Visualisation
Every recorded meteorite landing on Earth
32,187 space rocks with known coordinates, plotted as a single dot per strike. The continents draw themselves — but the densest clusters aren't where you'd expect.
NASA's Meteorite Landings dataset is a list of every meteorite humans have officially recorded — 32,187 of them with known coordinates, mass, mineralogical class, and date of fall or discovery. Plot every one on a world map and you get a strange portrait: the continents emerge from the dots, but the density is wildly uneven.
Why Antarctica looks like a strike zone
It isn't. Antarctica receives roughly the same meteorite flux per square kilometre as anywhere else on Earth — but two things make it the world's best meteorite-hunting ground. First, dark rocks lying on white ice are easy to spot from a distance. Second, the slow flow of the ice sheet concentrates meteorites into "stranding zones" — patches of blue ice near mountains where embedded rocks rise to the surface. The Allan Hills Main Ice Field alone has yielded thousands of specimens. So that cluster is really a record of human searching, not space's bias.
"Fell" vs "Found"
Each record is tagged either Fell (someone saw it land) or Found (it was discovered later, no observed arrival). The split is dramatic: 1,107 witnessed falls versus 44,609 found specimens. Witnessed falls are scientifically more useful — you know exactly when the rock arrived — but they're a tiny fraction of what's out there.
The biggest pieces
Most meteorites are small — gram-scale pebbles. A handful are tons. Here are the ten heaviest individual specimens on record:
| Name | Mass | Year | Coordinates |
|---|---|---|---|
| Hoba | 60,000,000 g | 1920 | -19.6°, 17.9° |
| Cape York | 58,200,000 g | 1818 | 76.1°, -64.9° |
| Campo del Cielo | 50,000,000 g | 1575 | -27.5°, -60.6° |
| Canyon Diablo | 30,000,000 g | 1891 | 35.0°, -111.0° |
| Armanty | 28,000,000 g | 1898 | 47.0°, 88.0° |
| Gibeon | 26,000,000 g | 1836 | -25.5°, 18.0° |
| Chupaderos | 24,300,000 g | 1852 | 27.0°, -105.1° |
| Mundrabilla | 24,000,000 g | 1911 | -30.8°, 127.5° |
| Sikhote-Alin | 23,000,000 g | 1947 | 46.2°, 134.7° |
| Bacubirito | 22,000,000 g | 1863 | 26.2°, -107.8° |
The undisputed champion, Hoba, is a single 60-ton iron-nickel meteorite that landed in what's now Namibia roughly 80,000 years ago. It was discovered in 1920 by a farmer plowing his field — he heard a metallic scrape and dug down to find a refrigerator-sized block of nickel-iron. It's never been moved, and at 60 tons it's the largest single piece of natural iron ever found at Earth's surface.
The shape of the data
| Total records | ~45,000 with coordinates |
|---|---|
| Observed falls | 1,107 |
| Later finds | 44,609 |
| Date range | ~860 CE (Nogata, Japan — recorded by Shinto priests) to present |
| Largest known | Hoba meteorite, ~60,000 kg |
Try it yourself
The CSV is small enough to load in any tool. Each row has a name, mass, class, year, and coordinates:
curl -O https://data.nasa.gov/docs/legacy/meteorite_landings/Meteorite_Landings.csv
# Quick: how many fell vs were found?
awk -F, 'NR>1 {print $6}' Meteorite_Landings.csv | sort | uniq -c