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Rock Identify

Identification guide

What Rock Is White? Compare Texture and Luster

Common white finds include milky quartz, calcite, marble, quartzite and limestone. Compare the broken face and how light passes through an edge.

Curved glassy breaks point toward quartz. Flat stepped faces that flash together suggest calcite. Tiny interlocking grains fit marble or quartzite. A dull, powdery surface may suggest chalk or another limestone. If you are asking what rock is white, start with the texture and keep more than one candidate when clues overlap.

This is the site's color hub. It groups the white rocks and the green rocks people most often pick up, gives each a table of luster, translucency and texture, then points gray, black, red and brown finds to their own guides. Upload one to three photos to Rock Identify and compare each candidate's evidence against the table row.

Guide updated

Why color is the weakest clue and texture is the strongest

Color shifts with weathering, wetness, iron staining and the light you shoot in. The same milky quartz pebble reads bright white dry, gray wet and yellow where iron has soaked into cracks, and a white limestone pebble beside it looks identical from a step away. Texture does not shift like that. How a rock breaks, how big its grains are against your fingernail, and whether light passes a thin edge stay the same in every photo.

So the order here is color first, texture second. Pick the color group, then narrow with luster in low angled light, translucency against daylight, and grain size. A photo shows all three. It cannot show hardness, streak, density or chemistry, so the last column of each table lists what still needs a hand check.

What rock is white? Eleven candidates and how they split

Turn the specimen so window light rakes across it and ask three questions. Does the broken surface show curved glassy fracture (quartz or chert), flat faces that flash in steps (calcite, feldspar or gypsum), or tiny interlocking grains (marble or quartzite)? Then hold a thin edge toward daylight. Quartz and calcite glow at the rim, marble glows faintly, chalk and limestone stay dead.

What rock is white? Eleven candidates and how they split

Material

Usual luster

Translucency

Texture

What separates it in a photo

What a photo cannot show

Milky quartz

Greasy to glassy

Edges glow, body cloudy

No grains, curved conchoidal breaks

No flat faces; iron stains follow cracks

Hardness; white glass not excluded

Calcite

Pearly to glassy

Clear to cloudy

Rhomb-shaped blocks, stepped cleavage

Flat faces at repeating angles flash together

Hardness; whether it fizzes

Marble

Sugary sparkle

Faint at thin edges

Even interlocking grains, gray veins

Grains glitter one by one; veins smear, not band

Marble or quartzite: rough scratch check

Quartzite

Glassy grains

Slight at edges

Fused sand grains, breaks across grains

Glassier sugar than marble; faint bedding; no veins

Hardness against marble

Chalk or limestone

Dull, earthy

None

Powdery or fine, shell pieces

Pits, fossil bits, white dust on fingers

Acid reaction; chalk against plaster

Feldspar-rich granite

Grainy, scattered flashes

None

Coarse white, pink and black crystals

Separate crystals bigger than a rice grain

Which feldspar

Gypsum or alabaster

Satin or pearly

Soft glow

Fibrous or fine; shows handling scratches

Satin sheen along fibers; scuffed corners

Softness; a rough fingernail check

White chert

Waxy, dull rind

Thin edges only

No grains, sharp conchoidal chips

Sharper edges than quartz; chalky rind over waxy core

Hardness

Dolomite

Pearly

Cloudy

Slightly curved faces; fine grain in rock

Saddle-shaped faces, cream or pink tint

Weak acid reaction

Pumice

Dull

None

Frothy, full of tiny holes

Vesicles across every surface

Lightness; float it in water

Concrete or plaster

Dull, chalky

None

Rounded gravel in gray-white paste, one flat side

Mixed pebbles in uniform paste; molded face

Age and origin

Milky quartz: cloudy body, glowing edges, no flat faces

Milky quartz: cloudy body, glowing edges, no flat faces

A reference photo of milky quartz. Note the greasy luster and curved break; nothing on the surface is a flat crystal face, the quickest separation from calcite.

Milky quartz reference photo, not a find from the area this page covers. Jan Helebrant · CC BY-SA 2.0 · Encyclopedia entry

The three white pairs that cause most wrong answers

Quartz against calcite: quartz has no cleavage and breaks with curved, shell-like surfaces, while a broken calcite crystal usually shows flat, mirror-like faces meeting at slanted angles, so a close-up of an existing broken face often settles it. Marble against quartzite: both are sugary, but marble turns dull where handled and carries smeared gray veins, while quartzite looks glassier grain by grain. Chalk against plaster: plaster shows a flat molded side, sometimes paint; chalk shows pits, shell fragments and a natural shape.

