Sentence examples for relatively uplifted from inspiring English sources

Exact(1)

A block that has been relatively uplifted between two normal faults that dip away from each other is called a horst.

Similar(59)

Question: is the sight of Ann Widdecombe on our screens in a time that now sees Michael Gove presiding over our justice system a more or less exquisite torture than it used to be? Has she been transfigured by recent events into a relatively uplifting reminder of better days?

If the uplifted surface had originally been low and without prominent relief, it is likely to remain relatively flat when uplifted to a relatively uniform elevation.

This type of analysis helps to identify the morphometric indices that are most useful for tectonic analysis in areas of unknown uplift, allowing for easy identification of short spatial variations of uplift rate and detection of areas with relatively fast uplift rates in unstudied coastal zones.

Relative uplift values reveal the presence of tectonically uplifted blocks together with relatively subsided or lesser uplifted zones along known faults.

Then, relatively rapid uplift gave rise to basin inversion and erosion prior to or during the early Tortonian.

Relatively small uplifts (less than 1 mm/year) are observed at the Alpine foothills and in a wide area comprised between the Euganean Hills and the lagoon.

Rocks belonging to medium-pressure facies series generally follow P-T-t paths that are clockwise loops on a pressure-temperature diagram, reflecting rapid burial during a collisional event followed by heating and relatively rapid uplift.

Our analysis suggests that Santa Catalina Island has recently experienced, and may still be experiencing, relatively rapid uplift, causing intense landscape rejuvenation that removed nearly all traces of marine terraces by erosion.

The structural and mineralogical features of the FPs can be explained by the development of fractures and fluid circulation due to the relatively rapid uplift of the granite during orogenesis.

The usual mechanisms for concomitantly gradualistic denudation by ice, wind, and running water are set aside in orogenic belts by relatively rapid uplifts of material ranging from nearly unconsolidated sediment to semicoherent but intensely deformed masses of metamorphic and igneous rocks.

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