Stratiform in a sentence

There is no stratiform type in this group because by definition, even very thick stratiform clouds cannot have towering vertical structure, although nimbostratus may be accompanied by embedded towering cumuliform or cumulonimbiform types.

The nature of the mineral occurrence: Massive stratiform/supergene manganese mineralisation hosted within sediments of the Ullawarra Formation.

Due to the variable shape of the breccia and vein zones, true widths estimates are not applicable for these intersections as is reported for the stratiform mineralization.

Mineralization at the ICO is characterized as syngenetic, stratiform/tabular exhalative deposits within, or closely associated with, the mafic sequences of the Apple Creek Formation.

Some crosscutting mineralization is present that may be in feeder zones to the stratiform mineralization or may be due to remobilization locally into fracture quartz veins and/or crosscutting structures.

Cirrocumulus in its pure form is actually a high cumuliform genus, and cirrostratus is stratiform, like altostratus and lower based sheet clouds.

Cumuliform clouds forming in the lower level were given the genus name cumulus from the Latin word for heap, citation and low stratiform clouds the genus name stratus from the Latin word for sheet or layer.

Low stratocumuliform, stratiform, and cumuliform genera Low-étage clouds are found from near surface up to convert.

Ragged stratiform and cumuliform species The species fractus shows variable instability because it can be a subdivision of genus-types of different physical forms that have different stability characteristics.

Stratocumuliform and stratiform clouds in the high étage carry the prefix cirro-, yielding the respective genus names cirrocumulus (Cc) and cirrostratus (Cs).

Stratocumuliform and stratiform genera have the prefix cirro- when they occur in the high étage, and alto- when based in the middle altitude range.

Stratocumuliform Clouds of this structure have both cumuliform and stratiform characteristics in the form of rolls or ripples.

These were respectively stratocumuliform and stratiform cloud genera of a newly defined middle étage above stratocumulus and stratus but below cirrocumulus and cirrostratus.

The stratiform group is cross-classified into the genera cirrostratus (high-étage), altostratus (middle-étage), stratus (low-étage), and nimbostratus (multi-étage).

When a low stratiform cloud contacts the ground, it is called fog if the prevailing surface visibility is less than 1 kilometer, although radiation and advection types of fog tend to form in clear air rather than from stratus layers.