Mineral identification chart you narrow down with home tests
Tell the chart what your stone does with a nail, a tile, a magnet and vinegar, and it narrows 49 common minerals and rocks. Free and printable.
Test your stone with things from home (a fingernail, a coin, a steel nail, a tile, a magnet and vinegar), then tick what happened. This mineral identification chart narrows 49 common minerals and rocks to the ones that fit and suggests the next test. Colour is the least reliable clue, so don't rely on it alone.
49 matches
What this chart can't tell you. It can't confirm a gemstone, say whether a stone or crystal is real, or put a value on anything. For those, ask a jeweller or a gem lab. It can't confirm a meteorite either. The finds most often mistaken for meteorites are iron-oxide lumps and slag from old industry, so take a heavy, magnetic stone to a museum or a university geology department.
The mineral and rock identification chart
All 49 minerals and rocks. Rows that don't fit your answers fade out. Hardness is on the Mohs scale: fingernail 2.5, copper 3, steel nail 5 to 5.5, glass 5.5.
| Name | Colour | Streak | Hardness | Shine | Magnet | Vinegar | Breaks | Weight | The giveaway |
|---|---|---|---|---|---|---|---|---|---|
| Quartzmineral | White, grey, pink, purple, yellow, brown, black | White or none | 7 | Glassy, greasy | No | No | Shell-like | Average | Scratches glass easily and breaks with curved, shell-like edges, never flat faces. |
| Chalcedonymineral | White, grey, blue, brown, red, orange, yellow, green, black | White or none | 6.5 to 7 | Greasy, dull | No | No | Shell-like | Average | Quartz in grains too fine to see, with a waxy shine. Agate shows bands, jasper is opaque red, brown or yellow. |
| Potassium feldsparmineral | White, pink, orange, grey, yellow, green | White or none | 6 to 6.5 | Glassy, pearly | No | No | Flat faces, rough | Average | The pink or cream blocky crystals in granite. Two flat breaking faces at right angles, and too hard for a steel nail. |
| Plagioclase feldsparmineral | White, grey, blue, green, brown | White or none | 6 to 6.5 | Glassy, pearly | No | No | Flat faces, rough | Average | Like potassium feldspar but white to grey, often with fine parallel lines on its flat faces. Labradorite flashes blue. |
| Calcitemineral | White, grey, yellow, green, orange, brown, pink, blue | White or none | 3 | Glassy, pearly | No | Fizzes | Slanted blocks | Average | Fizzes in vinegar, a steel nail scratches it, and it breaks into slanted blocks. Clear pieces show a doubled image. |
| Dolomitemineral | White, yellow, brown, pink, grey | White or none | 3.5 to 4 | Glassy, pearly | No | Weak or none | Slanted blocks | Average | Looks like calcite but barely reacts to vinegar unless you scratch some into powder first. Crystals often have curved faces. |
| Gypsummineral | White, grey, yellow, brown, pink, red | White or none | 1.5 to 2 | Glassy, pearly, silky | No | No | Thin sheets, fibres | Light | So soft your fingernail leaves a mark. Clear sheets bend without springing back. |
| Halitemineral | White, grey, pink, orange, red, blue, purple, yellow | White or none | 2 to 2.5 | Glassy | No | No | Cubes | Light | Breaks into cubes and dissolves in a glass of water. |
| Fluoritemineral | White, purple, blue, green, yellow, orange, pink, brown, black | White or none | 4 | Glassy | No | No | Flat faces | Average | Often cubes, but the corners break off as flat triangles. A steel nail scratches it, copper doesn't. |
| Barytemineral | White, grey, yellow, brown, pink, blue | White or none | 3 to 3.5 | Glassy, pearly | No | No | Flat faces | Heavy | Pale and glassy like calcite, but noticeably heavy for its size and no fizz. |
| Muscovite micamineral | White, grey, brown, green, yellow, pink | White or none | 2.5 to 3 | Glassy, pearly, silky | No | No | Thin sheets | Average | Peels into clear, paper-thin sheets that spring back when bent. |
