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The traditional scaling means that the square of the fissure thickness is of the same order as the permeability coefficient of the matrix set.
The embryonic fissure, which reaches the peripheral retina at the ventral-nasal aspect of the eye, was used as a landmark.
The other fissures have been destroyed by quarrying operations.
The upper and lower parts of some fissure fills were also obscured by quarry scree.
This process creates vesicles and fissures as near- and sub-surface pockets of these minerals volatilize.
Figure 7d shows the meniscus fill to the fissure.
Various fragments of both sculptures showed evidence of fissures and breakages, some of which appear to have been produced by contact with fire.
But this attempt fizzled, undermined by internal fissures and regional pressures that still preclude a strong central state.
For some permeability ratios and fissure widths, the large-scale description is achieved by introducing the so-called double porosity model.
Some fissure-fills contain angular fragments of wall-rock that can be matched to the adjacent margin.
The reptiles and mammals found in the fissure deposits are found, most frequently, in the form of numerous disarticulated skeletal elements.
Some smaller cavities, or larger cavities with restricted access to the unconformity, were apparently filled by sediment that trickled down into the fissure system.
However, a significant amount of extension is still represented by the sediment-filled fissures.
These changes opened up a series of structural fissures and internal conflicts.
In the model under consideration, the width of the fissure is much smaller than the dimension of the adjacent block.
