Laguna Caldera
{{Short description|Underwater volcanic caldera in Laguna de Bay, Philippines}}
{{More citations needed|date=February 2020}}
{{Infobox mountain
| name = Laguna Caldera
| other_name =
| photo = LagunaCaldera05.jpg
| photo_size =
| photo_alt =
| photo_caption = Laguna Caldera looking northwest
| elevation_m = 743
| prominence_m =
| prominence_ref =
| listing =
| range =
| location = Rizal, Philippines
| map = Philippines
| map_alt =
| map_caption = Location of Laguna Caldera in the Philippines
| map_size = 220
| label =
| label_position =
| region =
| coordinates = {{coord|14.42|N|121.27|E|type:mountain_scale:100000|format=dms|display=inline,title}}
| topo_map =
| type = Caldera
| volcanic_arc/belt = Macolod Corridor
| age =
| last_eruption = Approx. 1.2 Million Years Ago
| first_ascent =
| easiest_route =
}}
Laguna Caldera is a potentially active volcanic caldera and a geographical depression in Rizal, Philippines. It is broadly elliptical in shape, with dimensions of 20 by 10 km. It has a summit (Mount Sembrano) elevation of {{convert|743|m|ft|0}}.{{cite gvp|name=Laguna Caldera|vn=273080|access-date=2021-06-25}} The caldera forms the middle lobe of Laguna de Bay, bound by the Morong Peninsula and Talim Island to the west, and the Jalajala Peninsula to the east.
The caldera may have formed in two stages about 1 million and 27,000-29,000 years ago, during which time at least two major explosive eruptions took place. It is unknown when the Laguna Caldera last erupted but it may have been active during the Holocene. Deposits from the caldera form thick ignimbrite sheets in Rizal, Metro Manila, Laguna, and Bulacan.{{Cite book|title=Explosive volcanism in the Philippines|last=Catane, S. G.|date=2005|publisher=Tōhoku Daigaku Tōhoku Ajia Kenkyū Sentā|isbn=4901449257|location=Sendai-shi|oclc=61505021}} Remnants of volcanic activity include undated maars at the southern end of Talim Island and a solfatara field on nearby Mount Sembrano. Given the current shape of the lake and the caldera, and how it was once connected to Manila Bay as evidenced by its ground drill geology, its formation is speculated to have been a result of an even earlier cataclysmic eruption, pointing to a possibility that it was once a volcano of considerable elevation that exploded, similar to Krakatoa.{{cite web | url=https://llda.gov.ph/laguna-de-bay/ | title=Laguna de Bay |publisher = Laguna Lake Development Authority|access-date=2023-03-05}}
Photographs
LagunaCaldera01.jpg|Laguna Caldera looking east
LagunaCaldera02.jpg|Laguna Caldera looking south-east
LagunaCaldera03.jpg|Laguna Caldera looking south
LagunaCaldera04.jpg|Laguna Caldera looking west
See also
References
{{Reflist}}
{{Laguna de Bay}}
{{Volcanoes of the Philippines}}
{{Authority control}}
{{DEFAULTSORT:Laguna Caldera}}
Category:Landforms of Laguna (province)
Category:Potentially active volcanoes of the Philippines