The New Forest

Also within

Hampshire CountyWiltshire County NEW FOREST National Park

Condition (Natural England)

Unit	Feature	Condition	Area (ha)	Assessed
SU159080	—	Favourable	1.02	2008-05-13
SU160117	—	Unfavourable Declining	2.4	2008-10-06
SU161083	—	Favourable	12.11	2009-02-26
SU161087	—	Unfavourable Declining	9.54	2015-02-06
SU161115	—	Favourable	12.11	2009-02-26
SU161119	—	Unfavourable Declining	1.2	2008-07-07
SU163119	—	Favourable	12.11	2009-02-26
SU163122	—	Favourable	12.11	2009-02-26
SU163132	—	Unfavourable Recovering	1.01	2010-03-31
SU166075	—	Unfavourable Recovering	4.41	2012-10-30
SU166115	—	Favourable	37.79	2016-01-18
SU167088	—	Unfavourable Recovering	29.96	2008-07-07
SU167098	—	Unfavourable Recovering	20.57	2016-01-15
SU167112	—	Favourable	3.18	2016-01-15
SU168126	—	Favourable	2.07	2016-01-15
SU168165	—	Favourable	13.43	2012-09-18
SU169105	—	Favourable	34.33	2012-10-30
SU169111	—	Favourable	12.11	2009-02-26
SU170044	—	Unfavourable Declining	1.52	2009-02-26
SU170082	—	Unfavourable Recovering	13.58	2012-10-30
SU170162	—	Unfavourable Recovering	144.25	2011-09-28
SU171044	—	Unfavourable Declining	0.71	2009-02-26
SU171125	—	Unfavourable Recovering	56.86	2011-10-06
SU171135	—	Unfavourable Recovering	1.66	2010-05-27
SU172057	—	Unfavourable Declining	0.99	2008-05-12
SU172083	—	Unfavourable Recovering	130.87	2012-10-30
SU172132	—	Unfavourable Recovering	1.5	2016-02-02
SU173136	—	Favourable	0.92	2015-07-03
SU174077	—	Favourable	14.35	2011-10-10
SU174103	—	Favourable	290.73	2016-01-15
SU175002	—	Unfavourable Recovering	5.86	2011-11-14
SU175003	—	Unfavourable Declining	0.86	2008-05-12
SU175066	—	Favourable	0.98	2008-07-04
SU175074	—	Unfavourable Recovering	6.5	2011-03-30
SU175113	—	Favourable	34.33	2012-10-30
SU175118	—	Favourable	34.33	2012-10-30
SU176021	—	Unfavourable Declining	1.66	2008-08-20
SU176076	—	Unfavourable Recovering	1.06	2011-10-10
SU176149	—	Unfavourable Recovering	0.35	2013-11-19
SU177126	—	Favourable	2.07	2016-01-15
SU177167	—	Unfavourable Recovering	144.25	2011-09-28
SU178022	—	Unfavourable Declining	9.28	2009-02-26
SU178079	—	Unfavourable No Change	0.63	2010-07-23
SU178082	—	Unfavourable Recovering	5.99	2015-01-19
SU178086	—	Unfavourable Recovering	5.99	2015-01-19
SU178092	—	Favourable	290.73	2016-01-15
SU178094	—	Unfavourable Recovering	1.01	2011-05-23
SU178096	—	Unfavourable Recovering	37.75	2019-03-22
SU179021	—	Unfavourable No Change	2.03	2009-02-26
SU179054	—	Unfavourable Recovering	14.24	2011-10-06
SU179079	—	Unfavourable Declining	3.59	2009-02-26
SU180024	—	Unfavourable Declining	12.66	2003-04-01
SU180086	—	Favourable	100.75	2012-09-18
SU180131	—	Favourable	254.44	2017-06-22
SU181036	—	Unfavourable Declining	0.26	2009-02-26
SU181053	—	Favourable	715.67	2012-08-31
SU181059	—	Unfavourable Declining	2.64	2024-03-21
SU181160	—	Favourable	1610.64	2011-09-28
SU182013	—	Favourable	31.56	2011-10-06
SU182032	—	Unfavourable Declining	12.66	2003-04-01
SU182064	—	Unfavourable Recovering	1.25	2019-03-26
SU182116	—	Unfavourable No Change	13.87	2019-10-17
SU183014	—	Favourable	31.56	2011-10-06
SU183020	—	Unfavourable Declining	1.37	2008-07-23
SU183027	—	Unfavourable Declining	3.7	2009-02-26
SU183036	—	Unfavourable Declining	3.7	2009-02-26
SU183077	—	Unfavourable Recovering	55.05	2016-02-11
SU184018	—	Favourable	23.91	2011-10-06
SU184020	—	Unfavourable Declining	8.88	2009-02-26
SU184027	—	Unfavourable Declining	50.49	2009-02-26
SU184043	—	Unfavourable Recovering	7.71	2015-01-29
SU184050	—	Favourable	715.67	2012-08-31
