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The Triassic Lowlands represent an ancient normal fault landscape within the Appalachian Mountains.
Most of the landscape is less than 12 million years old but older relict landscapes persist including a subduction zone landscape, and a Basin and Range-type normal fault landscape.
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This chapter describes normal fault-dominated landscapes, which include the Basin and Range, the Rio Grande rift, and the Triassic Lowlands.
It is not Mr. Jarrold's fault that this landscape has been so heavily trodden over by others.
These active normal faults include WNW to E W and NE to ENE-trending faults affect the landscape and generate basin and range topography within the Beotia.
The faults affected the landscape and had important role the forming of the present drainage system.
To better understand the evolution of collision-related topography, we present the results of a geomorphological study in which elevation changes generated by reactivated pre-Alpine (Variscan and Triassic–Jurassic) faults drive a landscape evolution model.
In the Aegean's karstic landscape earthquake fault scarps act as limestone ramparts on which fortifications, citadels and acropoli were constructed, and underlying fault lines were preferred pathways for groundwater movement and egress.
Our trip south would lead through the Cascadia subduction zone, then down the line of the San Andreas fault, through a crumpled landscape of fracture, rift and upheaval.
Ms. Thomas has translated its pair of embracing women — a blonde and a brunette — into a dark-skinned black woman and a light-skinned one, transporting them from a silken bed to an Edenic landscape whose fault lines are highlighted in fluorescent orange.
For the LCMF (number 1 in Fig. 1), although this fault system has remarkable landscape feature based on studies of aerial photographs, the evidence of separation in strata is absence in the field (Sun 1971).
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