Skip to main content

Slate

  • Reference work entry
  • First Online:
  • 3 Accesses

Slate is a shallow metamorphic rock with a lamellar structure that can be formed by shallow metamorphism of various rocks, such as the clay rock, siltstone, siliceous rock, intermediate acidic tuff, carbonaceous rock and calcareous rock. The degree of metamorphism is very low, and the minerals are generally not recrystallized. The rocks are mainly clay slate, silty slate, siliceous slate, tuff slate, carbonaceous slate, and calcareous slate. Slate can be named by putting the name of the new metamorphic minerals in front, such as sericite clay slate and chlorite clay slate. Slate has a dense texture and fine grains with smooth cleavage surfaces.

This is a preview of subscription content, log in via an institution.

Buying options

Chapter
USD   29.95
Price excludes VAT (USA)
  • Available as PDF
  • Read on any device
  • Instant download
  • Own it forever
eBook
USD   549.99
Price excludes VAT (USA)
  • Available as EPUB and PDF
  • Read on any device
  • Instant download
  • Own it forever
Hardcover Book
USD   699.99
Price excludes VAT (USA)
  • Durable hardcover edition
  • Dispatched in 3 to 5 business days
  • Free shipping worldwide - see info

Tax calculation will be finalised at checkout

Purchases are for personal use only

Learn about institutional subscriptions

Editor information

Editors and Affiliations

Rights and permissions

Reprints and permissions

Copyright information

© 2020 Springer Nature Singapore Pte Ltd.

About this entry

Check for updates. Verify currency and authenticity via CrossMark

Cite this entry

(2020). Slate. In: Chen, A., Ng, Y., Zhang, E., Tian, M. (eds) Dictionary of Geotourism. Springer, Singapore. https://doi.org/10.1007/978-981-13-2538-0_2279

Download citation

Publish with us

Policies and ethics