Canyon National Park (Colorado River, USA)
5. John Day Fossil Beds National Monument (Oregon, USA)
6. Shenandoah National Park (Virginia, USA)
7. Coconut Island (Karnataka, INDIA ๐Ÿ‡ฎ๐Ÿ‡ณ)
8. Garni Gorge (ARMENIA ๐Ÿ‡ฆ๐Ÿ‡ฒ)

๐Ÿ“ท:ยฉ David Dixon / Basalt Columns, The Giant's Causeway / CC BY-SA 2.0

Scintillating Beauty

29/09/2026

๐ƒ๐Ž๐‹๐Ž๐Œ๐ˆ๐“๐„ ๐Ÿ˜โคโš’๏ธ

๐‘๐š๐ฃ๐š๐ฌ๐ญ๐ก๐š๐ง, ๐ˆ๐ง๐๐ข๐š ๐Ÿ‡ฎ๐Ÿ‡ณ

This video shows a rolled rockmass of dolomite which is bedded in nature. The aforementioned bedded nature appears due to uneven erosion of the rock comprising materials of alike competency.

๐…๐Ž๐‹๐ƒ โคโš’๏ธ๐Ÿ˜Elvalandet is an island located in Trรธndelag county, Norway. The mica slates and gneisses exposed there were me...
29/09/2026

๐…๐Ž๐‹๐ƒ โคโš’๏ธ๐Ÿ˜

Elvalandet is an island located in Trรธndelag county, Norway. The mica slates and gneisses exposed there were metamorphosed in the amphibolite facies and folded in the Silurian.

๐Ÿ“ท:ยฉ Simon Fuhrmann (distributed via imaggeo.egu.eu)

27/09/2026

Examining a piece of rock found in the field. Leave your geological guesses in the comments below.

๐“๐€๐…๐Ž๐๐ˆ ๐Ÿ˜โคโš’๏ธ๐‘๐š๐›, ๐‚๐ซ๐จ๐š๐ญ๐ข๐š ๐Ÿ‡ญ๐Ÿ‡ท44ยฐ 45โ€ฒ 26.43โ€ณ N, 14ยฐ 45โ€ฒ 28.15โ€ณ EThe photograph showing a eathered sandstone on the promenade...
26/09/2026

๐“๐€๐…๐Ž๐๐ˆ ๐Ÿ˜โคโš’๏ธ

๐‘๐š๐›, ๐‚๐ซ๐จ๐š๐ญ๐ข๐š ๐Ÿ‡ญ๐Ÿ‡ท
44ยฐ 45โ€ฒ 26.43โ€ณ N, 14ยฐ 45โ€ฒ 28.15โ€ณ E

The photograph showing a eathered sandstone on the promenade of park Komrฤar in Rab, Croatia ๐Ÿ‡ญ๐Ÿ‡ท.

Also called Tafoni.

๐Ÿ“ท:ยฉ Isiwal

๐’๐“๐„๐„๐๐‹๐˜ ๐ƒ๐ˆ๐๐๐ˆ๐๐† ๐๐„๐ƒ๐’ ๐Ÿ˜โคโš’๏ธSteeply dipping sedimentary rock strata along the Chalous Road in northern Iran ๐Ÿ‡ฎ๐Ÿ‡ท๐Ÿ“ท:ยฉ Ninara (v...
25/09/2026

๐’๐“๐„๐„๐๐‹๐˜ ๐ƒ๐ˆ๐๐๐ˆ๐๐† ๐๐„๐ƒ๐’ ๐Ÿ˜โคโš’๏ธ

Steeply dipping sedimentary rock strata along the Chalous Road in northern Iran ๐Ÿ‡ฎ๐Ÿ‡ท

๐Ÿ“ท:ยฉ Ninara (via Wikimedia Commons)

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