Start by getting an idea of your basic rock classigneous, sedimentary or metamorphic. Next observe the rock's textureits grain size and overall patternconduct a basic hardness test, and identify the minerals that compose it as well as you can. With that information, you can consult the table for the appropriate rock class. Detailed instructions are beneath the tables.
| Identification of Igneous Rocks |
| Grain Size |
Usual Color |
Other |
Composition |
Rock Type |
| fine |
dark |
glassy appearance |
lava glass |
Obsidian |
| fine |
light |
many small bubbles |
lava froth from sticky lava |
Pumice |
| fine |
dark |
many large bubbles |
lava froth from fluid lava |
Scoria |
| fine or mixed |
light |
contains quartz |
high-silica lava |
Felsite |
| fine or mixed |
medium |
between felsite and basalt |
medium-silica lava |
Andesite |
| fine or mixed |
dark |
has no quartz |
low-silica lava |
Basalt |
| mixed |
any color |
large grains in fine-grained matrix |
large grains of feldspar, quartz, pyroxene or olivine |
Porphyry |
| coarse |
light |
wide range of color and grain size |
feldspar and quartz with minor mica, amphibole or pyroxene |
Granite |
| coarse |
light |
like granite but without quartz |
feldspar with minor mica, amphibole or pyroxene |
Syenite |
| coarse |
light to medium |
little or no alkali feldspar |
plagioclase and quartz with dark minerals |
Tonalite |
| coarse |
medium to dark |
little or no quartz |
low-calcium plagioclase and dark minerals |
Diorite |
| coarse |
medium to dark |
no quartz; may have olivine |
high-calcium plagioclase and dark minerals |
Gabbro |
| coarse |
dark |
dense; always has olivine |
olivine with amphibole and/or pyroxene |
Peridotite |
| coarse |
dark |
dense |
mostly pyroxene with olivine and amphibole |
Pyroxenite |
| coarse |
green |
dense |
at least 90% olivine |
Dunite |
| very coarse |
any color |
usually in small intrusive bodies |
typically granitic |
Pegmatite |
Identification of Sedimentary Rocks |
| Identification of Metamorphic Rocks |
| Foliation |
Grain Size |
Usual Color |
Other |
Rock Type |
| foliated |
fine |
light |
very soft; greasy feel |
Soapstone |
| foliated |
fine |
dark |
soft; "tink" when struck |
Slate |
| foliated |
fine |
dark |
shiny; crinkly foliation |
Phyllite |
| foliated |
coarse |
mixed dark and light |
crushed and stretched fabric; deformed large crystals |
Mylonite |
| foliated |
coarse |
mixed dark and light |
wrinkled foliation; often has large crystals |
Schist |
| foliated |
coarse |
mixed |
banded |
Gneiss |
| foliated |
coarse |
mixed |
distorted "melted" layers |
Migmatite |
| foliated |
coarse |
dark |
mostly hornblende |
Amphibolite |
| nonfoliated |
fine |
greenish |
soft; shiny, mottled surface |
Serpentinite |
| nonfoliated |
fine or coarse |
dark |
dull and opaque colors, found near intrusions |
Hornfels |
| nonfoliated |
coarse |
red and green |
dense; garnet and pyroxene |
Eclogite |
| nonfoliated |
coarse |
light |
soft; calcite or dolomite by the acid test |
Marble |
| nonfoliated |
coarse |
light |
quartz (no fizzing with acid) |
Quartzite |
These three tables will help you identify almost any rock type you're likely to find. Read How to Look at a Rock for help with your observations. First, decide whether your rock is igneous, sedimentary or metamorphic. This is not that hard!
- Igneous rocks are tough, frozen melts with little texture or layering; mostly black, white and/or gray minerals; may look like granite or like lava (about igneous rocks)
- Sedimentary rocks are hardened sediment with sandy or clayey layers (strata); mostly brown to gray; may have fossils and water or wind marks (about sedimentary rocks)
- Metamorphic rocks are tough, with straight or curved layers (foliation) of light and dark minerals; various colors; often glittery with mica (about metamorphic rocks)
Next, check the rock's grain size and hardness.
- Grain Size: "Coarse" grains are visible to the naked eye, and the minerals can usually be identified using a magnifier; "fine" grains are smaller and usually cannot be identified with a magnifier. (using a magnifier, identifying minerals)
- Hardness: Hardness (as measured with the Mohs scale) actually refers to minerals rather than rocks, so a rock may be crumbly yet consist of hard minerals. But in simple terms, "hard" rock scratches glass and steel, usually signifying the minerals quartz or feldspar (Mohs hardness 6-7 and up); "soft" rock does not scratch a steel knife but scratches fingernails (Mohs 3-5.5); "very soft" rock does not scratch fingernails (Mohs 1-2). Igneous rocks are always hard. Metamorphic rocks are generally hard.
Now start in the left column of the appropriate table and work your way across. Follow the links to pictures and more information. If you don't find a match, try another table. |