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How to use sandstones in a sentence

Looking for sentences and phrases with the word sandstones? Here are some examples.

Sentence Examples
The tuffs are associated with subordinate sandstones and siltstones and minor lava.
Most sandstones arc characterized by erosional bases, hummocky cross-stratification and intensely burrowed tops.
Carrier-bed rocks are lithologically the same as reservoir rocks, that is, sandstones, limestones, or fractured rocks of all types.
It is thus unlikely that the bulk of the Carboniferous detritus could have been derived by recycling of preexisting Silurian sandstones.
It consists of phyllites, calcareous sandstones and limestone conglomerates that are boudinaged and folded.
The cross-bedded sandstones represent dunes from the dry intervals, when plant and animal life was less abundant.
Molasse is a dialect word used by French-speaking farmers in western Switzerland to describe soft, friable sandstones.
It contains over 50 chest beds which are interbedded with shales, carbonaceous sandstones and minor tuffs.
Does lithology account for the very different patterns of faulting in the Permian sandstones and dolostones?
The upper 300 m of the Haengefjeldet Formation is made up of 3-10 m thick well-sorted, normally graded, matrix-supported sandstones and wackes.
Among the 30 different types of stone recognized are varieties of diorite, granite, bedded tuff, sandstones, limestones, and tufa.
The most resistant rocks are quartzite and quartz-rich sandstones, and tough fine-grained rocks such as slate.
This member grades upwards into greenish mudstones and greenish-yellow, fine-grained sandstones of the overlying Cuarcitas Azules Member.
Whilst the greater part was just ordinary stone, many decorative elements were carved out of freestone such as sandstones and limestone.
Those sections expose concretionary mudstones interbedded with thinner quartz sandstones, limestones, and marl.
The significance of the contemporaneous, but kinematically very different fault sets in the sandstones requires explanation.
Occasional thin dark grey laminated mudstones are associated with some of the sandstones.
A comparison between all the techniques used to analyse calcite cements reveals subtle differences between injected and depositional sandstones.
Locally, near the village of Timirovo, the limestones are intercalated with arkosic sandstones.
They are interbedded with bioturbated muddy and sandy limestones, quartz-skeletal siltstones and sandstones.
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Examples from Classical Literature
The most durable of the red sandstones are those having a paler or grayer hue, like those of Woolton, Everton, and runcorn.
The beacons were found to be part of a horizontal, stratified series of sandstones underlying the igneous rock.
The coal is found, as already described, interbedded with shales and sandstones.
An upper series of sandstones and grits is seen for a short distance west of lamington.
Nodules of pyrites and of marcasite are common in many clays, sandstones and marls.
The separation of the mica in this case, or in that of micaceous sandstones, may be thus understood.
The sands and sandstones become highly crystalline quartzites, spotted with porphyritic developments of silicates.
The Eocene includes a series of sandstones and marls with lignite, and these are overlaid by nummulite limestones.
The Keweenawan is composed of immense piles of lava, such as those of Iceland, overlain by bedded sandstones.
These rocks have suffered thrusting and the shales are thus made in places to overlie the sandstones.
In the marls and sandstones of the Permian period there is also much gypsum.
Contemporaneous volcanic rocks are associated with the Ordovician beds and with the rhaetic sandstones in several places.
It occurs in a series of amygdaloidal dolerites or diabases, and in the associated sandstones and conglomerates.
The rocks along this stream are all sandstones, limestone and conglomerates, with many thin calcite veins.
Geologists are aware that many ancient sandstones and conglomerates are bound together or colored by iron.
The narrow foothill belt is composed of Tertiary sandstones that grade into loose sands and conglomerates.
In the sandstones of corncockle Moor reptilian footprints have been obtained.
The beds below these are referred to the English Yoredale series, and include some flaggy sandstones.
Slates and fine-grained sandstones appear here freely through the glacial drift.
The sandstones are grey in colour, weathering buff or reddish-brown, tinged more or less green by grains of glauconite.
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