IRON-NICKEL

  • Chemistry: Fe-Ni, Elemental Iron-nickel
  • Class: Elements
  • Group: Iron
  • Uses: as a mineral specimen and scientific studies.
  • Specimens

Native Iron is quite often a misnomer as natural iron is not necessarily "native" to Earth since it rarely occurs on the Earth's surface by terrestrial processes. It is mostly found in the form of meteorites that have impacted the Earth's surface. A few rare terrestrial gabbros and sulfide deposits do contain elemental iron-nickel deposits, these are the only truly native iron-nickel. All natural iron, whether it is native or meteoritic, is actually an alloy of iron and nickel. The two elements are combined in varying percentages from less than 6% nickel to as much as 75% nickel, although iron is by far more common than nickel.

The meteorites that contain iron-nickel crystals are fascinating in their possible origins and diversity. In the early solar system, asteroids and comets sometimes grew large enough to be considered planetary embryos (objects hundreds of kilometers in diameter, including the four largest remaining asteroids). These bodies were large enough to differentiate, even to melt due to the heat of formation and the decay of radioactive isotopes. This melting allowed the dense iron and nickel to sink to form a metallic core. At one point, there were at least tens of thousands of these planetary embryos, and they began to collide to form the planets. Some of the more violent collisions shattered the embryos, scattering fragments of their iron/nickel cores around the solar system (these fragments still comprise about 10% of all known asteroids). Different parent embryos would have resulted in meteorites of different compositions.

Meteorites are very diverse and even novice collectors can distinguish samples from different known meteorites by their unique character. Often these meteorites have inclusions of large crystals of other minerals such as olivines or pyroxenes, etc or the iron has a unique crystal pattern that is characteristic. The characteristic Widmanstatten patterns (revealed by polishing then acid-etching a slice of the meteorite) reflect the specific nickel-iron ratio and the rate of cooling of the host body and are effectively the fingerprint of an iron meteorite.

Due to the nature of iron, care should be used in the preserving of valuable iron-nickel samples. Rust is iron's worst enemy and it is recommended to store iron samples with a dehydrating agent (dessicant). Most iron meteorites are found using metal detectors in desert areas. Any dense natural (non-man-made) metal object is likely to be an iron meteorite, and they are primarily found in the desert because they last longer before rusting away. Still, they do rust, they are found entombed in rust, and the lovely metallic meteorites available here and elsewhere have been cleaned to remove the original surface rust. Surface oxidation at high temperature (aero braking) often results in coatings of the black iron oxide, magnetite.

PHYSICAL CHARACTERISTICS:

  • Color is steel gray or black.
  • Luster is metallic.
  • Transparency is opaque.
  • Crystal System is isometric; 4/m bar 3 2/m
  • Crystal Habits crystal form is extremely rare, when etched, meteoritic examples may show interesting and complicated intergrowths of crystals according to different nickel-iron concentrates. Terrestrial samples are massive and appear as small flakes and irregular masses. Meteoritic samples are usually rounded, pitted and irregular.
  • Cleavage is absent but crystals will have distinct parallel partings.
  • Fracture is hackly.
  • Streak is gray metallic.
  • Hardness is 4-5
  • Specific Gravity is 7.3-7.8 (heavy even for metallic)
  • Other Characteristics: malleable, strongly attracted to magnets.
  • Associated Minerals are olivine, pyroxenes, and some minerals that are only found in meteorites. In terrestrial samples it is found with gold and platinum and with sulfide ores.
  • Notable Occurrences for meteoritic iron are best found in Antarctica, where meteorites are easy to spot against a background of snow and ice. Many specimens are found in Diablo Canyon, Arizona, USA; and in Gibbeon, Hoba, Namibia. Also Meteor Crater (Barringer Crater), Arizona, USA; Australia; Poland and elsewhere. For terrestrial iron, good specimens can be found in the Kola Pennisula, Russia; Disco Island, Greenland; Kassel, Germany and New Zealand.
  • Best Field Indicators are color, malleability, attraction to magnets and forms. Of course, when hunting for iron meteorites, a metal detector is the perfect tool.
This Site Awarded
Available IRON specimens:
IRON specimen IRO-24
$2000.00 -5% = $1900.00
Dims: 6.5 x 5.0 x 4.5" (16.0 x 12.6 x 11.5 cm) .... Wt: 7.5 lbs. (3.4 kg) .... Loc: Nantan County, Guangxi, China
This is a wonderful specimen of the Nantan Meteorites, which fell to earth in May of 1516. These meteorites (first identified in 1958) were scattered over a 200 square kilometer area. Nantans fell in a humid region, and most specimens are heavily corroded. Once cleaned, however, specimens such as this one exhibit an octahedral crystal Widmanstatten pattern as surface features. This specimen is extremely impressive, as it shows an unusual "out of this world" and very aesthetic shape. Nantan meteorites are known to rust easily, and should be sprayed with a rust inhibitor (such as WD-40) every year or so.
no photo
IRO-24
$1900.00
no photo
IRON specimen IRO-37
$ 140.00 -10% = $ 126.00
Dims: 2.00x1.44x0.47" (5.09x3.67x1.21cm) .... Wt: 2.30oz (65.2g) .... Loc: Gibbeon desert, near Hoba, Namibia
This is an end slice of a Gibbeon meteorite, plus it has cuts on two more sides (the three cuts meet at right angles). At one time, all three cut faces had been polished and etched to show their Widmanstatten pattern, but the largest surface had been "cleaned" which removed the pattern.
no photo
IRO-37
$ 126.00
no photo
IRON specimen IRO-47
$ 125.00 -10% = $ 112.50
Dims: 3.32x2.21x0.86in (8.44x5.62x2.18cm) .... Wt: 6.4oz (180g) .... Loc: near Dalnerechensk, Marytime territory, Far East Russia
Another piece of Sikhote-Alin shrapnel, this one is essentially a single shard, and lightly shows ablation lines recording its fiery descent through the atmosphere.
no photo
IRO-47
$ 112.50
no photo
IRON specimen IRO-45
$ 125.00 -20% = $ 100.00
Dims: 2.28x1.25x0.44in (5.79x3.17x1.12cm) .... Wt: 2.38oz (67.4g) .... Loc: Sikhote-Alin, Russia
Being relatively thin, this specimen displays a lot of meteorite for the weight. The surface has multiple pits and other features suggestive of a high-speed transit through the air.
no photo
IRO-45
$ 100.00
no photo
IRON specimen IRO-48
$ 40.00 -20% = $ 32.00
Dims: 1.89x1.47x0.57in (4.81x3.72x1.45cm) .... Wt: 2.17oz (61.4g) .... Loc: Sikhote-Alin, Russia
This is clearly a piece of meteoric shrapnel resulting from a high-altitude (overpressure induced) explosion of a large iron meteor. The piece shows little sign of ablation, and is relatively flat.
no photo
IRO-48
$ 32.00
no photo
IRON specimen IRO-53
$ 90.00 -20% = $ 72.00
Dims: 2.36x1.79x0.45in (6.00x4.55x1.15cm) .... Wt: 3.07oz (87.0g) .... Loc: Sikhote-Alin, Russia
Another example of Sikhote-Alin meteorite shrapnel, this specimen appears to have been treated with a rust inhibitor (likely phosphoric acid). It is in excellent shape, and looks like one expects an iron meteorite to look. The front surface is covered by a large number of nearly parallel lines which add visual interest.
no photo
IRO-53
$ 72.00
no photo
see this List of ALL specimens including SOLD ones
 

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