A variety of
EisenkieselIn Spanish mineralogical literature, the name is traditionally used exclusively for the red-brown (hematite-included) variety of authigenic quartzes from continental gypsum-bearing marls of the Triassic Keuper formation. (They may also be found occasionally in younger Tertiary or Quaternary sediments, but in these cases the crystals were eroded out of the Keuper F.)
Two types are common: 1. Isolated biterminated crystals, 2. hedgehog-like spheroidal aggregates. Both characteristically occur as "floaters".