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Sikhote-Alin Meteorite1947

Sikhote-Alin meteorite

Introduction

On the morning of February 12, 1947, the sky over eastern Russia lit up brighter than the Sun. At about 10:30–10:38 a.m. local time, people across the Sikhote-Alin mountains of Primorsky Krai witnessed a blinding fireball tearing across the winter sky, trailing a smoke plume that stretched for tens of kilometers.

Moments later, a thunderous series of explosions shook the taiga. The meteor, an enormous mass of metal from space, broke apart in a low-altitude airburst and rained thousands of iron fragments into the forest. Some pieces punched deep craters into the frozen ground, others embedded in trees, and countless smaller shrapnel fragments peppered the snow.

This event became known as the Sikhote-Alin meteorite fall—one of the largest and best-documented iron meteorite showers in modern history. Classified as a IIAB coarse octahedrite, Sikhote-Alin is not only a spectacular collector’s meteorite, but also a key object for understanding how metal-rich bodies move through the Solar System, break up in Earth’s atmosphere, and shape the surface through impact.


Scientific Background: Classification & Composition

Type & Group

The Sikhote-Alin meteorite is classified as:

  • Type: Iron meteorite
  • Group: IIAB
  • Structural class: Coarsest octahedrite (Ogg – very wide kamacite lamellae)

“Iron meteorite” means Sikhote-Alin is dominated by a nickel–iron metal alloy, rather than silicate minerals like most stony meteorites. The IIAB group is defined by characteristic concentrations of nickel, gallium, germanium, and iridium, and by its structural pattern when etched.

Chemical Composition

Average composition for Sikhote-Alin is approximately:

  • Iron (Fe): ~93%
  • Nickel (Ni): ~5.9–5.94%
  • Cobalt (Co): ~0.38–0.42%
  • Phosphorus (P): ~0.46–0.48%
  • Sulfur (S): up to ~0.28%

Trace elements (Ga, Ge, Ir, etc.) fit well within the IIAB chemical group and help tie Sikhote-Alin to a differentiated metallic core of an ancient parent body.

Structure & Microscopic Features

As a coarse octahedrite, Sikhote-Alin displays:

  • Very wide kamacite lamellae (α-Fe(Ni,Co)) when etched
  • Taenite (γ-FeNi) along lamella boundaries
  • Iron–nickel phosphides (rhabdites, (Fe,Ni)₃P) and sulfides (troilite, FeS) scattered within the metal matrix

Shock experiments and microstructural studies show that Sikhote-Alin fragments experienced:

  • Moderate shock pressures (up to ~12 GPa in some simulations) during atmospheric passage and impact, causing plastic deformation and subtle changes in metal texture.

This makes it an excellent example for students and collectors to observe the interplay of metallic crystallization, shock, and weathering all within one meteorite.


The 1947 Fall: Fireball, Airburst & Impact

The Fireball

On February 12, 1947, a large meteoroid—estimated at 90–100 tonnes pre-atmospheric mass—entered Earth’s atmosphere over the Sikhote-Alin mountain range in what was then the Soviet Union.

Witness accounts and later reconstructions indicate:

  • Apparent brightness: brighter than the Sun
  • Entry velocity: ~14 km/s (~50,000 km/h)
  • Entry angle: ~41° relative to the horizon
  • A smoke and dust train roughly 20–32 km long visible for hours after the event

The fall occurred in daytime, which is relatively rare for such a large iron event—and crucially, it meant many people saw and reported the fireball, giving scientists an unusually rich observational data set.

Airburst & Fragmentation

As the meteoroid descended into denser atmosphere:

  1. Ram pressure and heating caused the outer layers to ablate.
  2. Dynamic stresses built up within the metal core.
  3. At an altitude of roughly 5.6–6 km, the main body catastrophically fragmented in a powerful airburst.

This explosion:

  • Produced a shock wave that shattered windows and shook buildings over a wide area.
  • Created a shower of meteorite fragments, some still moving at extremely high speed when they hit the ground.
  • Was heard up to 200–300 km away.

Impact on the Ground

The fragmented iron rained down over an elliptical area of roughly 0.5–1.3 km², creating a dense strewn field.

Field studies found:

  • More than 120 craters and pits of various sizes
  • The largest crater: about 26–26.5 m across and ~6 m deep
  • Meteorites embedded in tree trunks and roots
  • Fragments buried as deep as 6 m (20 ft) in the ground

Later estimates suggest that ≥23 tonnes of post-atmospheric mass have been recovered, making Sikhote-Alin one of the largest iron meteorite showers ever documented.


