Triassic

Anchor Church is a series of caves in a Keuper Sandstone (Triassic conglomerate) outcrop, close to the village of Ingleby, Derbyshire, England.

To the northwest, the watershed dividing the Nive and Bidassoa river basins follows the crest of a Permian-Triassic cuesta in the Baztan region, formed of pink sandstone.

This formation, a thin but fossiliferous succession of dolomite and black shale, is famous for its preservation of Middle Triassic (Anisian-Ladinian) marine life including fish and aquatic reptiles.

Clifton Down Limestone, which includes calcite and dolomitic mudstones of the Carboniferous period, is found in the adjoining central band and dolomitic conglomerate of the Triassic period.

The oldest rocks visible in Devils Tower National Monument were laid down in a shallow sea during the Triassic.

The geology of the area consists of Triassic sandstones and underlying Permian sedimentary rocks.

The Guanling Formation is a Middle Triassic (Anisian or Pelsonian in the regional chronostratigraphy) geologic formation in southwestern China.

The further north and west, towards the Brokenback Range and the Upper Hunter, the more Triassic sandstone that can be found leading eventually to the carboniferous rocks that form the northern boundary of the Hunter with the New England Fold Belt and the foothills of the Barrington Tops.

The Ischigualasto Formation contains Late Triassic (Carnian) deposits (231.4 -225.9 million years before the present), with some of the oldest known dinosaur remains, which are the world's foremost with regards to quality, number and importance.

20 million years between 200 to 180 million years ago) and thus also includes a part of the Triassic.

The Madygen Formation (Russian: Madygen Svita) is a Middle-Late Triassic (Ladinian-Carnian) geologic formation and lagerstätte in the Batken and Osh Regions of western Kyrgyzstan, with minor outcrops in neighboring Tajikistan and Uzbekistan.

The Mercia Mudstone Group is a middle to late Triassic lithostratigraphic group (a sequence of rock strata) which is widespread in Britain, especially in the English Midlands-the name is derived from the ancient kingdom of Mercia which corresponds to that area.

There are relatively small outcrops of Triassic sandstone at Broad Bay near Stornoway.

The desert is composed of stratified layers of siltstone, mudstone, and shale of the Triassic Chinle Formation, which erode easily.

The collision lasted nearly 90 million years in the late Carboniferous, early Triassic.

During the Triassic period, the Provence subsided and was covered by the sea, leaving thick layers of various limestone deposits.

Wingate layers are typically pale orange to red in color, the remnants of wind-born sand dunes deposited approximately 200 million years ago in the Late Triassic.

Mostly Triassic

Triassic