Green rocks: separate the serpentine family from the glass

Green is less common than white, so the list is shorter, but it holds the costliest mistake on this page: calling a green pebble jade. Most green stones from beaches, river bars and landscaping gravel are serpentinite, chlorite schist or epidote-stained rock. A photo rules out glass, malachite and aventurine quickly; it cannot confirm jade.

Green rocks: separate the serpentine family from the glass

Material

Usual luster

Translucency

Texture

What separates it in a photo

What a photo cannot show

Serpentinite

Waxy to greasy

Slight at edges

Smooth, mottled, slick streaks

Mottled greens with white veins; slick surfaces

Jade or serpentine: hardness, density

Jade lookalikes (nephrite, jadeite)

Waxy to oily

Even glow at thin edges

Fibrous (nephrite) or finely granular (jadeite)

Dense, even color, no vesicles or glitter

Authenticity, density, hardness

Epidote

Glassy

Translucent in small crystals

Pistachio-green needles or crusts

Yellow-green against pink feldspar, as in unakite

Composition beyond the color

Green aventurine quartz

Glassy with sparkles

Translucent edges

Granular quartz with mica flakes

Flecks that flash as you tilt it

Dye on tumbled beads

Chlorite schist

Dull to silky

None

Flaky, splits into sheets

Parallel sheen that moves in lines

Chlorite against talc softness

Malachite

Silky in bands

Opaque

Concentric bands, rounded bumps

Light and dark green bands over a lumpy crust

Resin-bound or reconstituted pieces

Olivine in peridotite

Glassy grains

Grains translucent

Olive-green sand-sized grains in a dark host

Glassy green grains inside black rock

Fresh against weathered grains

Chrysoprase

Waxy

Even apple-green glow

No grains, conchoidal

Even color without bands, flakes or sparkle

Dye, common in cheap beads

Green glass or slag

Glassy

Clear to cloudy

Bubbles, swirl lines, sharp chips

Round bubbles and flow lines in a close-up

Bottle glass against furnace slag

Serpentinite: mottled waxy green with white veins

Serpentinite: mottled waxy green with white veins

A reference photo of serpentinite. The surface looks pre-polished and the greens are mottled rather than even, which is the usual giveaway against jade in a photo.

Serpentinite reference photo, not a find from the area this page covers. James St. John · CC BY 2.0 · Encyclopedia entry

Gray, black, red and brown rocks: where they go next

Gray and black rocks are usually basalt, gabbro, slate, shale or dark limestone, and the deciding clue is grain and holes. Basalt is fine-grained with scattered vesicles, gabbro shows coarse black and gray crystals, slate splits into flat sheets, shale crumbles in thin layers, dark limestone is smooth and may hold fossils. Obsidian is the glossy exception, with conchoidal fracture. The metamorphic guide covers slate, schist and gneiss; the general guide covers the igneous ones.

Red and brown are almost always iron. Hematite coats a sandstone, jasper is red through and through, quartzite picks up a rust tint, and many plain pebbles wear a rust rind over a gray interior. Photograph a broken face beside the weathered one; if the inside is gray, the color is a skin. Jasper has no visible grains and takes a waxy polish, which is why it also appears on the polished rock page.

Photograph it so the tables and the tool both work

  1. Shoot the whole rock on a plain dark background in daylight, with a coin for scale.

  2. Take a close-up of the broken face at a low angle so luster and fracture show.

  3. Hold a thin edge toward the window and photograph the glow for translucency.

  4. Wet half the rock if it is dull; the wet half shows true color and veins.

  5. Upload one to three of these photos, read each candidate's evidence against its table row, then ask the follow-up question about the clue that still conflicts.

One question people ask about green rocks

Can a photo tell jade from serpentinite?

It can rule jade out when it sees mottling, white veins, flakes or bubbles, and it can say a stone is consistent with jade. It cannot confirm jade, because that rests on density and hardness. Treat a jade candidate as a reason to read the jade guide, not a result.

Sources