Matches in DBpedia 2016-04 for { <http://wikidata.dbpedia.org/resource/Q1641276> ?p ?o }
Showing triples 1 to 72 of
72
with 100 triples per page.
- Q1641276 subject Q15297304.
- Q1641276 subject Q15956771.
- Q1641276 subject Q7143668.
- Q1641276 subject Q7143689.
- Q1641276 subject Q8238922.
- Q1641276 subject Q8804205.
- Q1641276 subject Q8823352.
- Q1641276 abstract "Quilotoa (Spanish pronunciation: [kiloˈto.a]) is a water-filled caldera and the most western volcano in the Ecuadorian Andes. The 3-kilometre (2 mi)-wide caldera was formed by the collapse of this dacite volcano following a catastrophic VEI-6 eruption about 800 years ago, which produced pyroclastic flows and lahars that reached the Pacific Ocean, and spread an airborne deposit of volcanic ash throughout the northern Andes. This last eruption followed a dormancy period of 14,000 years and is known as the 1280 Plinian eruption. The fourth (of seven) eruptive phase was phreatomagmatic, indicating that a Crater lake was already present at that time. The caldera has since accumulated a 250 m (820 ft) deep crater lake, which has a greenish color as a result of dissolved minerals. Fumaroles are found on the lake floor and hot springs occur on the eastern flank of the volcano.Quilotoa is a tourist site of growing popularity. The route to the "summit" (the small town of Quilotoa) is generally traveled by hired truck or bus from the town of Zumbahua 17 km to the South, or more commonly by bus from Latacunga. Visitors may have to pay two US dollars each to look from the lip of the caldera. There are a number of simple hostels in the immediate area offering services such as mules and guides. Activities include a four to five-hour hike around the caldera (whose diameter is just over 3 km). The caldera rim is highly irregular and reaches its maximum elevations (3810 m to the N, 3894 m to the NW and 3915 m to the SE) at three lava domes. The 10 km hike is sandy and steep in places and can be quite taxing, particularly if there is fog.It's a half-hour hike down from the viewpoint (and 1-2 hour hike back up the 280-meter vertical ascent), and very basic lodging down in its bowl. Camping is permitted at the bottom of the crater, but there is no potable water (except half-litre bottles sold at the hostel), and only a single pit toilet, located in the hostel.The lake surface is located at 3,500 m asl. The total volume of water stored in Lake Quilotoa is 0.35 km3. According to local inhabitants, the lake level has been slowly declining over thelast 10 years. Travertine deposits occur along the shore up to 10 m above the lake level (in the year 2000).The village of Quilotoa and the associated crater is also a popular destination within the Quilotoa Loop and is a common starting point for the Quilotoa Traverse, a multi-day village to village hiking route.".
- Q1641276 elevation "3914.0".
- Q1641276 eruptionYear "1280".
- Q1641276 locatedInArea Q241140.
- Q1641276 locatedInArea Q385955.
- Q1641276 locatedInArea Q736.
- Q1641276 mountainRange Q5456.
- Q1641276 thumbnail Panorama_quilotoa_crater_lake_ecuador.jpg?width=300.
- Q1641276 type Q159954.
- Q1641276 wikiPageExternalLink en_ar_quilotoa.htm.
- Q1641276 wikiPageExternalLink lagunaquilotoa.html.
- Q1641276 wikiPageExternalLink quilotoa.
- Q1641276 wikiPageExternalLink quilotoa.html.
- Q1641276 wikiPageWikiLink Q105880.
- Q1641276 wikiPageWikiLink Q107099.
- Q1641276 wikiPageWikiLink Q15297304.
- Q1641276 wikiPageWikiLink Q15956771.
- Q1641276 wikiPageWikiLink Q159954.
- Q1641276 wikiPageWikiLink Q187156.
- Q1641276 wikiPageWikiLink Q204324.
- Q1641276 wikiPageWikiLink Q210510.
- Q1641276 wikiPageWikiLink Q221616.
- Q1641276 wikiPageWikiLink Q241140.
- Q1641276 wikiPageWikiLink Q379338.
- Q1641276 wikiPageWikiLink Q385955.
- Q1641276 wikiPageWikiLink Q466481.
- Q1641276 wikiPageWikiLink Q47212.
- Q1641276 wikiPageWikiLink Q5247872.
- Q1641276 wikiPageWikiLink Q5456.
- Q1641276 wikiPageWikiLink Q6452016.
- Q1641276 wikiPageWikiLink Q654772.
- Q1641276 wikiPageWikiLink Q7143668.
- Q1641276 wikiPageWikiLink Q7143689.
- Q1641276 wikiPageWikiLink Q736.
- Q1641276 wikiPageWikiLink Q747501.
- Q1641276 wikiPageWikiLink Q8072.
- Q1641276 wikiPageWikiLink Q8238922.
- Q1641276 wikiPageWikiLink Q8804205.
- Q1641276 wikiPageWikiLink Q8823352.
- Q1641276 wikiPageWikiLink Q974698.
- Q1641276 wikiPageWikiLink Q98.
- Q1641276 elevationM "3914".
- Q1641276 lastEruption "1280".
- Q1641276 location Q241140.
- Q1641276 location Q385955.
- Q1641276 location Q736.
- Q1641276 name "Quilotoa".
- Q1641276 range Q5456.
- Q1641276 type Q159954.
- Q1641276 point "-0.861193 -78.897285".
- Q1641276 type Mountain.
- Q1641276 type Place.
- Q1641276 type Location.
- Q1641276 type Mountain.
- Q1641276 type NaturalPlace.
- Q1641276 type Place.
- Q1641276 type Thing.
- Q1641276 type SpatialThing.
- Q1641276 type Q8502.
- Q1641276 comment "Quilotoa (Spanish pronunciation: [kiloˈto.a]) is a water-filled caldera and the most western volcano in the Ecuadorian Andes. The 3-kilometre (2 mi)-wide caldera was formed by the collapse of this dacite volcano following a catastrophic VEI-6 eruption about 800 years ago, which produced pyroclastic flows and lahars that reached the Pacific Ocean, and spread an airborne deposit of volcanic ash throughout the northern Andes.".
- Q1641276 label "Quilotoa".
- Q1641276 lat "-0.861193".
- Q1641276 long "-78.897285".
- Q1641276 depiction Panorama_quilotoa_crater_lake_ecuador.jpg.
- Q1641276 name "Quilotoa".