×
Your Cart
Cart items
Cart is empty.
Fill your cart with amazing items
Shop Nowbdfg
$0.00
Shipping & taxes may be re-calculated at checkout
$0.00
Keep Shopping
Goethite PS Marcasite
Posted by: macadmin on 05.14.2020 | Filed under:

Goethite PS Marcasite

Specimen # 100909
Mineral: Goethite PS Marcasite
Location: Goethite Pseudomorph After Marcasite, White Desert, North of Farafra Oasis, Egypt
Size: 6.0 x 4.9 x 4.7 cm

Description

Detailed Description

A dramatic goethite pseudomorph after marcasite, this specimen features two groups of marcasite crystal-form spires, each radiating from a centre, joined together. In the centre and around the back (as I’d display this) there are small pseudomorphs after pyrite crystals. The marcasite crystal forms are sharp and well-defined. From above, the cross-sections of some of the spires are a litte reminiscent of Phillips-head screwdrivers, with crystal aggregates at right angles creating this shape. In excellent condition, no damage. In my view this piece looks best if supported to stand vertically – it is a high-impact piece, really jumps out from the dispay case.

Browse More White Desert Pseudomorphs


About These White Desert Pseudomorphs

This locality has been known for a number of years and pseudomorph specimens have come out once in a while. The pseudomorphs occur within the Cretaceous Khoman Chalk, from which the White Desert derives its name. Most crystals have typically been fairly indistinct, and to date sharp specimens have been uncommon. These specimens are remarkable for their relatively sharp marcasite crystal forms in aesthetic crystal clusters.

Over the years, these pseudomorphs have been variously labeled hematite, goethite and limonite (the latter no longer a valid mineral species name, but is a term still used in reference to unidentified iron hydroxides, so its use has not been incorrect). Recent work by Hannah Allen at Hamilton College has confirmed that the White Desert pseudomorphs are predominantly goethite. The small white grains lodged in among the crystal blades are barite, calcite and gypsum. (Allen, Hannah M., Pseudomorphed Mineral Aggregates of the Khoman Chalk, Western Desert, Egypt, Geological Society of America Abstracts with Programs. Vol. 46, No. 2, p.66 (2014)).

Although pseudomorphs after cubic and cuboctahedral pyrite crystals have also been found in the Khoman Chalk, the pseudomorphs after marcasite are more dramatic. These pseudomorphs are excellent specimens featuring beautiful marcasite crystal morphology, showing habits and forms exhibited by the crystallized marcasite specimens from the famous occurrences at Cap-Blanc-Nez, Pas-de-Calais, France.

Additional information

Dimensions 60 × 49 × 47 cm