Anagram & Information om | Engelska ordet CLAYSTONE


CLAYSTONE

2

Antal bokstäver

9

Är palindrom

Nej

21
AY
AYS
CL
CLA
LA
LAY

1

1

AC
ACE


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Exempel på hur man kan använda CLAYSTONE i en mening

  • The deposits include siltstone, claystone, sandstone, and lignite coal laid down in a coastal plain during the Laramide orogeny.
  • The summit is formed by the laminated volcaniclastic claystone and siltstone of the Esk Pike Formation overlying the dacitic welded lapilli-tuff of the Lincomb Tarns Formation.
  • Parker from claystone in a marine layer of the Stewartby Member of the Oxford Clay Formation, which dates to the Callovian stage of the Jurassic period, approximately 162 million years ago.
  • The site locality is Dongargaon Hill, which is in a Maastrichtian crevasse splay claystone in the Lameta Formation of India.
  • They, and other tribes before them, created intricate pipes out of the claystone called "Catlinite" in the Buffalo Ridge area, which are displayed at Pipestone National Monument.
  • The Bloomsburg is defined as a grayish-red and greenish-gray claystone, argillaceous siltstone, shale, and very fine to fine-grained sandstone, arranged in fining-upward cycles.
  • Unit V, overlaying Unit IV, consists of a lower grey-to-purple claystone with abundant fist-sized chalcedony and barite concretions; the unit is highly bentonitic and contains occasional channel sands.
  • The municipal area's northwesternmost corner in the Rhaunen State Forest (Sangwald and Jungenwald) is part of a Taunus quartzite block, whose continuation can also be seen in the higher elevations to the west, namely the Sandkopf, the Wildenburger Kopf and the Mörschieder Burr (stratigraphy: Taunus quartzite; petrography: quartz sandstone and quartzitic sandstone with traces of claystone and siltstone).
  • An unconformity occurs before late Miocene sequences including the Dupi Tila sandstone and claystone, with another unconformity between the Dupi Tila units and Pliocene Dihing claysone and silty sandstone.
  • In the northern part of the map area, Sespe Formation is overlain by and inter-fingers with the upper Oligocene to lower Miocene Vaqueros Formation that is composed of transitional and marine sandstone, siltstone, and claystone with local sandy coquina beds.
  • The Deguyños Formation represents the distal prodelta portion of the Colorado River delta, and is characterized by upward-coarsening cycles of claystone, siltstone, sandstone and/or coquina shell beds.
  • This beds are overlain by some metres of arenaceous clays, iron claystone and calcareous sandstone with few intercalation of a coal seam (known as Tågaborg coal seam), where floral remains are also recovered such as Dictyophyllum nilssoni and Equisetites spp.
  • The primary lithology consists of 1 mm thick varve laminations of claystone, with a dark part and a light dolomitic part, which probably correspond to a wet and dry season respectively, alongside rare, several cm thick sandstone interbeds.
  • It is similar to Ashfield Shale in that both have low porosities, though differing in having a greater amount of calcareous, graywacke-type, lithic sandstone bands and lenses, carbonaceous claystone, siltstone, laminite, but would lack sideritic mudstone bands that Ashfield Shale has.
  • The formation is a sequence of dolomite, lacustrine limestones, claystone, evaporites, and fluviatile sandstones.
  • The formation consists of pink to reddish-brown gypsiferous claystone and siltstone; conglomerate; and conglomeratic sandstone.
  • The upper beds contains considerable latite to andesite breccia interbedded with tuffaceous claystone and siltstone.
  • Member B: Light-gray, light-greenish-gray, light-brown, and light-purple, mudstone and claystone with interbeds of greenish-gray, yellow, and brown fine-grained sandstone, and minor conglomerate and tuffaceous beds.
  • The rocks are nonmarine and lagoonal sandstone and claystone, named for exposures along the north side of Mission Valley near Friars Road.
  • Delmar Formation consists of dark green claystone and mudstone, greenish-gray muddy sandstone, interbeds formed by biostromes of shells of molluscs.


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