Hampshire Treasures
Volume 7 ( Havant)
Page 66 - Hayling West
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| Description and Date | Remarks | Protection | Grid Ref. and Punchcard No. | |
|---|---|---|---|---|
| Trees |
Newtown House Hotel, Manor Road. A group of austrian pine, and sycamore, weeping willow, oak, and monterey cypress standing separately, all in the hotel grounds. | T.P.O. No. 1079 |
SZ 715 998 1105 340 |
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| Trees |
St. Francis De Sales School, Beach Road. A group consisting mainly of holm oak, with oak and beech, and monterey pine, holm oak, and lime standing separately, all in the school grounds. | T.P.O. No. 1086 |
SZ 715 990 1105 341 |
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| Tree |
Site of Old Vicarage, Beach Road. A fine specimen of an evergreen oak. | SZ 715 993 1105 214 |
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| Trees and Shrubs |
Sinah Warren, Ferry Road. A large collection of mixed deciduous and coniferous varieties, a habitat for many wild birds. | SZ 696 997 1105 215 |
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| Woodland |
Honeyring Copse, junction of Church Road and Manor Road. Centred on grid reference given. | SU 721 006 1105 227 |
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| Tree |
St. Mary's Churchyard. An ancient yew, its' girth of 32 ft. is believed to be the largest in Hampshire. Ref: Churchyard and Immorality, (Cornish). | SU 722 000 1105 223 |
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| Woodland |
Pound Copse, junction of Church Road and Manor Road. Reference given locates the centre. | SU 723 006 1105 228 |
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| Trees |
Manor House, Manor Farm and environs. Mixed varieties including many fine oaks, forming an attractive setting to both the manor and the farm. | SU 721 009 1105 229 |
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| Trees |
Station Road, West Town. Line of conifers and fine single oak opposite. | SZ 710 997 1105 232 |
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| Tree |
Opposite Barley Mow Inn, West Town. Fine specimen of chestnut, one of the few large trees in this area. | SZ 711 996 1105 233 |
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| Woodland |
Opposite western end of Avenue Road and extending northwards along Havant Road. Attractive wooded area between road and shore. | SU 718 034 1105 238 |
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| Sarsen Stones |
St. Mary's Church. Flanking the south door, also two used as gravestones. Many are to be found in this area, they may originally have been incorporated in blocks of floating ice, which would account for their occasional presence in Pleitocene and Holocene gravels, later to form beach shingle. Ref: Sarsens, 1946, (Brentall), pp.419-439. | SU 722 000 1105 193 |
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