Calne is a welcoming city where you can spend time checking out the bars. Nature lovers can visit Bowood Garden and North Wessex Downs. You might find that sights like Bowood Golf & Country Club and Calne Library are worth a visit.
Photo by Andy Hicks
Hotels in Calne
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Bowood Hotel Spa and Golf Resort
Bowood Hotel Spa and Golf Resort
9.8 out of 10, Exceptional, (6)
The price is $159
includes taxes & fees
$132 per night
Mar 11 - Mar 12
Lowest nightly price found within the past 24 hours based on a 1 night stay for 2 adults. Prices and availability subject to change. Additional terms may apply.
Top landmarks in Calne
Bowood Garden
Ready for an education in local botany? Bowood Garden should make your list of places to visit, located 1.6 mi (2.7 km) from central Calne. Want to stretch your legs some more? Head to Bowood Playground and Bowood Gardens, both a short walk away.
Learn more about Calne
Notable for its gardens, Calne features attractions such as Bowood Garden and Bowood Golf & Country Club. This welcoming city has something for everyone including bars as well as sights like North Wessex Downs and Calne Library. All are within a secluded setting.

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Find out more about Calne
Find out more about Calne
Calne Travel Information
Best Time to Visit | April, May and November |
---|---|
Average Stay | 2 days |
International Airport | Bristol Intl. Airport (BRS) |
Popular Sights | Avebury Stone Circle, Lacock Abbey and Bowood Garden |
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