Reconstructing the Orbit: From Asteroid Belt to Earth

Because the fall happened in full daylight and was observed by hundreds of people, Soviet astronomers were able to reconstruct Sikhote-Alin’s pre-impact orbit with unusual precision.

Using trajectory, brightness, and timing data, V. G. Fesenkov and colleagues concluded that:

  • The meteoroid followed an elliptical, low-inclination orbit around the Sun.
  • Its aphelion (furthest point from the Sun) lay within the asteroid belt, similar to many Earth-crossing asteroids.
  • The orbit was likely created by collisions within the asteroid belt that nudged a metal-rich fragment toward an Earth-crossing path.

In other words, Sikhote-Alin began as a piece of a differentiated parent body (a proto-asteroid or small planet), was liberated by a collision, and then traversed space for millions of years before its 1947 encounter with Earth.


Collector’s Notes: Forms, Aesthetics & Market Position

Two Main Morphologies

Sikhote-Alin is famous for producing two distinct types of specimens:

  1. Ablation (aerodynamic) forms
    • Smooth, sculpted surfaces
    • Beautiful regmaglypts (thumbprint depressions)
    • Orientation features like flow lines and rollover lips
    • These pieces likely separated early and melted extensively in the upper atmosphere.
  2. Shrapnel (fragmentation) forms
    • Jagged, torn, twisted metal
    • Sharp edges and shear planes
    • Evidence of mechanical breakup in the airburst and ground impact

Widmanstätten Pattern

When cut, polished, and etched, Sikhote-Alin slices reveal:

  • A coarse Widmanstätten pattern with broad kamacite lamellae
  • Visible troilite and phosphide inclusions
  • Sometimes cracks or shock features from the violent breakup

The coarseness of the pattern makes it a good teaching specimen, although it’s not as “fine lace” as Muonionalusta or Gibeon.

Why Sikhote-Alin Is a Classic Collector Meteorite

  • It’s a witnessed fall with a precise date, time, and location.
  • It produced dramatic sculptural individuals ideal for display.
  • There is enough material that small specimens are accessible, but not so much that it feels common.
  • Its 1947 date ties it to mid-20th-century history and Soviet science.

Higher-end collections often include multiple Sikhote-Alin pieces—natural individuals, shrapnel fragments, and at least one etched slice.


Stability, Rust & Care

Like all iron meteorites, Sikhote-Alin can rust if not cared for properly.

Factors Influencing Stability

  • Original exposure in a humid, forested environment means some pieces have pre-existing weathering.
  • Internal sulfides and phosphides (troilite, schreibersite, etc.) can act as corrosion centers if moisture penetrates.

Care Tips for Collectors & Buyers

  • Keep meteorites dry; store with silica-gel packets.
  • Avoid prolonged high humidity or temperature swings.
  • Lightly coat etched slices or exposed metal with microcrystalline wax or a recommended corrosion inhibitor.
  • For jewelry, expect some patina over time; wipe dry after wear and avoid saltwater or chlorinated pools.

Sikhote-Alin is not as notorious for instability as some irons, but careful storage aligns with your brand’s emphasis on long-term stewardship of natural specimens.


Metaphysical & Symbolic Perspectives

For your crystal-healing and metaphysical audience, Sikhote-Alin can be framed as:

Key Themes

  • Impact & transformation – A literal explosion of change from the sky
  • Courage & decisiveness – Symbolizing sudden shifts and breakthroughs
  • Grounding cosmic energy – Dense iron linking space with Earth’s core

Chakra Associations

Practitioners often associate iron meteorites with:

  • Root Chakra – grounding, physical presence, resilience
  • Solar Plexus – willpower, strength, personal agency

Some also work with meteorites for Third Eye / Crown meditation to contemplate cosmic scale and perspective, but Sikhote-Alin’s energy is usually described as very physical and intense.

