Globe vintage spinning

Vintage spinning globe, a piece combining historical cartography and decorative design, found in studies and collections.

About this subject

The vintage globe is an object dating back to the early days of modern cartography, when the first terrestrial globes were created in the late 15th century. The earliest preserved example is the Erdapfel by Martin Behaim from 1492, which did not yet include the Americas. These globes were built with a wooden sphere coated with paper or plaster, onto which maps were drawn or pasted. A brass meridian ring and a carved wooden base were common, as was the axis tilted at 23.5 degrees, representing Earth's axial tilt.

During the 18th and 19th centuries, globe production expanded with manufacturers like J. & G. Cary (London) and the Blaeu family (Amsterdam). They were used in schools, libraries, and homes as educational tools and symbols of scholarship. The sphere was rotated manually or by simple mechanisms, and the maps often reflected the geographical knowledge of the time, including colonial territories and exploration routes.

Today, vintage globes are collectible items valued for their aesthetic beauty and historical significance. They can be found with original patina or restored, and the quality of the map, color accuracy, and condition of the brass ring influence their value. Beyond decorative objects, they tell the story of the evolution of geographical knowledge and cartographic techniques.

Frequently Asked Questions

What is the oldest globe in the world?

The oldest surviving globe is the Erdapfel, made by Martin Behaim in 1492. It does not show the Americas because it was made before Columbus reached the continent.

How were vintage globes manufactured?

They were usually built with a wooden or plaster sphere, covered with paper on which the map was printed or hand-painted. The meridian was made of brass and the base of turned wood.

Why are globes tilted on their axis?

The tilt of approximately 23.5 degrees represents the angle of Earth's rotation axis relative to its orbital plane, which causes the seasons.