Snowboard bindings ThirtyTwo T32M Fava Fase fava_white (T.27.BNU.TEF.100)

ThirtyTwo T32M Fava Fase fava_white snowboard bindings are an advanced solution for snowboarding enthusiasts that combines modern technology with precise craftsmanship. They feature EVA cushioning, which effectively reduces shocks while riding. The bindings' flex level of 7/10 provides the right balance between stability and flexibility.

Modern technologies

The ThirtyTwo T32M Fava Fase snowboard bindings utilise the innovative FASE Fast Entry System. This solution makes putting on and taking off the bindings quick and convenient, saving time on the slopes. The Canted Footbed, or specially contoured base, supports the natural position of the feet, resulting in greater comfort and better control while riding.

Cushioning and construction

ThirtyTwo T32M Fava Fase fava_white snowboard bindings are characterised by EVA cushioning, which effectively dampens vibrations, increasing comfort during descents. The 7/10 flex of the bindings provides optimal stiffness, enabling precise maneuvering on different types of surfaces. This construction is suitable for both dynamic riding and stable descents.

Materials and user comfort

The ThirtyTwo T32M Fava Fase snowboard bindings are made from high-quality materials, ensuring durability and reliability in challenging conditions. The construction, based on Canted Footbed technology, supports foot ergonomics, reducing fatigue during prolonged use. This makes the product suitable for those who value comfort and efficiency.

ThirtyTwo T32M Fava Fase fava_white snowboard bindings - features:

• Utilise FASE Fast Entry System technology, making them easy to put on and take off;
• Have a Canted Footbed that supports the natural position of the feet;
• EVA cushioning reduces shocks while riding;
• Bindings have a flex of 7/10, providing the right stiffness and control;
• Made from high-quality materials, ensuring durability;
• The construction supports ergonomics and user comfort;
• Designed for dynamic riding and stable descents.