SU184061	—	Favourable	17.2	2012-06-26
SU184093	—	Favourable	282.63	2012-07-05
SU184156	—	Unfavourable Recovering	9.57	2011-11-11
SU184164	—	Unfavourable Recovering	53.15	2012-08-29
SU184184	—	Unfavourable Declining	1.57	2010-03-31
SU185007	—	Favourable	31.57	2011-10-06
SU185010	—	Favourable	31.56	2011-10-06
SU185040	—	Favourable	715.67	2012-08-31
SU185046	—	Unfavourable Recovering	7.69	2015-01-29
SU185071	—	Unfavourable Recovering	24.59	2015-02-04
SU185089	—	Unfavourable Recovering	35.01	2017-02-09
SU185131	—	Favourable	11.19	2012-06-27
SU185145	—	Unfavourable Recovering	19.68	2013-12-05
SU186014	—	Favourable	31.57	2011-10-06
SU186077	—	Unfavourable No Change	46.3	2019-10-17
SU186109	—	Favourable	254.44	2017-06-22
SU186148	—	Favourable	254.44	2017-06-22
SU186170	—	Unfavourable Recovering	0.5	2011-03-29
SU187041	—	Unfavourable Recovering	71.13	2015-01-29
SU187053	—	Unfavourable Recovering	71.13	2015-01-29
SU187057	—	Favourable	715.67	2012-08-31
SU187075	—	Favourable	282.63	2012-07-05
SU187151	—	Favourable	254.44	2017-06-22
SU188010	—	Favourable	31.57	2011-10-06
SU188126	—	Unfavourable No Change	23.38	2019-10-17
SU188169	—	Unfavourable Recovering	1.63	2011-03-29
SU189066	—	Unfavourable Recovering	43.68	2012-06-26
SU189086	—	Favourable	88.58	2016-02-05
SU190000	—	Unfavourable Recovering	5.23	2008-07-10
SU190031	—	Unfavourable Recovering	161.45	2015-01-29
SU190139	—	Favourable	48.28	2012-06-27
SU191012	—	Unfavourable Recovering	73.36	2013-12-05
SU191060	—	Favourable	192.05	2017-05-30
SU191113	—	Favourable	13.65	2011-09-28
SU191123	—	Favourable	254.44	2017-06-22
SU191132	—	Unfavourable No Change	37.87	2019-10-17
SU191152	—	Favourable	254.44	2017-06-22
SU191162	—	Unfavourable Recovering	7.69	2013-12-05
SU191177	—	Favourable	8.43	2016-01-15
SU192129	—	Favourable	1610.64	2011-09-28
SU192189	—	Favourable	0.49	2017-02-14
SU193045	—	Unfavourable Recovering	161.45	2015-01-29
SU193077	—	Favourable	65.74	2017-05-15
SU193120	—	Unfavourable Recovering	37.12	2011-09-28
SU193157	—	Favourable	254.44	2017-06-22
SU193191	—	Favourable	3.56	2016-05-03
SU194015	—	Favourable	36.49	2012-08-31
SU194046	—	Favourable	715.67	2012-08-31
SU194072	—	Favourable	23.27	2011-09-28
SU194143	—	Unfavourable Recovering	37.08	2011-09-28
SU194147	—	Unfavourable Recovering	3.42	2013-12-05
SU194148	—	Favourable	7.29	2011-09-28
SU194177	—	Unfavourable Recovering	1.28	2015-01-19
SU195022	—	Favourable	715.67	2012-08-31
SU195129	—	Favourable	1610.64	2011-09-28
SU195145	—	Unfavourable Recovering	9.62	2015-02-04
SU195168	—	Unfavourable Recovering	53.15	2012-08-29
SU196004	—	Favourable	706.94	2017-08-12
SU196068	—	Favourable	282.63	2012-07-05
SU196110	—	Favourable	282.63	2012-07-05
SU196178	—	Unfavourable Recovering	1.08	2015-01-19
SU197103	—	Favourable	38.89	2011-09-28
SU197146	—	Unfavourable Recovering	37.08	2011-09-28
SU197182	—	Favourable	146.38	2022-08-04
SU198010	—	Favourable	36.49	2012-08-31
SU198043	—	Favourable	192.05	2017-05-30
SU198074	—	Unfavourable Recovering	21.69	2012-05-29
SU198103	—	Unfavourable Recovering	1.5	2013-12-05
SU198148	—	Unfavourable Recovering	1.93	2013-12-05
SU198155	—	Unfavourable Recovering	4.11	2013-12-05
SU198176	—	Unfavourable Recovering	40.09	2011-09-28
SU199021	—	Unfavourable Recovering	185.99	2013-12-05
SU199047	—	Favourable	192.05	2017-05-30
SU199080	—	Favourable	100.75	2012-09-18
SU199083	—	Unfavourable No Change	15.78	2016-11-17
SU199186	—	Favourable	5.43	2016-01-15
SU200030	—	Favourable	14.02	2017-07-25
SU200053	—	Favourable	18.36	2011-09-28
SU200062	—	Favourable	61.57	2017-09-26