| Biotite micamineral | Black, brown, green | White or none | 2.5 to 3 | Glassy, pearly, metallic | No | No | Thin sheets | Average | Black or brown flakes that peel into thin sheets. The dark sparkles in granite. |
| Talcmineral | White, green, brown, grey | White or none | 1 | Pearly, greasy, dull | No | No | Thin sheets, rough | Average | Feels soapy, and a fingernail scratches it with no effort. The softest mineral on the Mohs scale. |
| Chloritemineral | Green | White or none, green | 2 to 2.5 | Pearly, greasy, dull | No | No | Thin sheets | Average | Green flakes like a soft mica, but they bend and stay bent. |
| Serpentinemineral | Green, white, yellow | White or none | 2.5 to 3.5 | Greasy, silky, dull | No | No | Shell-like, fibres, rough | Average | Mottled green with a waxy, soapy feel. Some kinds are fibrous asbestos, so don't scrape or crush fibres. |
| Graphitemineral | Black, silver-grey | Grey to black | 1 to 2 | Metallic, dull | No | No | Thin sheets | Light | Writes on paper like a pencil and feels greasy. Light for a metallic-looking mineral. |
| Pyritemineral | Brassy gold | Grey to black | 6 to 6.5 | Metallic | No | No | Shell-like, rough | Heavy | Pale brassy cubes with a greenish-black streak. Too hard for a steel nail, while real gold is soft and leaves a gold streak. |
| Chalcopyritemineral | Brassy gold, blue, purple | Grey to black | 3.5 to 4 | Metallic | No | No | Rough | Heavy | Deeper yellow than pyrite, often with a rainbow tarnish, and a steel nail scratches it. |
| Galenamineral | Silver-grey | Grey to black | 2.5 to 2.75 | Metallic | No | No | Cubes | Heavy | Bright silver cubes that are very heavy for their size. Wash your hands after handling it. |
| Sphaleritemineral | Brown, yellow, black, red, green, white | Yellow-brown, white or none | 3.5 to 4 | Greasy, glassy | No | No | Flat faces | Heavy | Resin-like brown or black with many flat shiny faces, and a pale yellow-brown or white streak. |
| Hematitemineral | Silver-grey, black, red, brown | Red-brown | 5 to 6 | Metallic, dull | No | No | Rough | Heavy | Red-brown streak even when the stone itself is shiny black or grey. Heavy. |
| Magnetitemineral | Black | Grey to black | 5.5 to 6.5 | Metallic, dull | Yes | No | Rough | Heavy | A fridge magnet sticks to it. Black streak and heavy. |
| Goethitemineral | Brown, yellow, black, orange | Yellow-brown | 5 to 5.5 | Metallic, dull, silky | No | No | Rough, fibres | Heavy | Rusty brown with a yellow-brown streak. Earthy limonite crusts are softer than the crystals. |
| Pyrrhotitemineral | Brassy gold, brown | Grey to black | 3.5 to 4.5 | Metallic | Weak | No | Rough | Heavy | Bronze, tarnishes fast, and pulls weakly towards a strong magnet. |
| Malachitemineral | Green | Green | 3.5 to 4 | Glassy, silky, dull | No | Weak or none | Rough, fibres | Average, heavy | Bright green, often in bands, with a pale green streak. A copper mineral. |
| Azuritemineral | Blue | Blue | 3.5 to 4 | Glassy | No | Weak or none | Rough, shell-like | Heavy | Deep blue with a pale blue streak, often found with malachite. |
| Garnetmineral | Red, brown, black, purple, orange | White or none | 6.5 to 7.5 | Glassy, greasy | No | No | Shell-like, rough | Average, heavy | Dark red ball-shaped crystals with many faces, often sitting in schist. Scratches glass. |
| Olivinemineral | Green, yellow, brown | White or none | 6.5 to 7 | Glassy | No | No | Shell-like | Average | Bottle-green glassy grains, often in lumps inside dark basalt. |
| Hornblendemineral | Black, green, brown | White or none | 5 to 6 | Glassy, pearly | No | No | Flat faces | Average | Black, long crystals with two flat breaking faces at a slant (about 56 and 124 degrees). |
| Augitemineral | Black, brown, green | Green, white or none | 5.5 to 6 | Glassy, dull | No | No | Flat faces | Average, heavy | Like hornblende, but stubby, and its two flat faces meet at nearly a right angle. |
| Tourmalinemineral | Black, brown | White or none | 7 | Glassy, greasy | No | No | Shell-like, rough | Average | Black, long crystals with fine grooves along their length and a rounded triangle shape end-on. Common in granite. |
