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Sea caves are formed by the power of the ocean (or in some cases, lakes) attacking zones of weakness in coastal cliffs. The weak zone is usually a fault, or fractured zone formed during slippage. Another type of weak zone is formed where dissimilar types of rocks are interbedded and one is weaker than the other. Typically this is a dike, or intrusive vein of more easily eroded rock found within a stronger host rock. Yet a third instance is in sedimentary rocks where a layer of softer rock is interbedded between harder layers. The cave may begin as a very narrow crack into which waves can penetrate and exert tremendous force, cracking the rock from within by both the weight of the water and by compression of air. Sand and rock carried by waves produce additional erosive power on the cave's walls. Sea caves rarely have formations like solution caves or lava tubes, so we're just devoting one page to them here in The Virtual Cave. Occasionally some flowstone or small stalagmites are seen, formed much as in solution caves. Typically these occur in caves formed in sandstone, limestone, or sometimes even those in basalt. Sea caves are found all over the world, and may be one of the most numerous types of caves. Areas known for large concentrations of sea caves include the Pacific coast states of the USA (Alaska, Washington, Oregon, and California, and especially, California's Channel Islands); the Na Pali coast of Kauai; the Greek Isles; the British Isles, and many other places with cliffs of good solid rock to host the caves. Of special interest is New Zealand, which has both the world's two largest sea caves, in terms of their length, and also the world's largest in terms of volume. See below for details on these amazing caves. Author Dave Bunnell, has explored and surveyed over 500 sea caves around the world, and written numerous articles, two books on California sea caves, and an encyclopedia chapter on them. See the References section at the end of this page for links to articles in PDF format that the I've written on sea caves in California, Hawaii, and New Zealand and on special topics such as vertical sea caves. |
Arches & sea stacks Regions where sea caves form are often associated with arches and sea stacks. Often these are remnants from collapses of sea caves, and in some cases may line up along what had been a fault line in a rock unit that has been carved by the sea into isolated stacks of rock. Both arches and stacks are relatively ephemeral and numerous arches depicted on postcards from the early 1900s have already collpased. A database of sea arches is maintained by the National Arch and Bridge Society . |
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Life in a Sea Cave Sea caves may abound with life, both on their walls and floors.
Besides the kind of critters seen in normal tidepools, such as anemones,
starfish, and sponges, sea caves with dark zones may harbor organisms
not commonly seen in shallow water. . In California, the Giant Anemone
is normally green because of an algae that lives inside of it; but in
sea caves with dark zones, like the one middle left, these anemones may
be white because the green algae doesn't get enough sunlight to grow.
Similarly, sponges like that in the same image are generally always white in the darker recesses of sea caves, as opposed to the colorful ones in the upper left. |
World's Largest A list of the world's longest sea caves has been compiled by the author and Bob Gulden. Matainaka Cave, on the Otago coast of New Zealand' South Island, has been verified by surveys as of October 2012 as the world's largest sea cave by length, an amazing 1.54 km or 5,051 feet, not quite a mile. But if the rate of its formation outpaces that of its collapse, it could yet reach that milestone in centuries to come. Many fractures in the host sandstone have resulted in a cave with numerous interesecting passages and a dozen entrances in the sea cliff. Although the largest by length, it is probably not the largest by volume, although a volumetric survey wasn't produced. See below entry about Riko Riko Cave. |
![]() A passage in Matainaka shows its character, water-floored, smooth, sculpted walls and some calcite speleothems formed from the dissolution and re-deposition of the cement that binds the host sandstone together. |
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World's Largest Painted Cave is on California's Santa Cruz Island. It is 1227 feet long and large enough to take a 40-foot boat inside. On the left, looking out the 130-foot-high entrance. On the right are two views of the very dark inner chamber. The top image shows a sharp edge to the right of the red kayak, where the two faults along which the chamber eroded intersect. Sea lions inhabit the ledges in the back of the chamber much of the year. Click here to see a detailed map of the cave. |
Two views of the inner chamber of Painted Cave, usually explored by dinghy or kayak from a larger boat. |
Other contenders for world's largest sea caves
SCOTLANDHoll o Boardie is a cave on Papa Stour, one of the Shetland Islands, off the northern tip of Scotland. It hasn't been officially surveyed, but can be estimated fairly accurately since it is a tunnel passing through a headland. A local expert puts it at about 330m (1082 feet) long. This makes it somewhat longer in linear extent than any but Purple Cathedral, so by that yardstick is one of the world's longest. It is not surprising that the longest sea cave passage should be a two-entrance cave, as this has allowed the sea to attack it at both ends. Eventually, the tunnel's roof will collapse and leave a sea stack. |
NORWAYSome of the world's longest sea caves are relict or raised sea caves on the coast of Norway. These are caves formed by wave action over a long period that have been uplifted above the littoral zone. They range from 100 to 384 feet above the present sea level, so none are currently enlarging by wave action. They formed over a very long period of time, perhaps more than a million years in some cases according to dating of sediments within. No doubt this is why they are so much bigger than caves at current ocean level. The largest are formed in granitic rocks. Swedish caver Rabbe Sjoberg provided this list of the 10 longest based on accurate surveys: Halvikshulen, Osen 340 m (1,115 feet) In the photos on the right are 3 of these long caves. Note the people for scale in them. top: Halvikshulen entrance, 722 feet wide and 262 feet high. Probably the largest sea cave entrance in the world. |
![]() View of Halvikshulen (top image) from the sea |
![]() A 50-foot dive boat in the entrance of RikoRiko, viewed from inside and outside (upper right) |
World's Largest When we ask what is the world's largest sea cave by volume rather than horizontal length, we get a different answer: Riko Riko Cave, on the Poor Knight Islands off the east coast of New Zealand's North Island. Lengthwise, Riko tapes out at only about 500 feet, but the egg-shaped chamber was determined via laser survey to have a volume of about 7,800,000 cubic feet. Painted Cave's volume can only be estimated from its survey, to be roughly 56% that of Riko. Dive! Tutakaka offers boat tours of the Poor Knights that include a visit to Riko Riko. Click here for a detailed article on the 3D laser survey of Riko Riko with more photos, in Adobe Acrobat format. |
Articles about Sea Caves (PDF format) by Dave BunnellNote that the first 3 articles are scans so are larger files than the other 6. This material is copyrighted and may not be reprinted without permission from the author or cartographers. The Amazing Caves of Santa Cruz Island, NSS News, January 1983 (15.6 mb) Sea Caves of Kauai's Na Pali Coast, NSS News, December 1988 (19.5 mb) Sea Caving in the Channel Islands, NSS News, June 1993 (9.6 mb) California's Coastal Sea Caves, NSS News, October 1998 (2.8 mb) Riko Riko Cave, New Zealand-World's Largest Sea Cave? NSS News, May 2004 (.8 mb) Vertical Sea Caving, NSS News, October 2006 (4.2 mb) My Short Career as a Sea Cave Detective, NSS News, October 2007 (.9 mb) Return to Painted Cave, Santa Cruz Island, California, NSS News, January 2008 (8 mb) Return to Santa Cruz Island, NSS News, January 2009 (1.9 mb)
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Last updated February 19, 2013 |