Sedimentary Rocks
Brockram Breccia - Cumbria
SKU: SEDROK-005
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Brockram Breccia specimens sourced from Hoff, Cumbria, UK. Breccia, a type of clastic sedimentary rock, is characterized by its coarse-grained and poorly sorted nature, containing large angular fragments embedded in a finer-grained matrix.
Brockram is a basal breccia, composed of cemented limestone and sandstone fragments originating from the Permian period. The Permian was the last period of the Paleozoic era and occurred approximately 299 - 251 million years ago.
These samples are available in various sizes and are presented in a white card tray along with accompanying information label.
Brockram is a basal breccia, composed of cemented limestone and sandstone fragments originating from the Permian period. The Permian was the last period of the Paleozoic era and occurred approximately 299 - 251 million years ago.
These samples are available in various sizes and are presented in a white card tray along with accompanying information label.
Description
Brockram Breccia specimens sourced from Hoff, Cumbria, UK. Breccia, a type of clastic sedimentary rock, is characterized by its coarse-grained and poorly sorted nature, containing large angular fragments embedded in a finer-grained matrix.
Brockram is a basal breccia, composed of cemented limestone and sandstone fragments originating from the Permian period. The Permian was the last period of the Paleozoic era and occurred approximately 299 - 251 million years ago.
These samples are available in various sizes and are presented in a white card tray along with accompanying information label.
Brockram is a basal breccia, composed of cemented limestone and sandstone fragments originating from the Permian period. The Permian was the last period of the Paleozoic era and occurred approximately 299 - 251 million years ago.
These samples are available in various sizes and are presented in a white card tray along with accompanying information label.