| Apatitemineral | Green, blue, purple, pink, yellow, brown, white | White or none | 5 | Glassy, greasy | No | No | Shell-like, rough | Average | Six-sided crystals right on the line of a steel nail: the nail scratches it only just. |
| Epidotemineral | Green, yellow, black | White or none | 6 to 7 | Glassy, pearly | No | No | Flat faces, rough | Average | Pistachio green, often as veins or crusts in darker rock. |
| Graniterock | Pink, grey, white | Not useful | 6 to 7 | Glassy | No | No | Rough | Average | Speckled with crystals big enough to see: glassy grey quartz, pink or white feldspar and black mica. |
| Basaltrock | Black, grey | Not useful | 5.5 to 6.5 | Dull | Weak | No | Rough | Average | Dark and fine-grained, sometimes with gas holes or green olivine lumps. Some basalt pulls weakly on a magnet. |
| Obsidianrock | Black, brown, red | Not useful | 5 to 5.5 | Glassy | No | No | Shell-like | Average | Natural black glass with razor-sharp curved edges. Thin edges let light through. |
| Pumicerock | White, grey | Not useful | Varies | Dull | No | No | Rough | Light | Full of tiny holes, like frozen foam. It floats in water. |
| Sandstonerock | Yellow, brown, red, grey, white | Not useful | Varies | Dull | No | Weak or none | Rough, flat slabs | Average | Gritty like sandpaper, with sand grains you can see. Grains may rub off on your fingers. |
| Mudstone and shalerock | Grey, black, brown, red | Not useful | Varies | Dull | No | Weak or none | Flat slabs, rough | Average | Smooth with no grains you can see. Shale splits into thin layers. |
| Limestonerock | Grey, white, yellow, brown | White or none | 3 to 4 | Dull | No | Fizzes | Rough | Average | Fizzes in vinegar and often holds fossil shells. |
| Chalkrock | White | White or none | 1 to 3 | Dull | No | Fizzes | Rough | Light, average | Soft white limestone that marks your fingers and fizzes in vinegar. |
| Flintrock | Black, grey, brown | Not useful | 6.5 to 7 | Glassy, greasy, dull | No | No | Shell-like | Average | Dark grey or black inside a white crust, with sharp, curved edges where it breaks. It forms in chalk. |
| Marblerock | White, grey, pink, green | White or none | 3 to 4 | Glassy | No | Fizzes | Rough | Average | Sugary sparkling crystals that fizz in vinegar. A steel nail scratches it. |
| Slaterock | Grey, black, purple, green | Not useful | Varies | Dull | No | No | Flat slabs | Average | Splits into thin, flat, smooth sheets. |
| Quartziterock | White, grey, pink | Not useful | 7 | Glassy | No | No | Rough, shell-like | Average | Looks like sandstone, but breaks through its grains, not around them, and scratches glass. |
| Schistrock | Grey, silver-grey, green, brown | Not useful | Varies | Pearly, glassy | No | No | Flat slabs | Average | Glittery with mica flakes lined up in wavy layers. Often has garnets in it. |
| Gneissrock | Grey, pink, white, black | Not useful | 6 to 7 | Glassy | No | No | Rough, flat slabs | Average | Granite-like crystals sorted into light and dark stripes. |
| Conglomeraterock | Brown, grey, red, yellow, white | Not useful | Varies | Dull | No | Weak or none | Rough | Average | Rounded pebbles cemented together in a sandy rock. |
| Coalrock | Black | Grey to black | Varies | Dull, glassy, metallic | No | No | Rough, shell-like | Light | Black, light for its size, and leaves a black or brown-black streak. Dirties your fingers. |
Minerals from the Handbook of Mineralogy (Mineralogical Society of America). Rocks from the Natural History Museum's guide to UK rocks. Print source: carbonado.app/whatstone/tools/mineral-identification-chart/
What you need for the tests
- The unglazed back of a white bathroom tile, for the streak.
- A steel nail and a glass jar or bottle, for hardness.
- A copper coin. In the UK, check it first (see below).
- A fridge magnet. Don't use a strong neodymium magnet, which pulls on plenty of ordinary rocks.
- White vinegar and a dropper or a straw.
- A plain pebble about the size of your find, to compare the weight.
