Conglomerate

The Belogradchik Rocks (Bulgarian: Белоградчишки скали, Belogradchishki skali) are a group of strangely shaped sandstone and conglomerate rock formations located on the western slopes of the Balkan Mountains (Stara Planina) near the town of Belogradchik in northwest Bulgaria.

The 36 domes that make up Kata Tjuṯa / Mount Olga cover an area of 21.68 km2 (8.37 sq mi) are composed of conglomerate, a sedimentary rock consisting of cobbles and boulders of varying rock types including granite and basalt, cemented by a matrix of coarse sandstone.

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.

In this region, the oldest and stratigraphically lowest portion of the Chinle is the Shinarump Conglomerate.

Ukhaa Tolgod (also spelled Oka Tolga): The strata exposed at Ukhaa Tolgod is dominated by reddish sandstones, with some sandstones containing small amounts of conglomeratic lenses and/or cobbles and pebbles. Conglomerate itself is in this site, and to a lesser level are mudstones and siltstones, which are thin and laterally restricted.

Formation of graywacke-argillite-conglomerate, the Drake Icefall Formation of black shales and marble, the Conglomerate Ridge Formation of conglomerate and quartzite, the Liberty Hills-Springer Peak-Frazier Ridge Formations of quartzite-argillite, and the Minaret Formation of

The rocks of the Guiana Shield consist of metasediments and metavolcanics (greenstones) overlain by sub-horizontal layers of sandstones, quartzites, shales and conglomerates intruded by sills of younger mafic intrusives such as gabbros.

The formations consist of red-brown sedimentary conglomerate, sandstone, and minor mudstone rock from the Carboniferous Hopewell Cape Formation, part of the Mabou Group.

It was established in 1975 with a purpose of conservation of a unique geological formation, sheer cliffs composed of Tertiary red conglomerates.

The valley is situated between the Silurian Shawangunk quartz conglomerate and the lower Cambrian Hardyston quartzite.

However, they are not like the typical volcanic plugs of igneous rock found elsewhere, as they are composed of a mixture of sandstone and conglomerate.

The lowest layer is the Organ Rock Shale, the middle is de Chelly Sandstone, and the top layer is the Moenkopi Formation capped by Shinarump Conglomerate.

Mount of Danxia is identified by multi-layered red sedimentary rocks of sandstone and conglomerate, and the area of was formed by the fluvial deposition through the basin 140-65 million years ago.

Its predominantly composed of sedimentary materials such as sandstones, clays and conglomerates.

The Santa Clarita Valley is underlain by Quaternary alluvial deposits and coarse-grained Pleistocene age conglomerates dominated by sandstone of marine and non-marine origin.