Karren on laminar calcarenitic rock of Lagoa Santa (Minas Gerais, Brazil)
The form of the karren is dictated by the horizontal laminated beds and fissuring. They are dissected by characteristic rock forms that are traces of their development and current shaping. The permeable contacts between laminae and the vertical fissuring of the rock fostered a distinctive three-dimensional development of karren and with it unique forms.
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