Linked from

The 10 pages that link to Slate, each with the reason it gives.

• Metamorphic rockBroader topic: Slate demonstrates how low-grade metamorphism creates a strong, closely spaced cleavage.

• Dimension stoneBroader topic: Its natural cleavage allows production of flat slabs and tiles.

• GneissCompared with: Slate’s fine grain and planar cleavage differ from gneiss’s coarse mineral bands.

• FoliationBroader topic: Its planar cleavage is a characteristic fine-grained foliation.

• ShaleCompared with: Its sheet-like splitting resembles shale’s, but slate forms through metamorphism.

• SchistCompared with: Slate has a finer texture and slaty cleavage rather than schist’s visible grains.

• Billiard tableRelated: Slate commonly provides the table’s rigid, accurately leveled bed beneath the cloth.

• GreenschistCompared with: Slate is typically finer-grained and less rich in green metamorphic minerals.

• PhylliteCompared with: Phyllite has larger mica grains, a silky sheen, and commonly wavier surfaces than slate.

• Stone slabRelated: Slate’s natural cleavage makes it especially suited to thin slabs and paving.