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Typically a lineament will comprise a fault-aligned valley, a series of fault or fold-aligned hills, a straight coastline or indeed a
Kaynak: Lineament

The Olympic-Wallowa lineament (OWL) – first reported by cartographer Erwin Raisz in 1945 on a relief map of the continental United States
Kaynak: Olympic-Wallowa Lineament

The 38th parallel structures, also known as the 38th parallel lineament are a series of circular depressions or deformations stretching
Kaynak: 38th parallel structures

The Malvern Line or Malvern Lineament is the name applied to a north-south aligned lineament which runs through the Malvern Hills of
Kaynak: Malvern Line

The Pernambuco fault or Pernambuco Shear Zone in northeastern Brazil is a splay fault radiating from the Transbrasiliano lineament
Kaynak: Pernambuco Fault

The Cribarth Disturbance is a geological structure forming a lineament which stretches across south Wales from Swansea up the Swansea
Kaynak: Cribarth Disturbance

Helens is a NE (045°) trending line (red) of Pleistocene (about 4 Ma) plug domes and a topographic lineament (followed in part by Highway
Kaynak: Puget Sound faults

The Sobral shear zone of the Transbrasiliano lineament is considered a continuation of this lineament. Pankhurst | 2008 | pp 58 The fit
Kaynak: Kandi Fault Zone

Indeed the feature can be seen as a significant lineament in aerial and satellite views of Wales. The Steep Belt effectively marks the
Kaynak: Myddfai Steep Belt

The Sobral fault is a major fault in the Borborema geological province of northeastern Brazil , a part of the Transbrasiliano lineament .
Kaynak: Sobral Fault

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