homoclinal sentence in Hindi
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- All gradations occur between hogbacks, homoclinal ridges, and cuestas.
- Cuestas, homoclinal ridges, and hogbacks comprise a sequence of landforms that form a gradational continuum.
- The southernmost Golfe d'Arguin describes a homoclinal ramp profile with vast intertidal plains around Tidra Island.
- Generally, cuestas and homoclinal ridges are asymmetrical in that their dip slopes are less steep than their escarpments.
- In general, homoclinal ridges, or strike ridges, are associated with strata that dip between 10?and 30?
- Where hogback, homoclinal ridges, and cuestas occur depends upon whether the local rock attitudes are either nearly vertical, moderately dipping, or gently dipping.
- The opposite slope, its frontslope, that forms the front of a homoclinal ridge consists of an escarpment that cuts across the bedding of the strata comprising it.
- Because of the moderately dipping nature of the strata that forms a homoclinal ridge, a significant shift in horizontal location will take place the landscape is lowered by erosion.
- The surface of hard, erosion-resistant rock strata forms the caprock of the backslope ( dip-slope ) of the homoclinal ridges from which erosion has preferentially stripped any weaker strata.
- The erosion of tilted sequences of either stratified sedimentary or igneous rock, homoclines, of alternating resistance to erosion produce distinctive landforms that form a gradational continuum from cuestas through homoclinal ridges to hogbacks.
- Homoclinal ridges are the expression of regional outcrops of moderately dipping strata, typically sedimentary strata, that consist of alternating beds of hard, well-lithified strata, i . e . sandstone and limestone and weak or loosely cemented strata, i . e . shale, mudstone, and marl.
- For example, the erosion of homoclines consisting of resistant beds of either limestone, sandstone, or both interbedded with weaker, less resistant beds of either shale, siltstone, marl, or combination of them will produce either cuestas, homoclinal ridges, or hogbacks depending on the angle of dip of the strata.
- Because the slope of a homoclinal ridge dips in the same direction as the sedimentary strata underlying it, the dip angle of this bedding ( ? ) can be calculated by v / h = tan ( ? ) where v is equal to the vertical distance and h is equal to the horizontal distance perpendicular to the strike of the beds.
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