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词汇 example_english_sinkhole
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Examples of sinkhole


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The valley has been intensely karstified, as evidenced by the numerous sinkholes, springs, caves, and disappearing streams.
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Water erosion has left the calcareous plateaus strewn with dolines and poljes (sinkholes and flat-floored depressions).
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The animals apparently fell to their deaths tens of metres below, through narrow openings in the roof of the caves known as sinkholes.
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As a solution to the cholera problem, city officials constructed a sewer system to drain sinkholes that had become clogged with sewage and garbage.
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Sinkholes appear in hallways because outdoor sewage and drainage systems are outdated.
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Several sinkholes, some huge, have opened within the city.
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Karst is characterized by dissolved limestone formations such as sinkholes and haystack-shaped hills known as mogotes.
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All ramps and sinkholes are worth 5,000,000 for 30 seconds.
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Additionally, as many as 52 sinkholes were reported to have formed along roadways in the county.
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Many places are subject to earthquakes, landslides, tsunamis, volcanic eruptions, tornadoes, sinkholes, blizzards, floods, droughts, wildfires, and other calamities and disasters.
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Most of the parish has the typical limestone features of cockpits, sinkholes, caves and underground passages.
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The landscape includes many caves, sinkholes, springs, and streams.
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During dry spells all water sinks very quickly on reaching the limestone, through sinkholes.
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Large swells and dips can be encountered along the route, formed by swallets and sinkholes in the surrounding limestone.
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The geological process that is producing the sinkholes is under study, but is a total mystery.
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The other four caves are sinkholes capable of trapping animals, especially ground-dwelling and flightless birds, and contain the most fossils.
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Sinkholes are depressions in the earth caused by collapse of the roof of a cave.
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Sinkholes are the result of the collapse of the roof of a cave, and surface water can flow directly into them.
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The local terrain is hilly with patches of forest filled with sinkholes and many caves and caverns.
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Entire cities are built in cracks and crevices in the sides of the massive sinkholes, which extend inwards in perpetual twilight.
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About 9,000 sinkholes have been identified in the park, formed abruptly after gypsum in the soil has been dissolved by underground water.
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The damage at the surface is much greater if there is differential settlement, or large-scale features, such as sinkholes.
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The surrounding terrain is developed on limestone bedrock and exhibits karst topography due to dissolution of the limestone by ground water, creating water-filled sinkholes.
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The thousands of sinkholes known as cenotes throughout the region provide access to the groundwater system.
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Currently two first of them are sediment-filled sinkholes few meters above sea level, third one is submerged.
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On several occasions, the effects of heavy rainfall have created sinkholes beneath the settling ponds.
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Green sulfur bacteria are commonly found in meromictic lakes and ponds, sediments, and some sinkholes.
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Fast moving streams and rivers cutting into the limestone bedrock and in places creating caverns and sinkholes.
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Over time the wood rots and sinkholes can develop.
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The area has several caves, sinkholes, and bluffs overlooking the lake.
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Later, the connection of the individual sinkholes was explored.
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Most of the rock is limestone allowing for a number of formations such as caves and sinkholes.
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The ground is pitted with sinkholes, a danger to the cattle that graze the fields.
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There are more than 20 karst land formations such as huge caves, underground rivers, depressions, karst poljes, and sinkholes.
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They often also occur around geologic reef complexes and collapse features such as ancient sinkholes.
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Paleokarst features include isolated eaves and sinkholes as well as integrated cavern systems that are mineralized and can be traced from insurgence to outlet.
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The park is notable for its sinkholes, created by the dissolution of the gypsum underlying its soil.
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In karst topography, rivers may disappear through sinkholes, continuing underground.
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Other types of sinkholes, such as collapsed caves, are not washouts.
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Twelve water pipes were also cracked or destroyed by sinkholes resulting from the flooding.
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Since settler times it has been called the land of sinks for its many sinkholes.
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Carcar formation is typically a porous coralline limestone characterized by small sinkholes, pitted grooves, and branching pinnacles.
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Suffosion sinkholes are normally associated with karst topography although they may form in other types of rock including chalk, gypsum and basalt.
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A second catastrophe sees them falling into one of numerous dust-filled sinkholes, trapping them in a cavern.
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There are two natural sinkholes, or "cenotes", at the site of the city, which would have provided a plentiful supply of potable water.
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Medium-sized surface features may include sinkholes or cenotes (closed basins), vertical shafts, foibe (inverted funnel shaped sinkholes), disappearing streams, and reappearing springs.
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The limestone bedrock has formed bluffs, glades, caves, springs, and sinkholes.
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All ramps and sinkholes are worth 5,000,000 for 50 seconds.
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There are also sinkholes present- the most recent appeared in late 2013- believed to result from mine workings.
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Because of its limestone formation, the parish is noted for its 59 caves and numerous sinkholes.
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In 1969, 1981, and again in 2008, sinkholes formed in the area.
