<\/p>\n
+ The oldest oceanic basalt crust<\/strong> today is only about 200 million years.\n<\/p>\n <\/p>\n + They have a thick crust<\/strong> and deep roots that extend as much as several hundred kilometers into the Earth’s mantle.\n<\/p>\n <\/p>\n + The continental crust<\/strong> is mainly made of ArcheanArchaean, Proterozoic and some Palaeozoic granites and gneisses.\n<\/p>\n <\/p>\n + The source of the Siberian Traps basalt was, probably, a mantle plume at the base of the crust<\/strong> which erupted through the Siberian craton.\n<\/p>\n <\/p>\n + The Earth has an outer solid layer called the Crust<\/strong> crust<\/strong>, a highly viscous layer called the mantle, a liquid layer that is the outer part of the core, called the outer core, and a solid center called the inner core.\n<\/p>\n + The Earth’s crust<\/strong> has 17 major, rigid tectonic plates.\n<\/p>\n <\/p>\n + Sometimes a crust<\/strong> forms on top of the mantle.\n<\/p>\n <\/p>\n + Maillet’s geological observations convinced him that the Earth could not have been created in an instant because the features of the crust<\/strong> indicate a slow development by natural processes.\n<\/p>\n <\/p>\n + At ridges in the middle of oceans, new oceanic crust<\/strong> is created.\n<\/p>\n <\/p>\n + Below the crust<\/strong> is the mantle.\n<\/p>\n <\/p>\n + They are made of chopped pork and pork jelly sealed in a hot water crust<\/strong> pastry, and are most of the time eaten cold.\n<\/p>\n <\/p>\n + The crust<\/strong> is made up of different types of rocks: igneous, Metamorphic rockmetamorphic, and sedimentary rocks.\n<\/p>\n <\/p>\n + It escapes from the Earth’s crust<\/strong> into the atmosphere.\n<\/p>\n <\/p>\n + Other volcanic mountains form over hot spots, pockets of magma beneath the crust<\/strong> which erupt onto Earth’s surface.\n<\/p>\n <\/p>\n + Vanadium is an element that is widely distributed in Earth’s crust<\/strong> as well as in seawater and groundwater reservoirs.\n<\/p>\n <\/p>\n + Lava is magma, hot molten rock that flows through holes in the Earth’s crust<\/strong> and onto the surface.\n<\/p>\n <\/p>\n + To make this clear, seas around continents have continental crust<\/strong> beneath them.\n<\/p>\n <\/p>\n + Jean-Robert de Cavel is a French-American celebrity chef He was Chef de cuisine at The Maisonette from 1993-2002, Executive chef at Jean-Robert at Pigall’s from 2002-2009, and now works at Jean-Robert’s Table, Le Bar a Boeuf and French Crust<\/strong> Cafe.\n<\/p>\n <\/p>\n + Another is Iceland, which sits on top of the Mid-Atlantic Ridge, where new Earth’s crust<\/strong> is formed.\n<\/p>\n <\/p>\n + The moho, properly called the Mohorovi\u010di\u0107 discontinuity, is the boundary between the Earth’s crust<\/strong> and the mantle.\n<\/p>\n <\/p>\n + Furthermore, ideal crust<\/strong> development requires loaves of shapes not achievable in a machine’s loaf tin.\n<\/p>\n <\/p>\n + We now know that the existence of a viscous fluid under a thin crust<\/strong> is a much greater factor than the discovery of radioactivity, which was the textbook explanation for many years.\n<\/p>\n <\/p>\n + At Level Post Bay, the crust<\/strong> is more than one metre thick, and because of its flat surface it has been the site for various land speed record attempts.\n<\/p>\n <\/p>\n + The new crust<\/strong> then slowly moves away from the ridge.\n<\/p>\n <\/p>\n + Some people involved in the discipilne look at geodynamics, the Crust<\/strong> crust<\/strong>s, the motion of the geographical poles.\n<\/p>\n <\/p>\n + Fluorite naturally occurs on the earths’ crust<\/strong> in rocks, coal and clay.\n<\/p>\n <\/p>\n + An ophiolite is a section of the Earth’s oceanic crust<\/strong> and the underlying Earth’s mantleupper mantle that has been uplifted and exposed above sea level.\n<\/p>\n <\/p>\n + Earth’s mantle and crust<\/strong> formed about 100 million years after the formation of the planet, about 4.6 billion years ago.\n<\/p>\n <\/p>\n + The theory said that parts of the Earth’s crust<\/strong> move slowly on top of a liquid mantle of higher density.\n<\/p>\n <\/p>\n + Mid-ocean ridges are geologically active, with new magma constantly emerging onto the ocean floor and into the crust<\/strong> at and near rifts along the ridge axes.\n<\/p>\n <\/p>\n + They can also examine the crust<\/strong> in a seismic survey to try and find information about layers of rock, locate oil or gas fields and to get information about the internal structure of volcanos.\n<\/p>\n <\/p>\n + Such old continental crust<\/strong> and the mantle below it are less dense than other places in the Earth.\n<\/p>\n <\/p>\n + It has its own magma plumbing under the Earth that goes down under the Earths crust<\/strong> by 60 km.\n<\/p>\n <\/p>\n + Some of the earth’s crust<\/strong> gets pushed into Sichuan and southern China.