# django_session

session_key: kw1qtmqhrcor8e4m3dh3jnk6md4dgi2q
expire_date: 2013-08-10 12:00:15.980443
session_data:
  MTcwNjRmNGI3ZDgwYzc3Zjc5NmQzZDhmMThlNzdiNDVjODYwYzBjYTqAAn1xAShVEl9hdXRoX3VzZXJfYmFja2VuZHECVSlkamFuZ28uY29udHJpYi5hdXRoLmJhY2tlbmRzLk1vZGVsQmFja2VuZHEDVQ1fYXV0aF91c2VyX2lkcQRLAXUu


session_key: y9xdgeg6wziok1bbmpc89f9pputvwaf8
expire_date: 2013-11-26 01:06:55.904386
session_data:
  NTYwYWQ5N2ZmZmJhNWMzMmVhZjhjNDhmODgyYmI0MjhmMzUyNmRkMTqAAn1xAShVEl9hdXRoX3VzZXJfYmFja2VuZHECVSlkamFuZ28uY29udHJpYi5hdXRoLmJhY2tlbmRzLk1vZGVsQmFja2VuZHEDVQ1fYXV0aF91c2VyX2lkcQRLAnUu


# three_d_viewer_sample

model_filename: olivine.ctm
name: Olivine
description:
  A solid solution exists between the magnesium(Forsterite) and iron (Fayalite) end members. Due to the differing chemical composition, some of the properties also vary.


# three_d_viewer_mineral

streak: White
habit: Prismatic or massive
lustre: Vitreous/Transparent
colour: Colourless, white, milky. Uncommonly purple, pink, yellow, brown, black
cleavage_fracture: Conchoidal fracture, no cleavage
identifying_features: Hardness, lack of cleavage, conchoidal fracture, lustre
crystallography: Hexagonal (rhombohedral)
chemical_formula: SiO2
occurance:
  Common in sedimentary, igneous and metamorphic rocks. It is the primary mineral in quartzite and most sandstones, and occurs in all silicic igneous and metamorphic rocks.


streak: White(forsterite), white yellow(fayalite)
lustre: Vitreous
colour: Colourless, green, yellow
cleavage_fracture: Poor cleavage(010 and 100), conchoidal fracture
identifying_features: Glassy Lustre, conchoidal fracture, typical olive-green colour
crystallography: Orthorhombic
chemical_formula: (Mg, Fe, Mn) SiO4
habit:
  Typically granular. Rarely a combination of prisms and dipyramids forming a tabular or lozenge shape

occurance:
  Foresterite is commonly found in mafic and ultramafic rocks, and also commonly found in metamorphic rocks. Fayalite is found in iron-rich granitic igneous or metamorphic rocks. 


streak: White
habit: Masses or subhedral grains are the most common form. Exhibits polysynthetic twinning.
lustre: Pearly, vitreous
colour: White, gray, green
cleavage_fracture: Perfect (001), good (010), poor (110)
identifying_features: Cleavage, hardness, luster, and polysynthetic twinning
crystallography: Triclinic
chemical_formula: CaAl2Si2O8 (Anorthite) – NaAlSi3O8 (Albite)
occurance:
  It is the most abundant mineral in the Earth’s crust. Common in igneous, metamorphic and young sedimentary rocks. 


