
Crane sits at the geological intersection of the expansive Harney Valley and the rising volcanic terrain to the east. This 1990 provisional survey by the U.S. Geological Survey captures the town's position as a gateway between the flat valley floor and the rugged features of the Crane Butte landscape. The map illustrates a critical water network essential for high-desert life, anchored by Crane Creek and supported by numerous mountain sources like Temple Spring and Krueger Spring. A distinctive topographical landmark, Crane Gap, provides a natural pass through the hills toward the Willow Basin. Further north, Krueger Field and the seasonal waters of Crowcamp Creek suggest the area's ongoing agricultural and ranching utility at the end of the twentieth century.
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This is the sole edition of this map. No revisions or reprints were ever made.