On this sand a great mass of boulder clay usually quite devoid of fossils was accumulated.
The boulder clay, when it was first studied, seemed in many of its characters so singular and anomalous, that geologists despaired of ever being able to interpret the phenomena by reference to causes now in action.
The chalk, then, is certainly older than the boulder clay.
The difficulty, moreover, of accounting for the entire dearth of marine shells in till is removed when once we have adopted the theory of this boulder clay being the product of land-ice.
Examplesofboulder clay
boulder clay
Boulderclayis classed with a group of poorly sorted materials, described by the non-genetic term diamicton.
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Boulderclayand clays are also found south of the village.
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Boulderclayis also abundant and moraines cover substantial areas.
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So only at the margins of an ice sheet would the fluctuating sedimentary record be preserved, whereas interior glaciation might compound tills in final deposits ofboulderclay.
From theCambridge English Corpus
We will not, for example, have the fritillary without water meadows, nor the oxlip without ancientboulderclaywoods.
From the
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It is sour, limeless,boulderclay, with not very good drainage, and an unfortunate predilection for growing rushes.
From the
Hansard archive
Example from the Hansard archive. Contains Parliamentary information licensed under theOpen Parliament Licence v3.0
They told me that they had run into 12 kilometres ofboulderclayand that it was improbable that they would be able to bury the pipeline for that length.
From the
Hansard archive
Example from the Hansard archive. Contains Parliamentary information licensed under theOpen Parliament Licence v3.0
The valley bottoms have a thin deposit ofboulderclay.
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The local drift geology is mostly glacialboulderclay, as well as glacial sands and gravel.
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The clay-rich hilltop soils are primarily a consequence of blanketing of the area withboulderclayor glacial till during the recent glaciations.
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Till, also known asboulderclay, is a mix of unconsolidated sediment with a range of grain sizes (clay-boulder).
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Muchboulderclayis of a bluish-grey until exposed to weather which causes a transformation to a brown colour.
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Beneath the pasture the archaeology is onboulderclayoverlying magnesian limestone.
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The earliest masonry building was the church, which was constructed on shallow foundations of sandstone rubble and pebbles onboulderclay.
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It consists of ancient semi-natural woodland on aboulderclaysoil.
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