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leucothites

Leucothites are a mineral species described in mineralogical literature as pale, white to colorless silicate minerals that belong to the feldspathoid-related group. The name combines the Greek elements leukos, white, and lithos, stone, reflecting their characteristic light appearance.

Description and properties

Leucothites typically occur as short prismatic to tabular crystals or as fine-grained to compact masses. They

Chemistry and structure

The idealized chemical picture of leucothites involves a framework silicate with aluminum and alkali cations, commonly

Occurrence and associations

Leucothites have been reported from alkaline igneous and metasomatic settings, including nephelinite- and phonolite-related rocks, and

Locality and naming

The genus name commemorates the pale appearance, with the type locality associated with the Leucoth Range region.

See also

Leucite, Feldspathoids, Silicate minerals.

exhibit
a
vitreous
to
pearly
luster
and
a
pale
to
colorless
body
color.
Crystal
systems
reported
for
leucothites
include
monoclinic,
with
imperfect
cleavage
and
a
conchoidal
to
uneven
fracture.
Hardness
is
generally
in
the
mid-range
(approximately
5
to
6
on
the
Mohs
scale),
and
measured
densities
fall
near
2.9
to
3.2
g/cm3.
The
mineral
displays
varying
optical
properties,
with
low
to
moderate
relief
and
refractive
indices
that
correspond
to
silicate
frameworks
with
alkali
cation
content.
showing
substitutions
among
Na+,
K+,
and
Ca2+
in
the
crystal
structure.
Iron
and
magnesium
can
substitute
for
aluminum
in
small
amounts,
and
trace
amounts
of
hydroxyl
may
be
present.
Leucothites
are
often
described
as
forming
in
environments
where
alkaline,
silica-oversaturated
fluids
interact
with
rocks,
yielding
a
light-colored,
low-density
silicate
phase.
in
pegmatitic
pockets
within
carbonatites.
They
are
typically
found
with
other
feldspathoid
minerals
such
as
nepheline
and
leucite,
along
with
calcite
and
quartz.
As
a
relatively
recent
addition
to
mineral
taxonomy,
leucothite
references
are
primarily
found
in
specialized
mineralogical
databases
and
descriptive
papers.