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Geological Formation

Fajã

Volcanic Formations

A faja, also spelled faja with a tilde in Portuguese, is a term of obscure origin for the supratidal talus that collects at the foot of a coastal cliff, built up by landslides or by lava flows reaching the sea, and it also names the small flat, often cultivable, patch of land by the shore that this fallen material creates. Because tides and tidal currents have only a minor effect on the resulting coastal shape, these deposits tend to persist as stable, flat land once they form. Fajas occur worldwide but are especially characteristic of the Azores, Madeira and the Canary Islands, volcanic archipelagos with steep coastal cliffs and, in many cases, lava flows that reach the ocean.

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Source Fajã (Wikipedia)
Volcanism, Processes
Source Fajã (Wikipedia)
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Fajã (Wikipedia)
  • Caused By: Mass Wasting, Lead sentence
    Fajã (Portuguese pronunciation: [fɐˈʒɐ̃], of unknown etymology) is a Portuguese term of obscure origin used to describe supratidal talus at the foot of coastal cliffs, caused by landslides or lava flows.
  • Caused By: Volcanism, Lead sentence
    Fajã (Portuguese pronunciation: [fɐˈʒɐ̃], of unknown etymology) is a Portuguese term of obscure origin used to describe supratidal talus at the foot of coastal cliffs, caused by landslides or lava flows.
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