SU200136	—	Favourable	23.32	2011-09-28
SU201081	—	Favourable	19.73	2022-07-07
SU201091	—	Unfavourable Recovering	173.71	2013-12-06
SU201126	—	Unfavourable No Change	32.63	2019-10-17
SU201160	—	Unfavourable Recovering	23.48	2012-08-29
SU202025	—	Unfavourable Declining	0.38	2008-08-20
SU202128	—	Unfavourable Recovering	40.98	2016-02-12
SU202174	—	Unfavourable Recovering	56.72	2016-02-12
SU202181	—	Unfavourable Recovering	2.24	2015-01-19
SU203008	—	Unfavourable Recovering	185.99	2013-12-05
SU203018	—	Unfavourable Recovering	185.99	2013-12-05
SU203060	—	Favourable	31.01	2011-09-28
SU203105	—	Favourable	10.75	2015-01-22
SU203113	—	Unfavourable Recovering	55.1	2015-02-04
SU203136	—	Favourable	23.32	2011-09-28
SU204107	—	Favourable	282.63	2012-07-05
SU205046	—	Unfavourable Recovering	12.51	2015-11-25
SU205119	—	Favourable	254.44	2017-06-22
SU205150	—	Unfavourable Recovering	62.69	2013-12-05
SU206023	—	Unfavourable Recovering	0.6	2023-11-23
SU206050	—	Favourable	715.67	2012-08-31
SU207031	—	Unfavourable No Change	1.76	2024-07-16
SU207057	—	Favourable	715.67	2012-08-31
SU207135	—	Unfavourable No Change	126.47	2019-10-17
SU207180	—	Unfavourable Recovering	13.93	2009-01-30
SU208047	—	Favourable	192.05	2017-05-30
SU208059	—	Favourable	715.67	2012-08-31
SU208084	—	Favourable	282.63	2012-07-05
SU208169	—	Favourable	254.44	2017-06-22
SU208204	—	Favourable	2.35	2020-07-30
SU209000	—	Favourable	22.6	2012-07-06
SU209057	—	Favourable	715.67	2012-08-31
SU209099	—	Unfavourable Recovering	109.41	2012-05-29
SU209203	—	Unfavourable Recovering	2.17	2009-07-07
SU210063	—	Unfavourable Recovering	104.82	2015-01-29
SU210130	—	Unfavourable Recovering	78.12	2017-02-09
SU211017	—	Unfavourable Recovering	69.85	2015-01-29
SU211043	—	Favourable	715.67	2012-08-31
SU211078	—	Favourable	282.63	2012-07-05
SU211083	—	Unfavourable Recovering	45.55	2017-02-20
SU211086	—	Favourable	282.63	2012-07-05
SU211088	—	Favourable	17.28	2012-06-26
SU211144	—	Favourable	2.54	2012-10-08
SU211173	—	Unfavourable Recovering	24.78	2012-08-29
SU211180	—	Unfavourable Recovering	3.7	2013-12-05
SU212046	—	Unfavourable Recovering	34.79	2015-01-29
SU212109	—	Unfavourable Recovering	4.41	2022-09-01
SU212115	—	Unfavourable Recovering	38.57	2023-03-07
SU212150	—	Unfavourable Recovering	2.28	2014-08-12
SU213013	—	Unfavourable Recovering	185.99	2013-12-05
SU213071	—	Favourable	715.67	2012-08-31
SU213080	—	Favourable	282.63	2012-07-05
SU213164	—	Favourable	254.44	2017-06-22
SU213180	—	Unfavourable Declining	0.57	2013-09-20
SU213183	—	Unfavourable Recovering	1.43	2009-07-08
SU214006	—	Favourable	46.46	2013-12-05
SU214093	—	Favourable	15.22	2015-01-29
SU214126	—	Unfavourable Recovering	40.98	2016-02-12
SU215004	—	Favourable	192.05	2017-05-30
SU215042	—	Favourable	715.67	2012-08-31
SU215082	—	Favourable	282.63	2012-07-05
SU215123	—	Favourable	1610.64	2011-09-28
SU215158	—	Favourable	1610.64	2011-09-28
SU216022	—	Favourable	706.94	2017-08-12
SU216137	—	Favourable	1610.64	2011-09-28
SU217053	—	Favourable	14.33	2021-09-03
SU217058	—	Favourable	73.32	2011-09-28
SU217062	—	Unfavourable Recovering	71.13	2015-01-29
SU217189	—	Unfavourable Recovering	0.61	2022-08-15
SU217217	—	Unfavourable Recovering	1.93	2011-06-23
SU218026	—	Favourable	39.48	2008-08-15
SU218028	—	Favourable	192.05	2017-05-30
SU218050	—	Unfavourable Recovering	17.1	2022-05-11
SU218150	—	Unfavourable No Change	195.3	2019-10-17
SU218199	—	Favourable	0.83	2020-07-30
SU218202	—	Unfavourable Recovering	1.1	2013-09-20
SU219099	—	Favourable	10.29	2022-07-07
