Examples of lowermost

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The two lowermost units record progressive episodes of lake shallowing in deep-water, anoxic conditions, when lake stratification prevailed.
When the point of the disk attached to the wire came to the lowermost position, the wire was strained, the frame was pulled down, and an impulsive force was generated.
The lowermost part of the formation is characterized by relatively thick lava flows that exhibit well-developed columnar jointing where exposed in the walls of river gorges.
Whatever the cause, this scarp provides the only radial cross-section into the interior of the island and is therefore likely to expose some of the oldest (stratigraphically lowermost) accessible outcrops.
Furthermore, when grain number in heads exceeded eight, grain weight (mg) of the second uppermost grain, middle grain and second lowermost grain in each head was determined.
The lowermost part is composed of alternating cycles of fine-grained sands and sandstones.
Of particular note are the new borehole data from the lowermost part of the formation which does not crop out in the type area.
The latter species, however, is represented by only a few specimens in the lowermost sample of the zone and its identification remains somewhat tentative.
The lowermost 50 m consists of olivine gabbro in which layering becomes increasingly disturbed up-section by folds, slumps and trough layering structures.
The lowermost hybrid zones plot slightly below the mixing line, which could indicate super-heating of a few degrees.
Total organic carbon shows a gradual increase from around 0.4 % in the lowermost part to about 0.6 % near the core top.
The three lowermost samples all have the same measured age (450 ka) within uncertainties.
Thermoerosion takes place due to energy transported to the lowermost part of the frozen material by means of meltwater.
Medieval theory at times reverses interval order, so that in the chromatic we find the largest sometimes as the uppermost interval, sometimes as the lowermost.
The lowermost sediments consist of poorly consolidated cobble-to-boulder conglomerate with thin sandstone intervals.
Scattered pyrite nodules, 1 cm in diameter, occur within the lowermost metre.

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