Examples of 'lavas' in a sentence
Meaning of "lavas"
Lava is molten rock that erupts from a volcano or fissure in the earth's crust. It usually flows downhill and cools to form solid rock
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- plural of lava
How to use "lavas" in a sentence
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lavas
Lavas born in the center of the earth.
Therocksarehighlyaltered deformed volcanic lavas known as amphibolites.
Trident lavas are andesitic to dacitic in composition.
Presumably at first fluid basaltic lavas were erupted.
These lavas are thought to be a few months old.
Its upper section is made up of pillow lavas.
Viscous lavas tend to form stratovolcanoes or lava domes.
The chronology of sculptures and enamelled lavas.
Lavas lavas are primary volcanic rocks.
Water and lavas are there.
Lavas range from basanites to mugearites.
Later the main edifice was built by andesitic lavas.
Pillow lavas from a submarine volcano.
It is an extensive area covered with thick lavas and tuffs.
The thickness or viscosity of lavas can be shown in a number of ways.
See also
Tan areas are plains formed by eruption of highly fluid lavas.
The most alkalic lavas erupted outside the rift.
Who teaches us you do not often lavas your teeth.
Leucite is common in lavas but very rare in plutonic rocks.
The overthrusting event resulted in deformation of underlying pillow lavas.
Hawaii lavas are quite runny.
Most agates occur as nodules in volcanic rocks or ancient lavas.
We compare them with lavas from other tholeiitic provinces.
Abetti is a lunar crater that has been completely submerged by mare lavas.
Lava tubes allow fluid lavas to advance great distances.
Pillow lavas are used generally to confirm subaqueous volcanism in metamorphic belts.
Some of the lavas have.
Its lavas are andesitic.
This may have formed from contractional cooling of basltic lavas.
The composition of the lavas erupted in this stage is usually alkalic.
Lavas commonly erupt through reefs that form offshore as erosion progresses.
The composition of the lavas varies from tholeiitic basalt to rhyolite.
The soil resembled those produced from the weathering of basaltic lavas.
It is an eroded remnant of basaltic lavas originally laid down on a sedimentary base.
These lavas also erupted from vents on the flanks of the volcano.
Another more plausible explanation is that the lavas were extruded in layers.
The lower flanks consist of mostly basaltic and some andesitic lavas.
This helps provide insight on how the lavas of the region operate.
The coastal shelf is interpreted in terms of accumulation of hyaloclastites and pillow lavas.
This is especially critical for komatiite lavas and ultramafic intrusive rocks.
They tend to be ancient volcanic rocks that formed from very hot lavas.
The dacites are crystal rich and some lavas show evidence of magma mixing.
The lavas have significant amounts of carbonate but very low calcium and magnesium levels.
The lava production was high when the rhomb porphyry lavas were deposited.
That ultimately leads to the lavas that are erupted from the volcanoes at the surface.
The depression itself however does not appear to contain lavas from this plateau.
The majority of these lavas erupted or flowed into the depressions associated with impact basins.
Volatile compounds turn into gas as the lavas rise from the depths.
Mare lavas apparently could reach the surface more often and more easily there.
The green cores pyroxenes from martin vaz nephelinite lavas are characterized by a polibaric fractionation.
