Перевод и анализ слов искусственным интеллектом ChatGPT
На этой странице Вы можете получить подробный анализ слова или словосочетания, произведенный с помощью лучшей на сегодняшний день технологии искусственного интеллекта:
- как употребляется слово
- частота употребления
- используется оно чаще в устной или письменной речи
- варианты перевода слова
- примеры употребления (несколько фраз с переводом)
- этимология
Что (кто) такое SANDSTONE - определение
![Paradise Quarry, [[Sydney]], Australia](https://commons.wikimedia.org/wiki/Special:FilePath/(1)Saunders Quarry-1.jpg?width=200 "Paradise Quarry, [[Sydney]], Australia")
![Grus]] sand and the granitoid from which it is derived](https://commons.wikimedia.org/wiki/Special:FilePath/GrusSand.JPG?width=200 "Grus]] sand and the granitoid from which it is derived")
![17,000 yr old sandstone [[oil lamp]] discovered at the caves of [[Lascaux]], [[France]]](https://commons.wikimedia.org/wiki/Special:FilePath/Lampe a graisse - Lascaux.jpg?width=200 "17,000 yr old sandstone [[oil lamp]] discovered at the caves of [[Lascaux]], [[France]]")
![Cross-bedding and scour in sandstone of the [[Logan Formation]] ([[Lower Carboniferous]]) of Jackson County, [[Ohio]]](https://commons.wikimedia.org/wiki/Special:FilePath/Logan Formation Cross Bedding Scour.jpg?width=200 "Cross-bedding and scour in sandstone of the [[Logan Formation]] ([[Lower Carboniferous]]) of Jackson County, [[Ohio]]")
![Lower Antelope Canyon]], Arizona, worn smooth by erosion from [[flash flood]]ing over thousands of years](https://commons.wikimedia.org/wiki/Special:FilePath/Lower antelope 2 md.jpg?width=200 "Lower Antelope Canyon]], Arizona, worn smooth by erosion from [[flash flood]]ing over thousands of years")
![Photomicrograph of a [[volcanic]] [[sand grain]]; upper picture is plane-polarised light, bottom picture is cross-polarised light, scale box at left-centre is 0.25 millimeter. This type of grain would be a main component of a lithic sandstone.](https://commons.wikimedia.org/wiki/Special:FilePath/LvMS-Lvm.jpg?width=200 "Photomicrograph of a [[volcanic]] [[sand grain]]; upper picture is plane-polarised light, bottom picture is cross-polarised light, scale box at left-centre is 0.25 millimeter. This type of grain would be a main component of a lithic sandstone.")
![Sandstone statue ''Maria Immaculata'' by Fidelis Sporer, around 1770, in [[Freiburg]], [[Germany]]](https://commons.wikimedia.org/wiki/Special:FilePath/MariaImmaculatal Augustiner.jpg?width=200 "Sandstone statue ''Maria Immaculata'' by Fidelis Sporer, around 1770, in [[Freiburg]], [[Germany]]")
![sandstone university]]](https://commons.wikimedia.org/wiki/Special:FilePath/SydneyUniversity MainBuilding Panorama.jpg?width=200 "sandstone university]]")
![Alcove]] in the [[Navajo Sandstone]]](https://commons.wikimedia.org/wiki/Special:FilePath/MoabAlcove.JPG?width=200 "Alcove]] in the [[Navajo Sandstone]]")
![Kokh-type]] tombs cut into the multicoloured sandstone of [[Petra]]](https://commons.wikimedia.org/wiki/Special:FilePath/PetraSandStoneRock-cut tombs.jpg?width=200 "Kokh-type]] tombs cut into the multicoloured sandstone of [[Petra]]")
![Sand grains of [[quartz]] with [[hematite]] coating providing an orange colour](https://commons.wikimedia.org/wiki/Special:FilePath/CoralPinkSandDunesSand.JPG?width=200 "Sand grains of [[quartz]] with [[hematite]] coating providing an orange colour")
Википедия
Sandstone is a clastic sedimentary rock composed mainly of sand-sized (0.0625 to 2 mm) silicate grains. Sandstones comprise about 20–25% of all sedimentary rocks.
Most sandstone is composed of quartz or feldspar (both silicates) because they are the most resistant minerals to weathering processes at the Earth's surface. Like uncemented sand, sandstone may be any color due to impurities within the minerals, but the most common colors are tan, brown, yellow, red, grey, pink, white, and black. Since sandstone beds often form highly visible cliffs and other topographic features, certain colors of sandstone have been strongly identified with certain regions.
Rock formations that are primarily composed of sandstone usually allow the percolation of water and other fluids and are porous enough to store large quantities, making them valuable aquifers and petroleum reservoirs.
Quartz-bearing sandstone can be changed into quartzite through metamorphism, usually related to tectonic compression within orogenic belts.
