[timeout:300][out:json];
(
node(around:1000,32.73777,131.51313)["leisure"="nature_reserve"][~"^(addr:housenumber|.*name.*)$"~".",i];
way(around:1000,32.73777,131.51313)["leisure"="nature_reserve"][~"^(addr:housenumber|.*name.*)$"~".",i];
rel(around:1000,32.73777,131.51313)["leisure"="nature_reserve"][~"^(addr:housenumber|.*name.*)$"~".",i];
node(around:1000,32.73777,131.51313)[natural=peak][name];
way(around:1000,32.73777,131.51313)[natural=peak][name];
rel(around:1000,32.73777,131.51313)[natural=peak][name];
node(around:1000,32.73777,131.51313)[natural=volcano][name];
way(around:1000,32.73777,131.51313)[natural=volcano][name];
rel(around:1000,32.73777,131.51313)[natural=volcano][name];
);
out center tags;
大崩山（おおくえやま）は、宮崎県延岡市北西部にあり九州山地に属する大崩山群の主峰である。
Mount Ōkueyama (大崩山), also known as Mount Ōkue, is a Volcanic Mountain on the Japanese island of Kyushu. Part of an ancient volcanic formation known as the Okueyama Volcano-plutonic Complex, Mount Ōkueyama (and possibly several nearby volcanoes) experienced a massive eruption ~13.7 million years before present (13.7 Ma); it has been postulated that this eruption measured 8 on the Volcanic Explosivity Index, making the Ōkueyama eruption larger than any eruption in recorded history. The volcano is now considered to be extinct.
found a single match candidate
| mountain (Q8502) | natural=peak |