Tindar is a ridge made by subglacial volcanism. It can contain pillow lava, pillow breccia, hyalotuff, hyaloclastite. Examples are Skefilfjall, Kálfstindar, Helgafell in Iceland and Pillow Ridge in British Columbia, Canada.[1]

References

  1. ^ Russell, J.K.; Edwards, B.R.; Porritt, Lucy; Ryane, C. (2014). "Tuyas: A descriptive genetic classification". Quaternary Science Reviews. 87: 70–81. Bibcode:2014QSRv...87...70R. doi:10.1016/j.quascirev.2014.01.001.


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