The coin needs care. The Royal Mint says UK 1p and 2p coins have been copper-plated steel since September 1992, and a steel coin scratches like a nail, not like copper. Older bronze ones look identical, but a magnet won't pick them up. So hold your coppers to a magnet and use one that doesn't stick. A bit of copper pipe or thick copper wire works too.
Do the tests in this order
- Find or make a fresh surface. Weathered outsides hide the colour and the shine, so chip a corner if you can.
- Rub the stone hard across the back of the tile and look at the powder line, not the stone.
- Try to scratch it with your fingernail, then the copper, then the nail. Then see whether it scratches the glass. Wipe the mark with a wet finger, because soft powder can look like a scratch.
- Hold it near the magnet on a thread and watch for a pull.
- Put one drop of vinegar on a fresh surface and watch for a minute. If nothing happens, scratch a little powder and try the drop on that.
- Look at a broken edge. Thin sheets, cubes, slanted blocks and curved shell-like edges each point to a different group.
- Weigh it in your hand against the pebble.
Streak comes before scratching because the scratch test leaves marks. Vinegar comes late because the fizz is acid eating into the stone, so rinse it with water afterwards.
Which tests narrow it most
We counted how far each test cuts the chart's 49 entries, on average over every stone in it. How it breaks did the most. It left about 16. Colour left about 19, but colour is also the test most likely to mislead. Quartz alone comes colourless, pink, purple, yellow, brown or black, according to the Handbook of Mineralogy, depending on what's trapped inside it.
Scratch and weight each left about 26, and streak about 28. Streak looks weak only because 23 of the 33 minerals leave a white streak, and rocks rarely give a useful one. When a streak does have colour, it's one of the strongest clues you'll get. Hematite leaves a red-brown streak even when the stone itself is shiny black.
The magnet left about 46, because so few things here react. But when a fridge magnet does pull, the list drops to 3.
Reading the scratch test
The tools have rough Mohs hardness values. A Texas A&M International University lab guide puts a fingernail at 2.5 and a steel nail at about 5, with most pocket knives at 5 to 5.5. Western University's guide puts copper at 3 and a glass plate at 5.5. Sources disagree by half a step, and so do real nails and coins.
So the chart lets its scratch bands overlap a little. Calcite is hardness 3, right on the copper line, and it stays in the list whether you say the coin scratched it or not. If one of your answers was wrong, the chart also shows near misses: stones that fit everything except one test, with a note saying which.
Print the chart for a class
Print the chart prints all 49 rows, in landscape. Each row has every property and the giveaway, and the rest of the page stays off the paper. Faded rows print at full strength. Minerals are taken from the Handbook of Mineralogy, published by the Mineralogical Society of America, and rocks from the Natural History Museum's guide to UK rocks.
Rocks behave less neatly than minerals, because a rock is a mix of minerals. The chart gives a rock a hardness only when one mineral decides it, like the calcite in limestone. For the rest it says "Varies", and that test never rules the rock out.
What the chart can't tell you
It can't tell you whether a gem is real or what anything is worth. A jeweller or a gem lab can.
It can't confirm a meteorite either. The meteorite pages run at Washington University in St. Louis say about 95% of meteorites attract a cheap magnet, but so do rocks with magnetite in them and industrial slag. Iron-oxide lumps are the most common "meteorwrong" they're sent, and they suggest a streak test. On this chart, a red-brown or yellow-brown streak points to hematite or goethite. If a heavy, magnetic find gets past that, take it to a museum or a university geology department.
Fossils, shells, sea glass and man-made materials like brick and concrete aren't in the chart.
How we made this tool
Carbonado Apps built this chart to run entirely in your browser, so your answers stay on your device and nothing is sent to us. Mineral values come from the Handbook of Mineralogy and rock descriptions from the Natural History Museum's guide to UK rocks. The text on this page was written with the help of AI tools. If something doesn't work, email hello@carbonado.app and we'll fix it.
Sources (6)
- Handbook of MineralogyMineralogical Society of America
- Beginner's guide to identifying UK rock typesNatural History Museum
- Lab 9: MineralsTexas A&M International University
- Mystery Minerals guidebookWestern University
- Why are some UK coins magnetic?The Royal Mint
- Some meteorite realitiesWashington University in St. Louis
