Photo by Andy Hicks

Find 4 Star Hotels in Calne from AED 202

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Check availability on Calne 4 Star Hotels

Compare Calne 4 Star Hotels with updated room rates, reviews, and availability. Most hotels are fully refundable.

Bowood Hotel Spa and Golf Resort

4.0 star property
9.6 out of 10, Exceptional, (8)
"Great spa: clean and nice, wonderful area with gold fields and deers, modern spacious rooms with all the amenities. "
The price is AED 553
AED 664 total
includes taxes & fees
26 Mar - 27 Mar
Bowood Hotel Spa and Golf Resort

Dog and Partridge Inn

3.0 star property
8.4 out of 10, Very Good, (62)
"We had a lovely time here. The staff are all really friendly. I brought my little dog along as its dog friendly & they gave him some treats too. Had a great nights sleep, really comfortable & quite. The breakfast was great all you xan wat for £10 well worth it. Also there is a takeaway van in the car park which sells Kebabs etc so perfect for a Chicken Shish 🐔 👌 "
The price is AED 264
AED 316 total
includes taxes & fees
17 Mar - 18 Mar
Dog and Partridge Inn

The Lansdowne Hotel

3.0 star property
7.4 out of 10, Good, (339)
"Great staff. Courtyard room was small but fine. Bedcover very small. Noisy neighbours upstairs "
The price is AED 305
AED 365 total
includes taxes & fees
15 Mar - 16 Mar
The Lansdowne Hotel

The White Horse Inn

4.0 star property
9.4 out of 10, Exceptional, (130)
"Perfectly located for Stonehenge, Avebury, and Bath. William was brilliant all around"
The price is AED 330
AED 396 total
includes taxes & fees
17 Mar - 18 Mar
The White Horse Inn

The Duke Hotel

3.0 star property
10.0 out of 10, Exceptional, (1)
"The Duke Hotel is truly excellent. Fantastic rooms, nicely decorated with plenty of character and a fantastic shower and coffee machine. The food and service is exceptional. A truly fantastic place to stay. Highly recommended. "
The price is AED 433
AED 520 total
includes taxes & fees
28 Mar - 29 Mar
The Duke Hotel

Heritage Bed & Breakfast

3.0 star property
10.0 out of 10, Exceptional, (37)
"This is a great place to stay. My room and the whole house was spotless and very comfortable and cosy. The owners are lovely and welcoming. The breakfast was superb and I have yet to feel hungry, 9 hours later. I'll definitely be back when I'm in the area again. "
The price is AED 492
AED 591 total
includes taxes & fees
24 Mar - 25 Mar
Heritage Bed & Breakfast

The Bug & Spider

3.0 star property
8.4 out of 10, Very Good, (17)
"Fab place to stay, staff very friendly and welcoming food amazing. Entertainment was great Really enjoyed our stay. Definitely worth visiting again. "
The Bug & Spider
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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.

Learn more about Calne

Trip time! Discover the bars, gardens, and golf in secluded Calne.

Eroded hillside near Oliver's Castle The escarpment here is at the edge of chalk downland. Chalk readily absorbs rainwater so surface water in the form of streams and pools is only seen where the ground is below the water table, there us very little run-off. These gullies and ridges were probably formed by the water table breaking through to the surface and running down the hillside. The level of the water table has been reduced by extraction over the last hundred years or so. These gullies and ridges are easily seen from a distance and make a useful pointer to Oliver's Castle. My thanks to other contributors to Geograph for their help with these comments. Nigel Mykura has supplied the following: This is from tiscali reference: Such valleys are common on the dip slopes of chalk escarpments, and were probably formed by rivers. However, chalk is permeable (water passes through it) and so cannot retain surface water. Two popular theories have arisen to explain how this might have happened: 1) During the last ice age the chalk might have frozen and been rendered impermeable. During the summer thaw, water would then have flowed over the land, unable to sink into it, and river valleys would have been formed. When, after the ice age, the chalk thawed and became permeable again, rivers could no longer flow along the valleys and so these became dry. 2) At the end of the last ice age so much meltwater might have been created that the water table would be far higher than it is today. This would have enabled water to flow over the chalk surface without being absorbed, and create valleys. As the water table fell with time, however, water passed through the chalk once more and the valleys became dry. Good examples include Devil's Dyke, Fulking, England, and the Vale of the White Horse, Oxfordshire, England.
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Open Photo by Maurice Pullin (CC BY-SA) / Cropped from original