Microcline var. Amazonite

Object/Artifact

-

Crater Rock Museum

Name/Title

Microcline var. Amazonite

Entry/Object ID

2009.62.134

Description

Chemical Composition: Potassium aluminum silica Crystal System: Triclinic System Description: Common Name: Microcline Chemistry: KAlSi3 O8 , Potassium aluminum silicate. Group: Feldspars Location: Lake George.CO Description: Small group of large crystals with relatively smooth faces and a blue-green color with some areas of tan and brown. PHYSICAL CHARACTERISTICS: Color is usually off-white,yellowish, flesh pink, brown or green. Luster is vitreous to sometimes pearly or dull if weathered. Transparency crystals are translucent, but usually translucent to opaque. Crystal System is triclinic; bar 1 Crystal Habits include blocky, or tabular crystals. Crystals have a nearly rectangular or square cross-section with slightly slanted dome and pinacoid terminations. Twinning is common. Crystals can be twinned according to the Albite, Pericline, Carlsbad, Manebach and Baveno laws. Microcline can be found as a major rock forming component in granites, syenites and in metamorphic gneisses. Cleavage is perfect in one and good in another direction forming nearly right angled prisms. Fracture is conchoidal. Hardness is 6 - 6.5. Specific Gravity is approximately 2.5 (average) Streak is white. Associated Minerals are quartz, muscovite and plagioclase feldspars. Other Characteristics: Lamellar twinning may cause a grooved effect on cystal and cleavage surfaces that appear as striations. Perthite intergrowths causes a stripped appearance is some specimens. Best Field Indicators are occurence, twinning, color and luster. Fracture: conchoidal Hardness: 6 Orthoclase Luster: Vitreous Occurrence: IIt is common in granite and pegmatites. Microcline forms during slow cooling of orthoclase; it is more stable at lower temperatures than orthoclase. Sanidine is a polymorph of alkali feldspar stable at yet higher temperature. Microcline may be clear, white, pale-yellow, brick-red, or green; it is generally characterized by cross-hatch twinning that forms as a result of the transformation of monoclinic orthoclase into triclinic microcline. Rock Type: Sedimentary Specific Gravity: 2.5 Streak: white

Collection

RAGM Mineral Collection

Acquisition

Accession

2009.62

Source or Donor

Museum Collection of Minerals

Acquisition Method

Donation

Dimensions

Width

4-3/4 in

Depth

1-1/2 in

Length

3-1/4 in

Weight

0.64 oz

Location

Location

* Untyped Location

DS-11

Room

Delmar Smith Hall

Building

Crater Rock Museum

Category

Exhibit

Moved By

Ian C.

Date

January 21, 2025

Notes

USA Case Installation

Location

Display Case

FS-3

Room

Frieda Smith Hall

Building

Crater Rock Museum

Category

Permanent

Date

August 18, 2023