Anagram & Information om | Engelska ordet SCHIST

Exempel på hur man kan använda SCHIST i en mening

• Bolton was known for its high quality schist stone in the 18th century, and many tombstone carvers such as Gershom Bartlett and Jonathan Loomis sourced their stone from Bolton quarries.
• These cliffs are mostly made of schist, with some being granite, and vary from long smooth slabs to wildly overhung roofs and aretes.
• Rocks are mostly of the calciferous mica schist, except in the southeastern part, where they are granite.
• Along a path toward the southeast, a plaque on a low glaciated outcropping of schist lists the nations which contributed to building the memorial.
• The coticule is a metamorphic microcristalin schist, very fine grained, 35 to 40% of it small crystals of spessartine, of about 5 to 20 μm in diameter.
• These were carved from a micaceous schist (soapstone) on the tops of monoliths the height of a person.
• The lowest strata of the Spessart are made up of gneiss and mica schist, dating back around 1,200 million years.
• Mount Mitchell was formed during the Precambrian when marine deposits were metamorphosed into gneiss and schist.
• Other exploited sites includes the schist quarries at Wadi Hammamat, amethyst from Wadi el-Hudi, fine limestone from Tura, alabaster from Hatnub, red granite from Aswan, and diorite from Nubia.
• Next is a narrow range of Upper Helderberg limestone, followed by a vein of clay slate, the residue of the territory being calciferous mica schist.
• The Precambrian gneiss and schist that make up the majority of the steep walls of the Black Canyon formed 1.
• Just to the south of this schist is the Willows Diorite, also of the same age as the tonalite, or Late Jurassic.
• This area is situated north of the Main Central Thrust (MCT) and is made up of bedrocks of granites, garnet mica schist, quartz biotite schist, kyanite schist, augen gneiss and banded augen gneiss.
• These areas were made up of mica schist that was severely laminated, cross-faulted in many areas, and interspersed with talc.
• This and other surface features are the result of glacial activity from the Pleistocene epoch; the metamorphic and igneous rocks below the surface – schist, sandstone, serpentine, magnetite, iron oxide – are the result of tectonic activity from the much earlier Paleozoic era and volcanic activity from subsequent geologic eras.
• The geology is varied, which translates into the variety of soils, with zones of schist, greywacke, limestone and quartzite.
• In contrast to the higher peaks of Piz Linard and Fluchthorn, which are mainly composed of hornblende gneiss (and schist), Piz Buin is composed of lighter granite and eye gneiss.
• It has as a geological limit the La Victoria Fault, where the rocks of the Gran Caracas group outcrop, on the igneous-metamorphic basement of the Sebastopol Complex of the lower Paleozoic, which is constituted by gneissic granite and chlorite schist.
• The city was born under the name of Briovera on a rocky outcrop of schist belonging to the Armorican Massif, in the Cotentin Peninsula, between the confluences of the Vire – which dominates the city centre – with the Dollée and Torteron, two rivers channelled in their urban sections.
• They found that the bedrock outcrops inside the structure, mapped as "polymict impact breccia" and classified as "megabreccia", consists of massive granite and schist that are indistinguishable in the field from Archean outcrops outside the structure.

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