Примеры использования Calderas на Английском языке и их переводы на Русский язык
{-}
-
Colloquial
-
Official
Another attack on the Calderas is imminent.
The calderas widths can range from 1.5 to 5 km.
Some have collapsed craters called calderas.
The calderas are bordered by a well-preserved system of concentric normal faults and peripheral ring faults.
He's a little worried about what's going on at the Calderas.
The presence of two calderas suggests that two separate magma chambers underlie the volcano.
Praxis was blown to hell when the Calderas opened.
The two shield volcanoes have summit calderas of similar size, but Elysium Mons is 3.5 times larger in diameter and 6 times higher than its counterpart on Earth.
But there must be half a mile of solid rock covering those calderas.
Besides craters of impact origin, a lot of tholis, calderas and fissures are revealed within these planitiae.
I'm getting reports of massive explosions from the sites of each of the calderas.
Ksudach volcano is an ancient volcano with a truncated cone and calderas filled with crater lakes, 1,000 m high.
Lauca features include archaeological sites,lava fields and volcanic calderas.
Majority of paterae of Venus, Mars andIo are volcanic craters or calderas, but some others(like Orcus Patera on Mars), probably, are impact craters.
The Menengai volcano is considered one of the best-preserved Krakatau-style calderas in the world.
Lava flows and more than a hundred calderas are clearly seen on the moon's surface; the entire surface is covered with sulfur in various colored forms.
Between 1.0 million and 0.8 million years ago, they partially collapsed,forming large(5-10 km wide) calderas.
The Karymsky volcano and Academy Nauk caldera belong to a chain of volcanoes, calderas, and maars, the location of which is controlled by a local north-trending fault.
The growth of the mountain was occasionally interrupted by major eruptions,leading to the collapse of the summit to form calderas.
Several calderas are located at the summit of the volcano:two large calderas(I and II) formed in late Pleistocene; three calderas of smaller size(III, IV and V) formed in Holocene.
It is a truncated cone with a base of 18* 22km, crowned by a vast caldera 7* 9km,which in turn consists of smaller calderas and volcanic structures of different ages.
Uzon-Geysernaia twin calderas form a 9 x 18 km depression, which originated as a result of large explosive eruptions in the late Pleistocene time~39 600±1000 BP Florensky, 1984; Braitseva et al., 1995.
The present period began about 150,000 years ago and involved the development of the present volcanic edifice through the emplacement of lava domes made of andesite anddacite(igneous rocks) inside older calderas.
On the island there are active volcanoes located in the calderas of the more ancient volcanoes: Krenitsyn(1324 meters) in the caldera of Tao-Rusyr in the southern part and Nemo(1019 meters) in the northern part.
Larger clusters of sulphide occurrences are mainly controlled by geological features that can be readily identified in bathymetric surveys rift grabens or calderas with maximum dimensions of a few tens of kilometres.
The two nested calderas share the same rim on their western sides, but the older Island Park Caldera is much larger and more oval and extends well into Yellowstone National Park.
When the lava surged from the depths of the earth and formed these islands,it sculpted craggy peaks and calderas teeming with life, it carved geometric forms and deep gorges, it created fabulous beaches and incomparable seabeds….
More locally, sulphide occurrences may be found in volcanic or tectonic depressions that are superimposed on the volcanic highs e.g., rift grabens at the summit of a ridge segment;summit calderas of arc volcanoes.
The walls of rift grabens or summit calderas of recently active volcanic edifices are inherently unstable and rugged, although the bottoms of rifts and calderas may include locally flat areas where polymetallic sulphides may accumulate.
Despite its relatively small area, the island has much landscape diversity, which is explained by its complex geomorphology,in which there are stratovolcanic cones, calderas, lava flows, volcanic plateaus, various valleys, high and steep coastal ledges, sea terraces, and rocky beaches.