[timeout:300][out:json];
(
node(around:1000,36.22000,-116.82720)[natural=desert][name];
way(around:1000,36.22000,-116.82720)[natural=desert][name];
rel(around:1000,36.22000,-116.82720)[natural=desert][name];
node(around:1000,36.22000,-116.82720)[natural=lake][name];
way(around:1000,36.22000,-116.82720)[natural=lake][name];
rel(around:1000,36.22000,-116.82720)[natural=lake][name];
node(around:1000,36.22000,-116.82720)[natural=water][name];
way(around:1000,36.22000,-116.82720)[natural=water][name];
rel(around:1000,36.22000,-116.82720)[natural=water][name];
node(around:1000,36.22000,-116.82720)[water=lake][name];
way(around:1000,36.22000,-116.82720)[water=lake][name];
rel(around:1000,36.22000,-116.82720)[water=lake][name];
node(around:1000,36.22000,-116.82720)[water=pond][name];
way(around:1000,36.22000,-116.82720)[water=pond][name];
rel(around:1000,36.22000,-116.82720)[water=pond][name];
);
out center tags;
Lake Manly was a pluvial lake in Death Valley, California. It forms occasionally in Badwater Basin after heavy rainfall, but at its maximum extent during the so-called "Blackwelder stand," ending approximately 120,000 years before present, the lake covered much of Death Valley with a surface area of 1,600 square kilometres (620 sq mi). Water levels varied through its history, and the chronology is further complicated by active tectonic processes that have modified the elevations of the various shorelines of Lake Manly; during the Blackwelder stage they reached 47–90 metres (154–295 ft) above sea level. The lake received water mainly from the Amargosa River and at various points from the Mojave River and Owens River. The lake and its substantial catchment favoured the spread of a number of aquatic species, including some lizards, pupfish and springsnails. The lake probably supported a substantial ecosystem, and a number of diatoms developed there.
no matches found
| body of water (Q15324) | natural=water |
| lake (Q23397) | water=lake |