SU219109	—	Favourable	20.52	2022-07-07
SU219119	—	Unfavourable Recovering	57.83	2011-09-28
SU219136	—	Favourable	15.67	2016-02-05
SU219188	—	Unfavourable Recovering	1.09	2022-08-15
SU220035	—	Unfavourable Recovering	185.99	2013-12-05
SU220115	—	Favourable	100.75	2012-09-18
SU220139	—	Favourable	11.94	2012-09-18
SU220174	—	Favourable	15.95	2022-11-08
SU221056	—	Unfavourable Recovering	162.02	2011-09-28
SU221090	—	Favourable	27.38	2011-09-29
SU221180	—	Unfavourable Declining	4.54	2020-07-30
SU221197	—	Unfavourable Declining	1.79	2013-09-20
SU222003	—	Unfavourable Recovering	142.71	2023-03-07
SU222049	—	Unfavourable Recovering	162.02	2011-09-28
SU222093	—	Favourable	4.63	2012-07-05
SU223073	—	Unfavourable Recovering	16.26	2022-06-28
SU223075	—	Unfavourable Recovering	64.76	2013-12-05
SU223085	—	Favourable	715.67	2012-08-31
SU223095	—	Favourable	4.63	2012-07-05
SU223128	—	Favourable	38.84	2012-08-31
SU224068	—	Favourable	63.49	2022-06-16
SU224075	—	Favourable	11.2	2017-07-25
SU224124	—	Favourable	44.89	2019-03-22
SU224134	—	Favourable	1610.64	2011-09-28
SU225018	—	Favourable	706.94	2017-08-12
SU225042	—	Favourable	192.05	2017-05-30
SU225078	—	Unfavourable Recovering	64.76	2013-12-05
SU225101	—	Unfavourable Recovering	2.89	2013-12-05
SU225120	—	Favourable	282.63	2012-07-05
SU225154	—	Unfavourable Declining	74.01	2019-10-17
SU226056	—	Unfavourable No Change	16.19	2016-11-17
SU226089	—	Favourable	27.38	2011-09-29
SU226094	—	Unfavourable Recovering	41.74	2012-06-26
SU226120	—	Favourable	5.78	2015-01-22
SU226128	—	Unfavourable Recovering	13.77	2016-02-12
SU226135	—	Favourable	254.44	2017-06-22
SU226139	—	Unfavourable Recovering	2.15	2012-08-31
SU227059	—	Unfavourable Recovering	162.02	2011-09-28
SU227086	—	Favourable	8.48	2017-02-14
SU227112	—	Unfavourable Recovering	4.01	2013-12-05
SU227140	—	Favourable	1610.64	2011-09-28
SU227143	—	Favourable	16.22	2012-09-18
SU228045	—	Unfavourable Recovering	16.41	2016-02-12
SU228048	—	Favourable	10.22	2011-09-28
SU228073	—	Favourable	10.06	2022-06-28
SU228083	—	Unfavourable Recovering	29.57	2016-02-12
SU228124	—	Unfavourable Recovering	28.83	2016-02-12
SU228131	—	Favourable	38.84	2012-08-31
SU228139	—	Favourable	67.92	2017-06-20
SU229006	—	Unfavourable Recovering	19.72	2013-12-05
SU229105	—	Unfavourable Recovering	101.45	2012-06-26
SU229122	—	Favourable	100.75	2012-09-18
SU229162	—	Unfavourable Recovering	15.91	2012-10-08
SU230005	—	Favourable	2.27	2015-07-15
SU230064	—	Favourable	31.3	2011-09-28
SU230089	—	Favourable	715.67	2012-08-31
SU230092	—	Unfavourable Recovering	29.57	2016-02-12
SU231035	—	Unfavourable Recovering	57.21	2015-01-29
SU231038	—	Favourable	192.05	2017-05-30
SU231052	—	Unfavourable Recovering	159.53	2011-09-28
SU231076	—	Favourable	715.67	2012-08-31
SU231080	—	Favourable	14.67	2011-09-28
SU231116	—	Favourable	10.88	2013-12-05
SU231132	—	Favourable	14.52	2017-06-22
SU231197	—	Unfavourable Declining	7.16	2013-09-20
SU232016	—	Unfavourable Recovering	185.99	2013-12-05
SU232090	—	Favourable	11.2	2017-07-25
SU232109	—	Favourable	4.32	2019-06-21
SU232135	—	Favourable	254.44	2017-06-22
SU232195	—	Unfavourable Declining	2.21	2013-09-20
SU233036	—	Favourable	9.24	2016-02-05
SU233065	—	Unfavourable Recovering	165.89	2011-10-10
SU233084	—	Favourable	11.2	2017-07-25
SU233097	—	Favourable	100.75	2012-09-18
SU233107	—	Favourable	6.8	2012-07-05
SU233112	—	Favourable	4.32	2019-06-21
SU234004	—	Unfavourable Recovering	19.88	2015-02-04
SU234058	—	Unfavourable Recovering	159.53	2011-09-28
SU234073	—	Unfavourable Recovering	165.89	2011-10-10
