<\/p>\n
– The courthouse was built of local sandstone<\/strong> in 1896.\n<\/p>\n <\/p>\n – Jena partly lies in the middle hall valley between from mixed woodlands covered shelly limestone and sandstone<\/strong> slopes.\n<\/p>\n <\/p>\n – Miller described his collecting later, in a popular work on the rocks and fossils of the Old Red Sandstone<\/strong> in Scotland.Miller, Hugh 1841.\n<\/p>\n <\/p>\n – Most of the original texture of the sandstone<\/strong> is destroyed by the metamorphism.\n<\/p>\n <\/p>\n – Wat Karuna This temple houses Chai Nat’s largest sandstone<\/strong> Buddha image.\n<\/p>\n <\/p>\n – There are impressive rock islands of dark red or gray Torridonian sandstone<\/strong> which stick up out of the gneiss.\n<\/p>\n <\/p>\n – England had coarse limestone, red sandstone<\/strong> and dark green Purbeck marble which was often used for architectural decorations like thin columns.\n<\/p>\n – They were found in the 1830s in the Old Red Sandstone<\/strong> of Scotland.\n<\/p>\n <\/p>\n – The sandstone<\/strong> was then covered by a layer of marine sedimentary rock.\n<\/p>\n <\/p>\n – This formed a confining layer, trapping water in the sandstone<\/strong> aquifer.\n<\/p>\n <\/p>\n – The rock is from New Red Sandstone<\/strong> of the Permian or Triassic periods.\n<\/p>\n <\/p>\n – When sandstone<\/strong> is changed to quartzite, the individual quartz grains and cement material recrystallizes.\n<\/p>\n <\/p>\n – There are older and younger sandstone<\/strong> groups, with a long period between them.\n<\/p>\n <\/p>\n – Everyone should have seen the world-famed Rider or Bamberg horseman inside and many other medieval sandstone<\/strong> figures as well.\n<\/p>\n <\/p>\n – Over the years numerous visitors have added graffiti by carving names in the soft sandstone<\/strong> at the base of the pillar.\n<\/p>\n <\/p>\n – Its sediments extend 130 m downward and lie atop an older sandstone<\/strong> foundation.\n<\/p>\n <\/p>\n – With no real stone or sandstone<\/strong> available, brick was used as building material.\n<\/p>\n <\/p>\n – It is formed when sandstone<\/strong> is squeezed and heated under a chain of mountains.\n<\/p>\n <\/p>\n – At the western end of the lake and on the north shore, he described a sandstone<\/strong> range, which he named Long’s Range after his brother-in-law.\n<\/p>\n <\/p>\n – For example, clay layers may alternate with sandstone<\/strong> layers; or carbonate layers alternate with shales.\n<\/p>\n <\/p>\n – The New Red Sandstone<\/strong><\/strong> is much brighter and redder in colour than the Old Red Sandstone<\/strong><\/strong>, as the examples show.\n<\/p>\n <\/p>\n – The water of the GAB is held in a sandstone<\/strong> layer laid down by continental erosion of higher ground during the Triassic, Jurassic, and Lower Cretaceous periods.\n<\/p>\n <\/p>\n – Nearby Medicine Rocks State Park has many unusual sandstone<\/strong> rock formations.\n<\/p>\n <\/p>\n – However, not all the Old Red Sandstone<\/strong> is red or sandstone<\/strong>\u2014 the sequence also includes Conglomerate conglomerates, mudstones, siltstones and thin limestones and colours can range from grey and green through red to purple.\n<\/p>\n <\/p>\n – The Old Red Sandstone<\/strong> is a dark red sandstone<\/strong> laid down mainly in the Devonian period over a large part of the continent of Laurussia.\n<\/p>\n <\/p>\n – That sandstone<\/strong><\/strong> had more colors than the grey sandstone<\/strong><\/strong> that was local.\n<\/p>\n <\/p>\n – Study of hydrogeological conditions of the Nubian Sandstone<\/strong> Aguifer in the area between Abu Simbel Toschka, Western Desert, Egypt.\n<\/p>\n <\/p>\n – The range consists of sandstone<\/strong> hills, surrounded by Triodiaspinifex grasslands.\n<\/p>\n <\/p>\n – Saxon Switzerland is characterized by its sandstone<\/strong> rocks which draw many rock climbers.\n<\/p>\n <\/p>\n – Ratcliff name is from a sandstone<\/strong> cliff.\n<\/p>\n <\/p>\n – It is mainly forest on a sandstone<\/strong> plateau 60 to 180 kilometres inland from central Sydney.\n<\/p>\n <\/p>\n – Chambers Pillar is a sandstone<\/strong> formation about 160km south of Alice Springs, Northern TerritoryAlice Springs in the Northern Territory of Australia.\n<\/p>\n <\/p>\n – Most natural arches are formed from narrow fins and sea stacks that is made up of sandstone<\/strong> or limestone.\n<\/p>\n <\/p>\n – The site has over 3,000 quartzite sandstone<\/strong> pillars and peaks, many over in height.\n<\/p>\n <\/p>\n – It is made up of quartzite, quartz sandstone<\/strong><\/strong> and sandstone<\/strong><\/strong>.\n<\/p>\n <\/p>\n – The coast is made up of a lot of rocks, including grey sandstone<\/strong> and limestone.