\n<\/p>\n <\/p>\n + The lithosphere, above, includes the crust<\/strong> and the uppermost part of the mantle.\n<\/p>\n <\/p>\n + Some contain oceanic crust<\/strong> only.\n<\/p>\n <\/p>\n + It does include oceanic crust<\/strong> west to the Mid-Atlantic Ridge and north to the Gakkel Ridge.\n<\/p>\n <\/p>\n + The Earth’s mantle is a layer of silicate rock between the crust<\/strong> and the outer core.\n<\/p>\n <\/p>\n + There is also a lizard, the Lake Eyre Dragon, Ctenophorus maculosus, that lives in the cool mud below the salt crust<\/strong> of the lake.\n<\/p>\n <\/p>\n + As the oceanic crust<\/strong> moves away from the ridge axis, the peridotite in the underlying mantle cools and becomes more rigid.\n<\/p>\n <\/p>\n + The oceanic crust<\/strong> is thinner, 5 km thick.\n<\/p>\n <\/p>\n + The physical geography of the province was caused by extension and thinning of the lithosphere, which is composed of crust<\/strong> and upper mantle.\n<\/p>\n <\/p>\n + They are large areas of flat topped rocks that have been lifted high above the crust<\/strong> by continental plates.\n<\/p>\n <\/p>\n + That means the Earth’s crust<\/strong> is made of rock.\n<\/p>\n <\/p>\n + Melted material from the mantle and crust<\/strong><\/strong> moves up through the crust<\/strong><\/strong> and collects in magma chambers.\n<\/p>\n <\/p>\n + It is thought that the green ophiolite rock was formed at the moho, That is, the junction between the bottom of the Earth’s crust<\/strong> and the top of the Earth’s mantle.\n<\/p>\n <\/p>\n + These are all thought to have originated from the crust<\/strong> of the asteroid 4 Vesta, their differences being due to different geologic histories of the parent rock.\n<\/p>\n <\/p>\n + A terrane is a fragment of Earth’s crust<\/strong><\/strong><\/strong>crust<\/strong><\/strong><\/strong> from one tectonic plate stuck to crust<\/strong><\/strong><\/strong> lying on another plate.\n<\/p>\n <\/p>\n + In 2007 a team of scientists on board the RRS James Cook went to an area of the Atlantic seafloor where the mantle has no crust<\/strong> covering.\n<\/p>\n <\/p>\n + We can know the thickness of the Earth\u2019s crust<\/strong> with Love waves.\n<\/p>\n <\/p>\n + At first the crust<\/strong> was very thin, and was probably changed often as the tectonic plates shifted around a lot more than they do now.\n<\/p>\n <\/p>\n + As it moves away from the ridge, the crust<\/strong> becomes cooler and denser, while the sediment may build on top of it.\n<\/p>\n <\/p>\n + It forms new crust<\/strong> as the plates move away from each other.\n<\/p>\n <\/p>\n + It includes much of the continent of Africa, as well as oceanic crust<\/strong> which lies between the continent and various surrounding ocean ridges.\n<\/p>\n <\/p>\n + The crust<\/strong> is of two different types.\n<\/p>\n <\/p>\n + Past episodes of melting and volcanism at the outer levels of the mantle have produced a very thin crust<\/strong> of crystallized melt products near the surface, where we live.\n<\/p>\n <\/p>\n + The crust<\/strong> similar to that of an English muffin and mostly cooked in an electric oven.\n<\/p>\n <\/p>\n + The crust<\/strong> and the upper mantle make up the lithosphere.\n<\/p>\n <\/p>\n + Many of them have ribbed or nodular surfaces, and sometimes they have a crust<\/strong> intersected by many cracks like the surface of a loaf of bread.\n<\/p>\n <\/p>\n + The Andes are the result of plate tectonics processes, caused by the subduction of oceanic crust<\/strong> beneath the South American continental plate.\n<\/p>\n <\/p>\n + The salt crust<\/strong> on the lake is not thick and can break like glass under a person’s weight.\n<\/p>\n <\/p>\n + The crust<\/strong> and the relatively rigid peridotite below it make up the oceanic lithosphere.\n<\/p>\n <\/p>\n![\"Use](\"https:\/\/englishteststore.net\/blog\/wp-content\/uploads\/2021\/09\/Use-in-sentence-of-crust.jpg\" "\\"Use")
Example sentences of “crust”:<\/h2>\n
+ The Earth's crust<\/strong> has 17 major, rigid tectonic plates.\r\n
+ Sometimes a crust<\/strong> forms on top of the mantle.\r\n
+ Maillet's geological observations convinced him that the Earth could not have been created in an instant because the features of the crust<\/strong> indicate a slow development by natural processes.\r\n
<\/pre>\nMore in-sentence examples of “crust”:<\/h2>\n
+ At Level Post Bay, the crust<\/strong> is more than one metre thick, and because of its flat surface it has been the site for various land speed record attempts.\r\n
+ The new crust<\/strong> then slowly moves away from the ridge.\r\n
+ Some people involved in the discipilne look at geodynamics, the Crust<\/strong> crust<\/strong>s, the motion of the geographical poles.\r\n
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