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To the north lie the Apuseni Mountains, centred on the Bihor Massif, from which emerge fingerlike protrusions of lower relief.
Water is well established as a major driver of the geomorphic change that eventually reduces mountains to lower relief landscapes.
The sand cover of the Arabian Desert occurs as dunes of varying size and complexity or as a thin film on surfaces of lower relief.
It shows human beings, sea monsters, and fish, with the waves of the sea rendered in lower relief than the figures.
In the western part of the upland, the lower relief, gentler slopes, and milder winters render the region more suitable for crop farming, and much of the forest cover has been cleared; most farmers also raise sheep and beef cattle.
Whereas the southern Longmen Shan exhibits only subtle differences associated with slightly lower hillslope and channel gradients, the northern Longmen Shan is characterized by topography of significantly lower relief, lessened hillslope gradients, and low-gradient channels.
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As shown in the lower right part of the diagram, the shape of the hypsometric curve varies in early geologic stages of development of the watershed, but once a steady state (mature stage) is attained, tends to vary little thereafter, despite lowering relief.
In analysis, a curve is derived by plotting the relative height (h/H) and relative areas (a/A); the obtained curve is called as hypsometric curve (Suresh 1997).The shape of hypsometric curve varies in early geologic stages of development of the drainage basin, but once a steady state is attained it tends to vary little despite lowering relief (Kumar 1991; Suresh 1997).
Barber completed work on his version of the design, with a greatly lowered relief, and the new coin went into production on a large-scale basis.
The slope-based Grid-to-Grid (G2G) model adequately simulated observed river flows under current climate conditions for high relief catchments, but was less successful when applied to lower-relief and/or groundwater-dominated areas.
The geomorphological study of alluvial plains takes great advantage from the integration of detailed altimetry with high-resolution images, especially in the lower-relief sectors, like those in the distal plain of the Brenta and Bacchiglione rivers near the city of Padua (mean slope 1 0.8‰).
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