Приклади вживання Igneous Англійська мовою та їх переклад на Українською
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The Igneous angel".
The North Atlantic Igneous Province.
Igneous rock is formed by the cooling and crystallization of magma or lava.
North Atlantic Igneous Province.
These minerals are typical weathering products of mafic igneous rocks.
Not quite an igneous rock, but pretty close to it.
Granit- this is one of the most solid rock, igneous rocks.
Historical novels:" the Igneous angel"(1908)," the Altar of victory"(1913).
The magma may cool and solidify to form intrusive igneous bodies(plutons).
Under them there are igneous and metamorphic rocks of Archean age.
Igneous rock can be found nearly everywhere on the earth's crust, particularly near volcanic hot spots.
For creating"mountains", usually igneous volcanic rocks, rugged mountain rocks with sharp edges, are used.
Igneous rocks are those that have formed by the cooling and crystallisation of magma, either at the Earth's surface or within the crust;
Low silicon content is indicative of mafic and ultramafic igneous rocks, such as basalt and dunite.
The most ancient formations are igneous and metamorphic rocks of the Ukrainian crystalline shield, exposed at the day surface in the West region.
As non-metallic mineral rocksappear all known genetic in nature types(igneous, metamorphic, sedimentary) and minerals almost all classes.
It is interspersed with igneous intrusions of a more recent age, the remnants of which have formed mountain massifs such as the Cairngorms and Skye Cuillins.
Knowing that the Flood would greatly modify thecraters, we need to look for more indirect, subtle evidence for these impacts in Precambrian igneous and metamorphic rocks.
Rocks laid down, usually in the last stages of igneous consolidation from magma rich in water and other volatile substances.
The initial plume head may have been several thousand kilometers in diameter, and it erupted volcanic rocks on both sides of the presentocean basin to produce the North Atlantic Igneous Province.
The Caribbean Plate is thought to be a large igneous province that formed in the Pacific Ocean tens of millions of years ago.
Many of the same magmatic processes that occur on Earth also occurred on Mars, and both planets are similar enough compositionally that thesame names can be applied to their igneous rocks and minerals.
In the 1820's, when the volcanic origin of basalt was proved andscientific theories about igneous and sedimentary rocks were developed, neptunism began to lose its significance.
Geologists believe that igneous oceanic plateaus may well represent a stage in the development of continental crust as they are generally less dense than oceanic crust while still being denser than normal continental crust.
Carved through sedimentary layers of sandstone, limestone,and shale and into the basement formations of mostly metamorphic schists and igneous granites, the Grand Canyon is a testimony to the erosive power of water.
The Deccan Traps are a massive igneous province- think of it as a lava flood plain- comparable in size to the US states of Oregon and Washington combined and composed of numerous lava flow layers having a total depth of over 6,500 feet(2,000 meters).
As part of the study, the researchers calculated the greenhousegas fluxes associated with the North Atlantic Igneous Province(NAIP)- one of Earth's largest LIPs that spans Britain, Ireland, Norway and Greenland.
An oceanic plateau(also submarine plateau) is a large, relatively flat submarine region that rises well above the level of the ambient seabed.[1][2] While many oceanic plateaus are composed of continental crust, and often form a step interrupting the continental slope,some plateaus are undersea remnants of large igneous provinces.
Rare-earth minerals areusually found in association with alkaline to peralkaline igneous complexes, in pegmatites associated with alkaline magmas and in or associated with carbonatite intrusives.
The Kerguelen Plateau is a large igneous province formed by a volcanic hot spot, but was associated with the breakup of Gondwana, was for a time above water, and is therefore considered to be a microcontinent, though not a continental fragment,[4][5] whereas other hotspot islands such as Iceland and Hawaii are considered neither microcontinents nor continental fragments.