Olistolith (to the left) of the destructured red clay-marl

Alternation of red claystone, sandstone and marl of Gercus Formation at

Oleh HNYLKO Research profile

File:RED CLAY SOIL CAUSES MUCH OF THE SILTATION PROBLEM IN THE LAKE OF THE OZARKS REGION. ALONG ROUTE 54, SOUTHWEST OF - NARA - 551233.jpg - Wikimedia Commons

Olistolith (to the left) of the destructured red clay-marl sediments in

Olistolith - an overview

2-2 Clay Minerals – GEOL 2391 SW3: Course Units

Olistolith (to the left) of the destructured red clay-marl sediments in

Olistolith - an overview

PDF) GEOLOGICAL ENVIRONMENTS FORMING THE EOCENE BLACK-SHALE FORMATION OF THE SILESIAN NAPPE (UKRAINIAN CARPATHIANS)