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5.6" Tall, Polished Septarian Bookends - Madagascar
This is a pair of bookends made from a cut & polished septarian formation. The septarian comes from the Betsiboka Region of Madagascar and was deposited during the Jurassic period.
The edges of the bookends have been lined with felt and the base has round rubber "feet" to prevent scratching of the display surface. Each bookend varies slightly in size, with one measuring 5.6" tall, 3.85" wide and 3.55" thick while the other is 5.6" tall, 4.1" wide and 3.7" thick.
The edges of the bookends have been lined with felt and the base has round rubber "feet" to prevent scratching of the display surface. Each bookend varies slightly in size, with one measuring 5.6" tall, 3.85" wide and 3.55" thick while the other is 5.6" tall, 4.1" wide and 3.7" thick.
About Septarian
Septarian or septarian nodules are concretions containing angular cavities or cracks, called "septaria", filled with calcite and aragonite. A concretion is a hard, compact mass of rock that often forms around decaying organic matter. In the case of septarian nodules, the concretions formed around decaying sea life in a marine environment.
The exact mechanism for how the cracks form in the concretions is a mystery. One possible mechanism is the dehydration of the clay-rich core of a concretion, causing it to shrink and crack. The cracks could also be caused by gas expansion produced by the decaying organic matter within a concretion. Earthquakes have also been suggested as yet another mechanism.
The cracks in the concretions are then filled in with minerals such as calcite (yellow), aragonite (brown), and sometimes pyrite, causing very interesting patterns. They have often been described as looking like dragon's skin. They are frequently found as geodes with hollow, calcite crystal-filled cavities. More rarely, the fossils that originally started the formation of the concretion are still preserved in the septarian.
Septarian or septarian nodules are concretions containing angular cavities or cracks, called "septaria", filled with calcite and aragonite. A concretion is a hard, compact mass of rock that often forms around decaying organic matter. In the case of septarian nodules, the concretions formed around decaying sea life in a marine environment.
The exact mechanism for how the cracks form in the concretions is a mystery. One possible mechanism is the dehydration of the clay-rich core of a concretion, causing it to shrink and crack. The cracks could also be caused by gas expansion produced by the decaying organic matter within a concretion. Earthquakes have also been suggested as yet another mechanism.
The cracks in the concretions are then filled in with minerals such as calcite (yellow), aragonite (brown), and sometimes pyrite, causing very interesting patterns. They have often been described as looking like dragon's skin. They are frequently found as geodes with hollow, calcite crystal-filled cavities. More rarely, the fossils that originally started the formation of the concretion are still preserved in the septarian.
SPECIES
Septarian
LOCATION
Ambondromamy, Betsiboka Region, Madagascar
SIZE
5.6 x 3.85", up to 3.55" thick
CATEGORY
ITEM
#152427
