Príklady outcrop

• Concentrations of pumice clasts towards the base form trains of clasts that are traceable along the length of outcrops.

• We can therefore confidently assume that transgression proceeded well beyond all of these limiting outcrops.

• If o lightning impacts on an outcrop with abundant cracks and fractures, the strong currents will cause moisture in the cracks to evaporate instantaneously.

• Distances are approximations based on known outcrops of materials.

• Therefore, alteration conditions must always be studied individually in each outcrop and cannot be assumed to be spatially invariant.

• The terrain at the western end of the hills consists of a plateau region with sandstone outcrops and slow-flowing streams.

• It is obvious that the lightning hit and blasted an outcrop of metacherts.

• These can be compared with what we see preserved in the field, thus enhancing our interpretations of outcrop geology.

• It is important to use structural geometries on an outcrop scale and local cross-cutting relationships to evaluate their relative timing.

• Map shows the outcrop distribution and, where differentiated, the formations are indicated by patterned fill.

• Thicknesses estimated from structural dip of the units where intersected by boreholes or at outcrop.

• In laterite outcrops, where the influence of the rains is hardly felt, large expanses of small bamboos of stunted appearance are met with.

• These were collected from different outcrops several kilometres apart, within the mangrove swamp units of the area, with a vibracorer at very shallow depth.

• The papers are illustrated with maps, cross-sections, burial history curves, seismic lines, and photographs of cores, photomicrographs and even rocky outcrops.

• Also, a low concentration would be preferred since free water on ironstone outcrops is largely unavailable.