SU234091	—	Favourable	155.46	2022-08-09
SU234100	—	Favourable	11.25	2012-09-18
SU234128	—	Unfavourable Recovering	20.92	2011-09-28
SU234153	—	Unfavourable Recovering	79.02	2012-08-29
SU235004	—	Favourable	98.37	2012-08-31
SU235086	—	Favourable	24.76	2012-07-06
SU235114	—	Favourable	922.91	2011-09-28
SU235166	—	Favourable	44.88	2022-11-08
SU236022	—	Favourable	706.94	2017-08-12
SU236068	—	Unfavourable Recovering	33.08	2013-12-06
SU236221	—	Unfavourable Declining	2.69	2023-12-07
SU237045	—	Unfavourable Recovering	158.06	2016-02-12
SU237103	—	Unfavourable Declining	74.82	2017-03-17
SU237130	—	Unfavourable Recovering	11.54	2015-01-22
SU238016	—	Unfavourable Recovering	185.99	2013-12-05
SU238119	—	Favourable	100.75	2012-09-18
SU238129	—	Favourable	13.64	2011-09-28
SU238192	—	Unfavourable No Change	0.92	2013-09-20
SU238220	—	Unfavourable Declining	1.4	2023-12-07
SU239072	—	Unfavourable Recovering	165.89	2011-10-10
SU239084	—	Favourable	10.29	2016-05-23
SU239088	—	Unfavourable Recovering	16.89	2009-12-18
SU239097	—	Favourable	270.67	2011-09-28
SU239122	—	Favourable	100.75	2012-09-18
SU239132	—	Unfavourable Recovering	26.3	2011-09-28
SU239193	—	Unfavourable No Change	1.28	2013-09-20
SU240051	—	Unfavourable Recovering	7.37	2016-02-12
SU240161	—	Favourable	24.92	2011-09-28
SU241037	—	Favourable	192.05	2017-05-30
SU241056	—	Unfavourable Recovering	165.89	2011-10-10
SU241107	—	Favourable	270.67	2011-09-28
SU241109	—	Favourable	57.71	2020-10-30
SU241113	—	Favourable	100.75	2012-09-18
SU241134	—	Favourable	13.64	2011-09-28
SU242033	—	Unfavourable Recovering	84.16	2015-01-29
SU242122	—	Favourable	4.98	2022-09-01
SU242157	—	Favourable	254.44	2017-06-22
SU243062	—	Unfavourable Recovering	159.53	2011-09-28
SU243100	—	Favourable	28.6	2012-07-06
SU243106	—	Favourable	155.46	2022-08-09
SU243108	—	Favourable	270.67	2011-09-28
SU243110	—	Favourable	100.75	2012-09-18
SU243160	—	Favourable	24.92	2011-09-28
SU244009	—	Unfavourable Recovering	204.67	2012-11-21
SU244116	—	Favourable	63.68	2017-06-08
SU244159	—	Favourable	254.44	2017-06-22
SU245000	—	Unfavourable Recovering	27.37	2012-11-19
SU245139	—	Favourable	18.78	2011-09-28
SU246002	—	Favourable	2.69	2020-12-17
SU246080	—	Unfavourable Recovering	14.64	2013-12-05
SU246111	—	Favourable	5.91	2017-02-10
SU246119	—	Favourable	922.91	2011-09-28
SU247037	—	Favourable	9.24	2016-02-05
SU247068	—	Favourable	1.89	2020-07-23
SU247099	—	Favourable	18.28	2011-09-28
SU247152	—	Favourable	254.44	2017-06-22
SU247163	—	Favourable	254.44	2017-06-22
SU248001	—	Favourable	2.73	2020-12-17
SU248062	—	Unfavourable Recovering	159.53	2011-09-28
SU248108	—	Favourable	155.46	2022-08-09
SU248119	—	Unfavourable Recovering	17.06	2017-07-13
SU249001	—	Favourable	2.55	2009-02-26
SU249027	—	Unfavourable Recovering	104.89	2012-08-31
SU249049	—	Unfavourable Recovering	164.61	2024-03-21
SU249056	—	Favourable	155.46	2022-08-09
SU249143	—	Unfavourable Recovering	85.49	2012-09-19
SU249180	—	Favourable	1.42	2016-06-07
SU250042	—	Favourable	171.72	2011-09-28
SU250075	—	Favourable	171.72	2011-09-28
SU250105	—	Favourable	270.67	2011-09-28
SU250133	—	Unfavourable Recovering	29.82	2012-09-19
SU250180	—	Favourable	1.46	2020-07-30
SU251044	—	Unfavourable Recovering	40.73	2009-11-26
SU251071	—	Favourable	8.51	2016-02-10
SU251077	—	Unfavourable Recovering	11.58	2013-12-05
SU251101	—	Favourable	270.67	2011-09-28
SU251196	—	Unfavourable Declining	1.79	2013-09-20
SU252038	—	Favourable	38.58	2015-02-04
SU252073	—	Favourable	171.72	2011-09-28
