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===Geology=== Burns is in [[southeastern Oregon]] near the northern edge of the arid [[Harney Basin]]. The basin is part of the [[Northern Basin and Range ecoregion#High Lava Plains (80g)|High Lava Plains]], a region dominated by erupting volcanoes in the late [[Miocene]], five to ten million years ago. Centered on the [[Brothers Fault Zone]], which runs southeast–northwest between [[Steens Mountain]] and [[Bend, Oregon|Bend]], the High Lava Plains merge with the [[Blue Mountains (Pacific Northwest)|Blue Mountains]] to the north and the [[Basin and Range Province]] to the south.{{sfn|Orr|Orr|1999|pp=104–08}} Shallow basins formed by crustal stretching in the Basin and Range province were much wetter during the late [[Pleistocene]], up to 11,000 years ago, than they are in the 21st century. Lakes formed in these basins, including those in the southern part of the High Lava Plains. Among these, the largest depression was the Harney Basin, covering {{convert|5300|mi2|km2}}. Within the Harney Basin, ancient Malheur Lake—the 21st-century remnants of which include [[Malheur Lake]], [[Harney Lake]], and Mud Lake—covered {{convert|900|mi2|km2}} and extended as far north as Burns. These remnant wetlands have become the [[Malheur National Wildlife Refuge]].{{sfn|Orr|Orr|1999|pp=104–08}}
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