\n<\/p>\n <\/p>\n – The fossil was in a layer of sandstone<\/strong> rocks on the foreshore of Cowie, near Stonehaven.\n<\/p>\n <\/p>\n – It is mainly a sandstone<\/strong> plateau.\n<\/p>\n <\/p>\n – In the east is a heavily eroded sandstone<\/strong><\/strong> mountain range, which can be seen as sandstone<\/strong><\/strong> outcrops such as those around Gin’s Leap between Baan Baa and Boggabri.\n<\/p>\n <\/p>\n – The Old Red Sandstone<\/strong> was first discovered in Great Britain, and it played a big part in early geology.\n<\/p>\n <\/p>\n – It is often called the Old Red Sandstone<\/strong> Continent or Euramerica.\n<\/p>\n <\/p>\n – The hilly landscape is formed by way that the sandstone<\/strong> wears down evenly.\n<\/p>\n <\/p>\n – The ranges are made from Devonian era sandstone<\/strong> and have been eroded over 20 million years into shapes like towers and cones.\n<\/p>\n <\/p>\n – It had a gun pit that was built out of large blocks of sandstone<\/strong> and carved partly from the original rock that was already there.\n<\/p>\n <\/p>\n – The map shows the sandstone<\/strong> as orange: it is on the western edge of the mainland, and on part of Skye.\n<\/p>\n <\/p>\n – It is 1084.6 meters tall, of sandstone<\/strong> and granite.\n<\/p>\n <\/p>\n – The southwest of the country forms a sandstone<\/strong> massif.\n<\/p>\n <\/p>\n – It is built out of red sandstone<\/strong> and stands on a hill in the neck of the meander of the River Severn.\n<\/p>\n <\/p>\n – Other beaches close to the city include “Sandspit BeachSandspit”, “Hawke’s Bay”, and “Paradise Point” – a sandstone<\/strong> rock promontory with a natural arch, but Clifton Beach is the most popular picnic destination in Karachi.\n<\/p>\n <\/p>\n – The fault divides the Old Red Sandstone<\/strong> and Devonian deposits brownish, no.\n<\/p>\n <\/p>\n – They were discovered in the first half of the 19th century in the Old Red Sandstone<\/strong> of Britain.\n<\/p>\n <\/p>\n – Arkose is a kind of sandstone<\/strong> which is rich in the mineral feldspar.\n<\/p>\n <\/p>\n – Also, because fossils of early tetrapods are found widely in the Old Red Sandstone<\/strong> continent, formed by the joining of North America and northwestern Europe they must have spread by following the coastal lines.\n<\/p>\n <\/p>\n – As a result of later periods of Rift rifting and mountain-building, some of the Torridian sandstone<\/strong> lies under the sea, and some of it is uplifted into mountains.\n<\/p>\n <\/p>\n – The barracks were made from large sandstone<\/strong> blocks and carved out of the rock on the headland.\n<\/p>\n <\/p>\n – They are usually made up of granites or gneisses, but can sometimes be found in other rock types like limestone, sandstone<\/strong> and conglomerate.\n<\/p>\n <\/p>\n – This town had a sandstone<\/strong> mine, and had a railroad that went through it.\n<\/p>\n <\/p>\n – The main source of placoderm fossils is the Old Red Sandstone<\/strong> continent.\n<\/p>\n <\/p>\n – The lower sandstone<\/strong> is a breccia, with broken fragments of earlier rocks.\n<\/p>\n <\/p>\n – The most important monuments in the commune are the “Boule de Gargantua”, a block of sandstone<\/strong> moved there by the giant “Gargantua the “Peyzieu churchPeyzieu” church and the ruins of the “Ch\u00e2teau de Longecombe”, a castle from the 12th century.\n<\/p>\n <\/p>\n – The Casquets are a group of rocks 13km northwest of Alderney and are part of an underwater sandstone<\/strong> ridge.\n<\/p>\n <\/p>\n – Ortac and Alderney, along with the Casquets, are part of the same sandstone<\/strong> ridge.\n<\/p>\n <\/p>\n – The rock is made up of quartzite and sandstone<\/strong> rock, resting on slates of Kaolinitekaolinised clay.\n<\/p>\n <\/p>\n – These are sandstone<\/strong> deposits containing rounded pebbles.\n<\/p>\n <\/p>\n – However, the outlook of the place has not much changed due to the existence of sandstone<\/strong> walls and four Khmer style pagodas.\n<\/p>\n <\/p>\n – There was “a beautiful picture of this junction washed bare by the sea”, where 345 million year old Devonian Old Red Sandstone<\/strong> overlies 425 million year old Silurian greywacke.\n<\/p>\n <\/p>\n![\"sandstone](\"https:\/\/englishteststore.net\/blog\/wp-content\/uploads\/2021\/09\/sandstone-use-in-sentences.jpg\" "\\"sandstone")
Example sentences of “sandstone”:<\/h2>\n
- They were found in the 1830s in the Old Red Sandstone<\/strong> of Scotland.\r\n
- The sandstone<\/strong> was then covered by a layer of marine sedimentary rock.\r\n
- This formed a confining layer, trapping water in the sandstone<\/strong> aquifer.\r\n
<\/pre>\nMore in-sentence examples of “sandstone”:<\/h2>\n