SU252093	—	Unfavourable Recovering	292.37	2016-02-12
SU252104	—	Favourable	270.67	2011-09-28
SU253079	—	Unfavourable Recovering	11.58	2013-12-05
SU253107	—	Favourable	25.73	2017-02-14
SU253124	—	Unfavourable Recovering	43.62	2012-09-19
SU253128	—	Unfavourable Declining	16.99	2017-07-13
SU253169	—	Unfavourable Recovering	24.49	2016-02-12
SU253181	—	Favourable	0.71	2020-07-30
SU253185	—	Unfavourable Recovering	1.55	2010-10-07
SU254033	—	Unfavourable Recovering	8.27	2017-02-13
SU254101	—	Favourable	270.67	2011-09-28
SU254103	—	Favourable	155.46	2022-08-09
SU254144	—	Unfavourable Recovering	37.55	2012-09-19
SU255097	—	Unfavourable Recovering	31.98	2011-09-28
SU256029	—	Favourable	1104.58	2017-08-07
SU256076	—	Favourable	2.62	2017-02-10
SU256120	—	Unfavourable Recovering	12.17	2014-05-07
SU256141	—	Favourable	4.95	2011-09-28
SU256149	—	Unfavourable Recovering	33.28	2012-09-19
SU256181	—	Favourable	2.22	2020-07-30
SU256185	—	Unfavourable Recovering	1.49	2014-01-16
SU257027	—	Favourable	91.2	2012-08-31
SU257031	—	Favourable	1104.58	2017-08-07
SU257064	—	Unfavourable Recovering	208.99	2016-02-12
SU257076	—	Favourable	171.72	2011-09-28
SU257132	—	Unfavourable Recovering	89.74	2011-09-28
SU257176	—	Favourable	254.44	2017-06-22
SU258084	—	Unfavourable Recovering	115.38	2016-02-12
SU258103	—	Favourable	5.69	2021-11-25
SU258162	—	Favourable	273.89	2017-05-12
SU259042	—	Unfavourable Recovering	93.91	2011-09-28
SU259151	—	Favourable	57.71	2020-10-30
SU260122	—	Favourable	100.75	2012-09-18
SU260125	—	Favourable	44.59	2011-09-28
SU260142	—	Favourable	23.42	2011-09-28
SU260152	—	Favourable	100.75	2012-09-18
SU260226	—	Favourable	7.58	2016-12-05
SU261073	—	Unfavourable Recovering	97.43	2016-02-12
SU261121	—	Favourable	100.75	2012-09-18
SU262051	—	Unfavourable Recovering	137.04	2016-02-11
SU262138	—	Favourable	50.34	2012-09-18
SU262147	—	Favourable	57.71	2020-10-30
SU262154	—	Favourable	254.44	2017-06-22
SU262174	—	Favourable	254.44	2017-06-22
SU263013	—	Favourable	98.37	2012-08-31
SU263089	—	Unfavourable Recovering	108.56	2016-02-12
SU263103	—	Unfavourable Recovering	11.72	2024-02-15
SU263104	—	Favourable	2.36	2024-03-21
SU263130	—	Favourable	100.75	2012-09-18
SU263153	—	Favourable	100.75	2012-09-18
SU263175	—	Unfavourable Recovering	2.15	2012-03-30
SU264000	—	Unfavourable No Change	31.73	2017-05-13
SU264103	—	Favourable	5.8	2024-03-21
SU264137	—	Favourable	23.42	2011-09-28
SU265009	—	Favourable	1104.58	2017-08-07
SU265031	—	Favourable	17.29	2020-07-15
SU265034	—	Unfavourable Recovering	15.1	2011-09-28
SU265089	—	Unfavourable Recovering	108.56	2016-02-12
SU265094	—	Unfavourable Recovering	108.56	2016-02-12
SU265112	—	Unfavourable Recovering	2.37	2011-11-14
SU265123	—	Favourable	44.59	2011-09-28
SU266011	—	Favourable	98.37	2012-08-31
SU266111	—	Unfavourable Recovering	4.44	2012-01-24
SU266124	—	Favourable	100.75	2012-09-18
SU267064	—	Favourable	270.67	2011-09-28
SU267068	—	Favourable	22.98	2012-07-06
SU267082	—	Favourable	155.46	2022-08-09
SU267084	—	Unfavourable Recovering	108.56	2016-02-12
SU267089	—	Favourable	155.46	2022-08-09
SU267093	—	Favourable	14.41	2024-03-19
SU267106	—	Unfavourable Recovering	97.11	2024-03-19
SU267143	—	Favourable	100.75	2012-09-18
SU268062	—	Favourable	139.17	2017-09-05
SU268064	—	Favourable	204.75	2011-09-28
SU268113	—	Unfavourable Recovering	9.82	2023-03-07
SU268154	—	Favourable	5.92	2020-07-30
SU269004	—	Favourable	98.37	2012-08-31
SU269018	—	Unfavourable Recovering	46.24	2013-12-06
SU269035	—	Unfavourable Recovering	65.51	2015-02-04
SU269077	—	Favourable	19.93	2017-03-16
