Strawberry Schoolhouse
Strawberry Schoolhouse, Historic schoolhouse in Strawberry, Arizona.
Strawberry Schoolhouse is a single-room wooden school building in Strawberry, Arizona, constructed from pine logs. The structure features a sandstone foundation and walls made of ponderosa pine wood.
The schoolhouse was built in 1885 during Arizona's territorial period to serve the growing settlement. Operations ended in 1916 when student numbers declined, leading to its closure.
The building served the community as a gathering place for teaching, celebrations, and religious services. Residents came together here to strengthen their bonds and share important moments.
The Pine-Strawberry Archaeological and Historical Society maintains the building as a museum today. Visitors can view the interior with its original school furnishings and period materials.
The interior preserves original fixtures including double student desks, a large wall blackboard, and a pump organ from when the school operated. A Webster's dictionary among the artifacts shows what daily learning looked like.
Location: Arizona
GPS coordinates: 34.40580,-111.51900
Latest update: December 6, 2025 17:47
Arizona contains geological formations spanning millions of years alongside evidence of Spanish colonial settlement and prehistoric cultures. The landscape includes sandstone canyons such as Antelope Canyon X and Canyon de Chelly National Monument, extensive desert areas with saguaro and organ pipe cacti, and volcanic remnants at Sunset Crater. Historical sites include Spanish missions like Tumacácori, pueblo ruins at Montezuma Castle, and mining towns such as Bisbee and Jerome. The state holds significant paleontological sites at Petrified Forest National Park, where fossilized tree trunks from the Triassic period lie exposed, and cave systems like Kartchner Caverns with active speleothem formations. The Vermilion Cliffs region displays layered sandstone formations including The Wave, while the Chiricahua Mountains show volcanic rock pinnacles formed from welded ash. Waterfalls such as Havasu Falls and Grand Falls result from geological faulting and seasonal water flow. Archaeological sites document occupation by the Hohokam, Sinagua, and Ancestral Puebloans between 300 and 1400 CE. Tonto Natural Bridge forms one of the largest travertine bridges in North America, while Besh-Ba-Gowah shows Salado culture construction methods from the 13th century. The territory spans from the Sonoran Desert in the south to the Colorado Plateau in the north, creating distinct climate zones and ecosystems within a compact area.
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