Moulin de la Gandouinière

The Moulin de la Gandouinière is a historic windmill located in La Chaize-le-Vicomte, France.

History

• The construction year of the Moulin de la Gandouinière is believed to date from the late 18th century, although exact details are not available.
• Originally built for grain milling purposes, the Moulin de la Gandouinière was used to grind wheat into flour for local bakeries.

Architecture

The mill is classified as a smock mill, with a single tower and a single sail. It features a traditional French windmill design, typical of those found in the region during this period.

Original Purpose

The Moulin de la Gandouinière was originally built for grain milling purposes.

Current Status and Use

The mill is currently a ruin, no longer operational. Despite its current state, it remains an important part of the region's cultural heritage.

Architectural Features and Construction Materials

• The mill's tower is constructed from limestone, while the base is made of brick.
• The windmill's sails are typically painted in bright colors to enhance visibility.

Location and Setting

The Moulin de la Gandouinière is situated in a picturesque landscape near La Chaize-le-Vicomte. It overlooks the surrounding countryside, providing stunning views of the Loire Valley.

Heritage Status and Preservation Efforts

As part of France's rich cultural heritage, the Moulin de la Gandouinière has been recognized as an important historical landmark. Efforts are ongoing to preserve this historic site for future generations.

Visiting Information

The Moulin de la Gandouinière is open to visitors who wish to explore its ruins and learn about its history. Visitors can access the mill by appointment, which should be made in advance to ensure availability.

Notable Historical Events or Famous Millers

Unfortunately, no notable historical events or famous millers are recorded for this specific windmill.

Technical Details

• The Moulin de la Gandouinière features a single sail and one grinding stone.
• Its machinery is typical of those found in 18th-century French windmills.