SU269086	—	Favourable	155.46	2022-08-09
SU269114	—	Favourable	7.77	2008-07-07
SU269124	—	Favourable	44.59	2011-09-28
SU269140	—	Favourable	4.23	2008-05-12
SU269174	—	Favourable	22.49	2016-01-15
SU270041	—	Unfavourable Recovering	65.51	2015-02-04
SU270061	—	Favourable	204.75	2011-09-28
SU270067	—	Favourable	270.67	2011-09-28
SU270090	—	Favourable	270.67	2011-09-28
SU270179	—	Favourable	35.43	2012-10-08
SU271050	—	Unfavourable Recovering	102.69	2011-09-28
SU271075	—	Favourable	270.67	2011-09-28
SU271077	—	Favourable	155.46	2022-08-09
SU271080	—	Favourable	270.67	2011-09-28
SU271131	—	Favourable	3.15	2016-05-03
SU272008	—	Unfavourable Recovering	35.84	2016-02-11
SU272029	—	Unfavourable Recovering	9.28	2013-12-06
SU272056	—	Unfavourable Recovering	6.22	2012-11-09
SU272062	—	Favourable	139.17	2017-09-05
SU272097	—	Unfavourable Declining	2.53	2008-08-15
SU273068	—	Favourable	15.17	2017-03-16
SU273078	—	Unfavourable Recovering	108.56	2016-02-12
SU273186	—	Favourable	35.43	2012-10-08
SU274014	—	Favourable	98.37	2012-08-31
SU274032	—	Unfavourable Recovering	52.16	2011-09-28
SU274036	—	Unfavourable Recovering	39.85	2009-02-26
SU274055	—	Favourable	139.17	2017-09-05
SU274077	—	Favourable	270.67	2011-09-28
SU275023	—	Favourable	1104.58	2017-08-07
SU275076	—	Favourable	155.46	2022-08-09
SU276083	—	Favourable	3.0	2015-01-29
SU276087	—	Favourable	155.46	2022-08-09
SU276182	—	Favourable	140.52	2012-10-08
SU276190	—	Favourable	35.43	2012-10-08
SU277042	—	Favourable	6.03	2017-08-31
SU277074	—	Favourable	15.35	2021-06-21
SU277084	—	Unfavourable Recovering	108.56	2016-02-12
SU277190	—	Favourable	2.94	2016-01-15
SU278001	—	Favourable	98.37	2012-08-31
SU278026	—	Favourable	139.17	2017-09-05
SU278029	—	Favourable	17.22	2017-09-05
SU278073	—	Favourable	15.35	2021-06-21
SU279018	—	Unfavourable Recovering	41.3	2014-02-18
SU279048	—	Unfavourable Recovering	20.82	2013-12-06
SU279145	—	Unfavourable Recovering	4.04	2011-03-24
SU279178	—	Favourable	35.43	2012-10-08
SU280014	—	Unfavourable Recovering	3.51	2012-08-31
SU280015	—	Unfavourable Recovering	45.26	2013-12-06
SU280030	—	Favourable	7.58	2016-12-05
SU280042	—	Favourable	50.48	2017-02-10
SU280053	—	Favourable	22.38	2017-02-13
SU280182	—	Unfavourable Recovering	83.55	2009-03-25
SU281044	—	Favourable	139.17	2017-09-05
SU281060	—	Favourable	204.75	2011-09-28
SU281075	—	Favourable	140.16	2021-06-18
SU281129	—	Favourable	100.75	2012-09-18
SU281188	—	Favourable	35.43	2012-10-08
SU281193	—	Favourable	6.44	2016-01-15
SU282008	—	Unfavourable Recovering	41.22	2012-10-08
SU282039	—	Favourable	139.17	2017-09-05
SU282056	—	Favourable	12.83	2017-02-10
SU282187	—	Favourable	6.45	2013-12-05
SU282189	—	Favourable	2.56	2016-01-15
SU283000	—	Favourable	98.37	2012-08-31
SU283036	—	Unfavourable No Change	8.0	2017-09-22
SU283070	—	Unfavourable Recovering	12.35	2015-01-30
SU283075	—	Favourable	15.35	2021-06-21
SU283191	—	Favourable	35.43	2012-10-08
SU284050	—	Unfavourable Recovering	9.62	2013-12-06
SU284067	—	Unfavourable Recovering	12.35	2015-01-30
SU284157	—	Favourable	23.88	2014-11-11
SU284181	—	Unfavourable Recovering	83.55	2009-03-25
SU285134	—	Favourable	100.75	2012-09-18
SU285167	—	Favourable	3.67	2014-11-04
SU286047	—	Unfavourable Recovering	12.15	2013-12-06
SU286126	—	Unfavourable Recovering	85.12	2011-09-28
SU286152	—	Favourable	301.78	2012-11-09
SU287054	—	Unfavourable Recovering	65.32	2016-02-11
SU288027	—	Unfavourable Recovering	23.16	2024-03-27
SU288119	—	Favourable	173.12	2011-09-28
SU289169	—	Unfavourable Recovering	2.6	2015-01-19
