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词汇 example_english_crater-lake
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Examples of crater lake


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Several groups visited the penguin colonies on the east coast and the craterlake, but the dense vegetation cover of some parts limits access.
We presented a comprehensive model for the ancient crater lakes, which contains : sedimentation style, possible niche migration in and below a craterlake, and possible ' foods ' and their distribution.
It is one of three cones constructed within the 7x11mi km caldera, which also contains an elongated craterlake on its southwest side.
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During a dawn flight, sample bottles were filled with craterlake water.
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A small craterlake about 1015 m in diameter is found within the crater.
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Some volcanic craters may fill either fully or partially with rain and/or melted snow, forming a craterlake.
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Between major eruptions, a warm acidic craterlake forms, fed by melting snow.
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A 600 m wide of craterlake is located at the summit.
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The 300 m (984 ft) -wide summit crater is often ice-free due to the geothermal heat and contains an intermittent acidic craterlake.
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It has an uneroded summit crater about 1.5kmmi 0 in diameter which contains a small craterlake.
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A craterlake lies between the two peaks.
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As of 2006, the craterlake had re-formed.
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Melting snow and ice, intense rainfall or the breakout of a summit craterlake can all generate lahars.
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Geologists, ecologists, archaeologists, naturalists and astronomers have reported several studies on the various aspects of this craterlake ecosystem.
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A maar characteristically fills with water to form a relatively shallow craterlake.
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Boiling water cascaded down the flanks of the mountain from the craterlake, and seismological equipment near the crater ceased working.
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It is a small pyroclastic shield truncated by a 2 km wide caldera filled by a craterlake.
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Botos is a beautiful cold, green water craterlake with a diameter of.
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It is a stratovolcano with a summit craterlake.
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The highest cone, which contains the heart-shaped craterlake, is located at the far northeastern end of the island.
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The oval-shaped, 1.8 x 3 km caldera has a central cone containing a 0.5 km wide crater, partially filled by a craterlake.
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Within the crater, the explosion also formed a series of small cones (known as scoria cones) and spheres surrounded by a craterlake.
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Sympatric speciation suggested by monophyly of craterlake cichlids.
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The crater appears to be an old craterlake bed, filled with sediments up to 3000 feet thick.
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This is because of its small range-size (one single craterlake) and the likelihood that fish could be introduced to the lake.
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The crater contains a classic craterlake with an island formed by the central uplift.
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The 1641 eruption caused the formation of the craterlake.
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It has 600 m wide of craterlake at the summit and some sulfur deposits.
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Its collapse created the caldera now occupied by the lake, which is a craterlake.
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The volcanic craterlake is 100 meters long by 70 meters and has a depth of 8 meters.
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The east maar has a 49 m-high lava dome within the craterlake.
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A new 1-km-wide, 300-m-deep crater was created that now contains an acidic craterlake.
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It was visible at the time of the expedition in 1916, but has since been submerged by the craterlake.
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Almost 100% of the volcano fell into the ocean, leaving a small craterlake.
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An eruption sometime before the twentieth century created a craterlake that is said to be shaped like a heart.
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There is a beautiful craterlake on its summit, at 3107 m.
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The highest peak is 2956 ft, with a 2.5km mi diameter craterlake.
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Steam from the summit craterlake and ash on the flank was reported in 1962.
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The volcano has a wide crater which contains a wide craterlake.
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The southwestern peak contains four cones, one of which has a craterlake.
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The volcano has a warm and highly acidic craterlake approximately 160 m (525 ft) wide.
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Inside the crater is a large sulphurous craterlake and several active steam vents.
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The oreum forms a shallow craterlake on top of it.
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The peak is topped by a wide summit crater, which contained a shallow craterlake until 1959.
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The deep quarry, which is filled with water, resembles a craterlake.
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Seepage of sulfurous gases has also caused acidic discolouration of the small craterlake.
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The environmentalists recommended that the craterlake be fenced again, on the account of the residual radioactivity.
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The following day, a lava dome rose through the centre of the craterlake atop the mountain.
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Together with the long-finned char it is endemic to this remote impact craterlake, being able to live in its environmentally very harsh conditions.
