Base materials with high potential

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Very good materials

Best of the best

Best diamondoids

Best SiO2 polymorphs

Metastable ultrahard and dense SiO2 polymorphs:

Simple titanium gemstones

First row elements

  • TiB2 Titanium diboride - hexagonal 2D layered - 3230°C - 4.52g/ccm - optically metallic - highly refractory
  • TiC Titanium carbide - simple cubic - 3160°C (800°C in air) - 4.93g/ccm Mohs 9 to 9.5 - water insoluble (almost)
  • TiN Titanium nitride - simple cubic - 2,947°C - 5.21 g/cm3 - optically metallic (golden) - "barrier metal" - water insoluble (almost)

Second row elements:

Titanium oxides:

  • TiO [1] - simple cubic - 1,750C° - 4.95g/ccm - optically metallic (golden)
  • Ti2O3 [2] - tristarite - hexagonal corundum structure (like sapphire) - 2,130°C (decomposes) - 4.49g/ccm - semiconducting to metallic at 200°C
  • TiO2 [3] - rutile, anatase, brookite, and more

Quite simple rutile structure & Hard

Neo-polymorphs with rutile structure
See: the stishovite continuum currently on the page about silicon
Silicon group: GeO2, SnO2, β-PbO2
Other: MnO2, FeSbO4

Mono metal monoxides (simple cublic NaCl salt structure)

Earth alkali based

  • MgO periclase
  • CaO - questionable - highly reactive with water

Transition metal based

Some transition metal monoxides (Typical: Max 1300-1900°C - Mohs 5-6)

  • TiO hongquiite
  • MnO manganosite - (Mn is less abundant)
  • FeO wüstite
  • NiO brommelite - (Ni is not too abundant on earth but very abundant on metallic asteroids)

V vanadium, Cr chromium, Co cobalt do that too but
these elements are more scarce thus
not included as pure high volume base materials here

Other

  • spinell MgAl2O4 - very hard and cubic

Quite good materials with some hampering weakness(es)

Con: low crystal structure symmetry

Con: Rather soft materials

Others

  • garnets - hard and cubic (but big unit cell)
  • brommelite BeO - very hard but beryllium is scarce and poisonous