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Statements

Subject Item
dbr:Montezuma_Well
rdf:type
yago:Object100002684 yago:Region108630985 owl:Thing geo:SpatialThing yago:ServiceArea108648781 dbo:Cave yago:Area108497294 yago:Point108620061 yago:YagoPermanentlyLocatedEntity yago:WikicatProtectedAreasOfYavapaiCounty,Arizona yago:YagoLegalActorGeo yago:YagoGeoEntity yago:WikicatUnitedStatesNationalParkServiceAreasInArizona yago:Location100027167 yago:TopographicPoint108664443 yago:PhysicalEntity100001930
rdfs:label
Montezuma Well
rdfs:comment
Montezuma Well (Yavapai: ʼHakthkyayva), a detached unit of Montezuma Castle National Monument, is a natural limestone sinkhole near the town of Lake Montezuma, Arizona, through which some 1,500,000 US gallons (5,700,000 L; 1,200,000 imp gal) of water emerge each day from an underground spring. It is located about 11 miles (18 km) northeast of Montezuma Castle. Montezuma Well's steady outflow has been used for irrigation since the 8th century. Part of a prehistoric irrigation ditch is preserved near the park's picnic ground, and portions of the ditch's original route are still in use today.
geo:lat
34.64916610717773
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-111.7522201538086
foaf:depiction
n18:Camp_Verde-_Montezuma_Well-Sinagua_pit_house_ruins-1.jpg n18:Montezuma_Well_-_38670493161.jpg n18:2021_Montezuma_Well,_cliff_dwellings_2.jpg n18:Montezuma_Well_crop.jpg n18:Montezuma's_Well.jpg n18:Montezuma_Well_-_38638244442.jpg n18:2021_Montezuma_Well,_cliff_dwellings_close_2.jpg n18:2021_Montezuma_Well,_irrigation_ditch_1.jpg
dcterms:subject
dbc:Protected_areas_of_Yavapai_County,_Arizona dbc:Native_American_history_of_Arizona dbc:Sinagua dbc:Springs_of_Arizona dbc:History_of_Yavapai_County,_Arizona dbc:Sinkholes_of_the_United_States dbc:Bodies_of_water_of_Yavapai_County,_Arizona dbc:National_Park_Service_areas_in_Arizona dbc:Archaeological_sites_in_Arizona
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dbo:abstract
Montezuma Well (Yavapai: ʼHakthkyayva), a detached unit of Montezuma Castle National Monument, is a natural limestone sinkhole near the town of Lake Montezuma, Arizona, through which some 1,500,000 US gallons (5,700,000 L; 1,200,000 imp gal) of water emerge each day from an underground spring. It is located about 11 miles (18 km) northeast of Montezuma Castle. The "well" measures 386 feet (118 m) in diameter from rim to rim and contains a near-constant volume of spring water even in times of severe drought. The water is highly carbonated and contains high levels of arsenic. At least five endemic species, the most of any spring in the southwestern United States, are found exclusively in Montezuma Well: a diatom, the Montezuma Well springsnail, a water scorpion, the Hyalella montezuma amphipod, and the Motobdella montezuma leech. Montezuma Well's steady outflow has been used for irrigation since the 8th century. Part of a prehistoric irrigation ditch is preserved near the park's picnic ground, and portions of the ditch's original route are still in use today. As with Montezuma Castle, the label "Montezuma" is a misnomer: the Aztec emperor Montezuma had no connection to the site or the early indigenous peoples that occupied the area.
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dbr:Sinkhole
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