Suggested Uses

  • Held during difficult decision-making to symbolize direct action and momentum
  • Placed on a desk or altar as a reminder of cosmic context and personal resilience
  • Used in grounding meditations for those who feel scattered or overwhelmed

Practical Uses: Education, Display & Jewelry

Education & Museum Displays

Sikhote-Alin is an outstanding teaching meteorite:

  • Impact physics: airbursts, fragment trajectories, crater formation
  • Iron meteorite structure: Widmanstätten patterns, inclusions, and group classification
  • Human observation: eyewitness reports, Soviet research, and orbital reconstruction

Home & Shop Display

Popular formats include:

  • Natural sculpted individuals on acrylic stands
  • “Shrapnel” fragments for a more dramatic, industrial aesthetic
  • Cut and etched slices mounted in frames or display cases

Jewelry & Wearable Art

Sikhote-Alin is sometimes used in:

  • Pendants featuring small sculpted individuals or polished slices
  • Inlaid rings or bracelets (often stabilized and sealed)
  • Pocket talismans or key fobs (small individual fragments)

As with other iron meteorites, jewelry buyers should be informed about:

  • Potential for patina and minor rust over time
  • Best practices: keep dry, occasional cleaning and resealing

Modern Relevance: Science, History & Collecting Ethics

Scientific Importance

Sikhote-Alin remains important for:

  • Studying coarse octahedrite structure and shock effects in iron meteorites
  • Understanding fragmentation of large irons in the atmosphere and the formation of multi-crater strewn fields
  • Providing a well-documented example for impact risk assessments—what happens if a large iron enters over a populated region?

Russia regulates access to meteorites, especially large or scientifically significant finds, but Sikhote-Alin:

  • Has been collected for decades
  • Exists in large quantity in older museum and private collections

Best practices for a responsible brand:

  • Source from established dealers with long-standing stock
  • Favor material with clear provenance (older Western or Russian collections, museum deaccessions, reputable importers)
  • Avoid encouraging fresh “digging runs” that may disturb protected sites or cultural landscapes

FAQs

1. What kind of meteorite is Sikhote-Alin?

Sikhote-Alin is an iron meteorite of group IIAB, structurally a coarsest octahedrite. It consists mostly of iron–nickel alloy with minor cobalt, phosphorus, sulfur, and trace elements like gallium and germanium.


2. When and where did it fall?

It fell on February 12, 1947, around 10:30–10:38 a.m., over the Sikhote-Alin mountains in Primorsky Krai, southeastern Russia, roughly 440 km northeast of Vladivostok.


3. How big was the original meteoroid?

Estimates suggest a pre-atmospheric mass of ~90–100 tonnes, making Sikhote-Alin one of the largest iron meteoroids ever seen to fall in recorded history. About 23 tonnes of metal are known to have reached the ground and been recovered.


4. How large is the strewn field and how many craters did it make?

The strewn field covers roughly 0.5–1.3 km², with more than 120 craters and pits, the largest about 26 m across and ~6 m deep.


5. Does Sikhote-Alin show a Widmanstätten pattern?

Yes. When cut, polished, and etched, Sikhote-Alin reveals a coarse Widmanstätten pattern typical of coarsest octahedrites, along with troilite and phosphide inclusions.


6. Is Sikhote-Alin safe to handle and wear?

Sikhote-Alin is mainly iron–nickel metal and is safe to handle. Like all iron meteorites, it can rust if damp. Jewelry pieces are usually stabilized and sealed, but owners should avoid moisture, saltwater, and harsh chemicals, and wipe pieces dry after wear.


7. Is Sikhote-Alin rare?

Sikhote-Alin is not as rare as small, single-find irons, but it is historically important and finite. There is a healthy supply of small individuals and shrapnel fragments, while large, sculptural pieces with provenance are considered more collectible and command higher prices.


Conclusion

The Sikhote-Alin meteorite is a perfect example of why meteorites capture the human imagination. It combines:

  • A spectacular witnessed event—a daytime iron fireball and airburst over Siberia
  • Rich scientific value, revealing details about iron meteorites, planetary cores, and atmospheric fragmentation
  • Strong collector appeal, from sculpted regmaglypted individuals to etched slices
  • Deep symbolic meaning, tying together impact, transformation, and cosmic context

Like this topic, read our meteorite articles TatahouineMarsLunarPallasitesMeteorite Classification-Science, Campo Del Ceilo. Shop your favorite Meteorites. Check our free E Book Library for deeper dives on specific topics.

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Grounded Lifestyles

At Grounded Lifestyles, our love for crystals began in the peaceful flow of Reiki and energy healing sessions — where we saw how natural stones could amplify intentions, restore balance, and bring comfort. But the more time we spent with these treasures, the more curious we became about their origins. That curiosity led us into the fascinating world of geology and mineral specimen collecting. We fell in love not just with the energy of crystals, but with the science and artistry of their creation — the intricate crystal structures, the vibrant mineral hues, and the wonder of holding a piece of Earth’s history in our hands.

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