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The limestone composition halted the development of an airport as coralline limestone is soluble which causes formation of caves and sinkholes.
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About 500 years ago there was clearly another collapse which resulted in the creation of two larger sinkholes.
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The area is dominated by limestone with numerous karst (caves, crevices, sinkholes).
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Over 90% of the parish's surface is limestone so there is an abundance of cockpits, sinkholes, caves and underground passages.
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Pollution of the local environment may occur as well, such as contamination of groundwater or aquifers by leakage or sinkholes or soil contamination.
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To at least a depth of 55 m below sea level, the limestone has been dissolved forming cavities, sinkholes and caves.
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The sinkholes and cave systems provide a source of groundwater for the caves.
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Lapiez, sinkholes and caves resolve from the solution of the limestone.
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Branchwork caves are the most common of cave patterns and are formed near sinkholes where groundwater recharge occurs.
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The dissolution process produces a distinctive landform known as "karst", characterized by sinkholes, and underground drainage.
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During subsequent millennia these work deeper, leaving in their wake enormous waterless caverns, sinkholes and grottoes and forming underground labyrinths of channels and shafts.
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As its name suggests, the river in places goes underground due to the chalk bed being dissolved, forming swallow holes (sinkholes).
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Because these mines are located throughout the community and township, the area is subject to excessive erosion because of sinkholes.
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Both cuestas have a northward-facing scarp perforated by numerous sinkholes and caves.
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Is a semi-desertic world full with sinkholes, in which there are sources of water.
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Due to the nature of the karst soil there are also some depressions and sinkholes.
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The walls of sinkholes in hammocks are either bare or covered by mosses, liverworts, and ferns.
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Rockland hammocks are found on elevated outcrops of limestone, often in association with limestone sinkholes.
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Hammocks on limestone substrates, however, are dependent on the underlying water table to keep humidity levels high, especially in limestone sinkholes.
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When conditions are appropriate, wetland trees, such as pond-apple and coco-plum, may be found growing out of the bottom or walls of sinkholes.
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Sinkholes are cylindrical or conical depressions with steep limestone walls, found in karst rockland areas.
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The reason for this is the limestone in the region, which makes sinkholes a very common site.
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In many places, large sinkholes open up, as well as surface cavities.
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Most of the area is a karst landscape, where there is no direct drainage into any streams, but instead the rainfall goes directly into sinkholes.
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Anything disrupting the air flow through sinkholes and out the vents can affect the habitat.
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Several days of persistent rainfall resulted in house flooding, sinkholes, and sewer backups.
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Future expansions or collapses in the underground system are conceivable; these would show above ground as sinkholes or ponors.
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The region is pockmarked with natural sinkholes, called cenotes, which expose the water table to the surface.
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When they were exposed to the atmosphere, their limestones were subjected to chemical weathering that created the caves and sinkholes common to karst terrain, resulting in structures like blue holes.
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The year after the line opened, nine air pockets above the tunnel, caused by soil slides above the tunnel boring machine, were discovered and filled with cement to prevent sinkholes.
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Marl prairies are located where marl covers limestone that may protrude as pinnacles or erode into "solution holes": depressions formed by the same processes that create sinkholes.
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Access to water was a limiting factor on agriculture, with the limestone escarpment giving way in water filled sinkholes (cenotes), but rivers and streams were generally absent on the peninsula.
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They very frequently are home to unusual plants and animals because they usually have water at the bottom, and because the steep walls protect the sinkholes from herbivores.
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One, slight elevations of the terrain (predominant soil is of calcareous origin) above flooding levels during the rainy season, and two, the presence of sinkholes or cenotes.
The site is stated to be an example of a sediment-filled former sinkhole having become the summit of a low hill by differential erosion.
Their main options are to limit access, reduce services, increase copayments, and drive out patients with "sinkhole" problems by serving them poorly.
Rainwater (which percolates into sinkholes in the limestone), is enriched with dissolved calcium carbonate.
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Erosion of gypsum by this underground water has caused many sinkholes, some of which have become very deep lakes that are home to unique species.
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The cave is located in an area of karst topography, including sinkholes, springs, and limestone bedrock.
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Several of these karst features have unusual characteristics like travertine lids over several of the sinkholes with isolated waterbodies below.
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There are karstic sinkholes in the island's central limestone massif, and limestone caves with stalactites.
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Found in the area are approximated 18 sinkholes.
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Karst features such as sinkholes and caves are not uncommon in this area.
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The area is characterized by thin loess soil cover, isolated patches of glacial drift, deeply entrenched river valleys, and karst (sinkholes, caves, and springs) topography.
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Extended systems of underwater caves, sinkholes and springs are found throughout the state and supply most of the water used by residents.
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By the 1960s most of the mines had closed, leaving mine shafts, sinkholes, chat piles, and other dangers for future cleanup.
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Water may leak into the underground system from many sources including permeable earth, sinkholes, and losing streams.
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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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