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The summit has a 300m ft diameter crater, containing fumaroles and sometimes a craterlake.
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In 1975 the surface of the craterlake was at an elevation of about, and the estimated elevation of the caldera floor is about.
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The caldera was once partly filled by a craterlake that covered about 50% of the crater.
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A wide summit crater caps the peak, and it contains a heart-shaped craterlake.
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The inner crater is filled by a craterlake.
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There are about 30 villages near this craterlake, with a combined population of about 70,000 people.
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Our conclusions could be useful for future searching programs, which look for signs of ancient life forms in crater lakes.
There are nine volcanic craters along a 2kmmi 1 line, and the eastern summit crater contains a briny, acidic 300 m (1000 ft) wide craterlake.
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If volcanic activity continues or restarts, the centre of the caldera may be uplifted in the form of a resurgent dome, to become a craterlake island.
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Its crater contains a craterlake.
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Despite the generally dry conditions, there is a permanent craterlake about 100 m in diameter at an elevation of 6390 m on the eastern side of the mountain.
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Because the walls of the inner crater are higher than the adjacent caldera floor, precipitation flowing inwards from the outer crater walls does not enter the inner craterlake.
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If we take into account the possible upward migration of water full of living organisms, we can count on living organisms in crater lakes.
Therefore, characterizing the lifetime of crater lakes (and associated hydrothermal circulation) is vital to understanding the constraints placed on any biological system that may have existed there.
In our work we present models for the niche migration and for the changes in the environmental factors in and below crater lakes.
There are many other volcanic cones with forty containing crater lakes.
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Due to their unstable environments, some crater lakes exist only intermittently.
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The volcanic island is dotted with cinder cones, tuff cones, pyroclastic cones, maars and crater lakes.
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Maars containing crater lakes have formed along a line through the summit of the volcano.
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Many of these volcanoes offer some great possibilities for tourists with activities such as hiking, climbing, camping, and swimming in crater lakes.
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Such features may include volcanic crater lakes and lava domes after the event.
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The north side is deeply eroded and the eastern side contains parasitic crater lakes and parasitic cones.
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While many crater lakes are picturesque, they can also be deadly.
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The nine most recently described members of this species complex are considered endemic to their respective small, volcanic crater lakes.
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At least two of the maars host crater lakes.
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There are eight plains and 12 crater lakes on the mountain that were formed by volcanic activity.
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It is observed that polythionates in crater lakes are drastically decreased before an eruption occurs.
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A long history of volcanism has also created a number of crater lakes in the province, the results of collapsed volcanoes filling with water.
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There are no reliable sources of surface water (rivers, streams, or lakes), save the crater lakes which are inaccessible.
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There are eleven volcanic crater lakes on the island.
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Many of these pit craters have been filled with water creating several crater lakes.
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Images also revealed several small hot crater lakes on the newly formed island.
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Isolated and relatively homogeneous habitats such as crater lakes and islands are among the best geographical settings in which to demonstrate sympatric speciation.
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Volcanism here has created crater lakes.
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Because it is part of a historically volcanic region, volcanic rock formations are a common sight, including lava beds, volcanic buttes, crater lakes, volcanic plugs, and lava tubes.
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Formed by the destructive eruption of an andesitic stratovolcano about 9,100 years ago, it contains three crater lakes, one 2 mi wide and two others about 1.5 mi wide.
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Such conditions necessarily require the widespread presence of crater lakes across a large proportion of the surface, for which there is also independent mineralogical, sedimentological and geomorphological evidence.
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By the middle of the last century the hills were almost completely denuded and virtually the only wildlife to be found were waterfowl that came to the crater lakes.
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Maars range in size from 61to- 1981 across and from 9to-198 m deep and are commonly filled with water to form a craterlake.
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Crater lakes are formed in volcanic craters and calderas which fill up with precipitation more rapidly than they empty via evaporation.
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Crater lakes dot the plateau, the result of dead volcanoes filling with water.
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These examples are from corpora and from sources on the web. Any opinions in the examples do not represent the opinion of the Cambridge Dictionary editors or of Cambridge University Press or its licensors.
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