1954 Map of Dixonville

About this map

Dixonville and Singleton Valley anchor the western edge of this mid-century survey, where the valley floors transition into the dense terrain of the Umpqua National Forest. The landscape is defined by the complex drainage systems of the North Fork Deer Creek and Myrtle Creek, illustrating a rural economy tied to the land through timber and mineral extraction. Evidence of early industry and community life is scattered throughout the drainages, including a Sawmill on a tributary of Myrtle Creek and the Grange Hall near the local Cem.