Karst processes in Niue
Volcano and coralls
Niue has formed on a volcano rising almost 4,000 m from the bed of ocean. It is capped with some 400 m thick layer of Miocene – Pliocene carbonates mostly formed by coralls. Island rises up to 70 m high above the sea.
Coast of Niue represents abrupt cliff – it is constantly washed out by sea waves. But, contrary to similar basalt or granite cliffs, here are no streams falling over the edge in the ocean. Such streams disappear in numerous cracks and seeps of carbonate rock well before the coast.
As a result there are no surface streams on Niue – even after a heavy rainfall on few minutes the land is dry.
As the time goes many seeps become wider and more and more water is diverted to them. Finally there forms a chasm or cave. Caves over the time become larger and larger and finally the ceiling collapses in some places (sinkhole) or wholly (chasm). Often natural rock bridges over the chasm remain. Hard water from the smaller seepages is depositing lime along the walls of these larger caves and as a result there form beautiful speleothems: stalactites, stalagmites and others.
Caves meet ocean
The cave streams of Niue inevitably reach the ocean. Ocean also takes active part in cave formation. First: the powerful waves wash out the cave entrance. Second: waves cause sharp, constant air pressure changes in the cave. Sometimes the rocks are literally blown out through the cracks. Third: the salty water facilitates dissolution of carbonates.
Such processes are observed along the whole coast of Niue – here have formed hundreds of chasms and caves, numerous natural arches and blowholes.
Showroom of karst processes
Possibly the best and most impressive place to see all these processes is Talava Caves and Arches.
This amazing natural landmark starts as a cave – beautiful cave with numerous stalactites and other dripstone formations. This cave has one exit towards the sea (dangerous when the sea is rough) and another – towards a large sinkhole.
The sinkhole is some 35 m long and up to 16 m wide, depth is around 20 m. It represents a section of collapsed cave – there still are entrances into several smaller caves from it. Amazing features of this sinkhole are two natural arches – one is 15 m wide and 14 m high, another – 15 m wide and 8 m high.
Talava sinkhole represents one of the most magnificent sights in Niue. Bottom of this formation is covered with green plants. Walls are adorned with flowstone and resemble a weird sculptural artwork in the style of H.R. Giger. It is hard to imagine more suitable place for making movies about dragons or dinosaurs. Sensations are supplemented by the sound of nearby waves.
Natural arch in the sea
After crossing the bottom of sinkhole one can reach the sea with the last and possibly best geomorhological wonder of this site: the third – largest natural arch. This is 35 m wide, 8 m high and some 9 – 12 m broad natural arch standing with one leg into the sea. It is hard to say how long it will last against the power of waves – but sooner or later it will collapse.
- Natural Arch and Bridge Society. Accessed 10.01.11.
- Portal Oceania, Talava Arches & Caves. Accessed 11.01.11.
|Coordinates:||19.9599 S 169.8779 W|
|Categories:||Caves, Sinkholes, Rock formations, Karst landscapes, Natural arches|
|Rating:||(2.5 / 5)|
|Address:||Australia and Oceania, Polynesia, Niue, at the northern coastline|
|Alternate names:||Tavala Arches (erroneously)|
This is the story of Niue, the world’s smallest self-governing nation,written by leading citizens of the country itself.The book outlines the origins and early history of a vigorous Polynesian people, and the changes which have come about as the result of contact with Christianity, commerce and colonial government. The authors then describe the move towards independence, the situation in Niue today and the prospects for the future.
Physical landscapes are one of the most fascinating facets of our Planet, which tell stories about the evolution of the surface of the Earth. This book provides up-to-date information about the geomorphology of the selected ‘classic’ sites from around the world and shows the variety of geomorphological landscapes as moulded by different sets of processes acting over different timescales, from millions of years to days.