SU290020	—	Favourable	30.66	2020-07-15
SU290060	—	Favourable	139.17	2017-09-05
SU290061	—	Unfavourable Recovering	2.01	2013-12-06
SU290153	—	Favourable	23.88	2014-11-11
SU291117	—	Favourable	41.79	2012-09-21
SU291158	—	Favourable	10.4	2012-09-19
SU291164	—	Unfavourable Recovering	8.05	2015-01-19
SU292000	—	Favourable	98.37	2012-08-31
SU292003	—	Favourable	1104.58	2017-08-07
SU292050	—	Unfavourable Recovering	41.63	2023-03-07
SU292063	—	Unfavourable Recovering	36.77	2013-12-06
SU292113	—	Favourable	41.79	2012-09-21
SU292129	—	Unfavourable Recovering	13.58	2022-04-27
SU292133	—	Favourable	24.98	2011-09-28
SU293026	—	Favourable	1104.58	2017-08-07
SU293057	—	Favourable	139.17	2017-09-05
SU293107	—	Favourable	41.79	2012-09-21
SU293141	—	Favourable	7.29	2012-09-21
SU294001	—	Favourable	98.37	2012-08-31
SU294019	—	Unfavourable Declining	0.58	2008-08-20
SU294032	—	Favourable	123.94	2017-09-12
SU294092	—	Unfavourable Recovering	160.11	2015-01-30
SU294167	—	Favourable	11.95	2012-09-19
SU295038	—	Unfavourable Recovering	38.89	2013-12-06
SU295063	—	Favourable	139.17	2017-09-05
SU295096	—	Favourable	16.33	2011-09-28
SU295127	—	Unfavourable Recovering	160.11	2015-01-30
SU295152	—	Favourable	23.88	2014-11-11
SU296092	—	Unfavourable Recovering	8.7	2017-02-10
SU296094	—	Favourable	542.25	2017-07-13
SU296112	—	Unfavourable Recovering	20.24	2009-11-26
SU296133	—	Favourable	24.98	2011-09-28
SU296158	—	Favourable	2.99	2012-09-21
SU297062	—	Unfavourable Recovering	7.81	2015-01-30
SU297090	—	Unfavourable Recovering	160.11	2015-01-30
SU298058	—	Favourable	85.72	2017-09-19
SU298109	—	Unfavourable Recovering	88.1	2011-09-28
SU298119	—	Favourable	6.04	2017-02-08
SU298122	—	Favourable	42.19	2011-09-28
SU300015	—	Unfavourable Declining	1.36	2009-03-26
SU300105	—	Unfavourable Recovering	88.1	2011-09-28
SU300109	—	Favourable	8.35	2013-12-06
SU301017	—	Favourable	3.05	2009-02-26
SU301042	—	Unfavourable Recovering	23.16	2024-03-27
SU301047	—	Unfavourable Recovering	20.24	2009-11-26
SU301087	—	Unfavourable Recovering	160.11	2015-01-30
SU301096	—	Favourable	542.25	2017-07-13
SU301113	—	Unfavourable Recovering	88.1	2011-09-28
SU303000	—	Favourable	1104.58	2017-08-07
SU303017	—	Unfavourable Recovering	3.79	2010-11-08
SU303040	—	Unfavourable Declining	33.25	2011-09-28
SU303049	—	Favourable	6.48	2016-05-12
SU303097	—	Unfavourable Recovering	160.11	2015-01-30
SU304088	—	Favourable	40.22	2022-10-10
SU304092	—	Favourable	21.32	2019-06-27
SU304102	—	Unfavourable Recovering	160.11	2015-01-30
SU304111	—	Unfavourable Recovering	32.49	2016-02-12
SU304161	—	Unfavourable Recovering	4.35	2008-06-03
SU305060	—	Favourable	20.65	2017-02-10
SU305065	—	Unfavourable Recovering	63.57	2016-02-11
SU305090	—	Unfavourable Recovering	4.57	2022-10-10
SU305104	—	Favourable	14.24	2013-12-05
SU305126	—	Favourable	542.25	2017-07-13
SU306048	—	Favourable	124.27	2011-09-28
SU306112	—	Favourable	236.79	2017-05-23
SU307085	—	Unfavourable Recovering	40.73	2009-11-26
SU307086	—	Favourable	236.79	2017-05-23
SU307098	—	Favourable	236.79	2017-05-23
SU307106	—	Favourable	542.25	2017-07-13
SU307150	—	Unfavourable Recovering	14.08	2012-02-14
SU307151	—	Unfavourable Recovering	1.3	2012-02-14
SU308034	—	Favourable	84.74	2016-08-25
SU309076	—	Unfavourable Recovering	76.99	2017-03-14
SU309154	—	Unfavourable Recovering	15.5	2024-02-07
SU310071	—	Unfavourable Recovering	76.99	2017-03-14
SU310105	—	Favourable	236.79	2017-05-23
SU310111	—	Unfavourable Recovering	32.49	2016-02-12
SU311091	—	Unfavourable Recovering	16.16	2023-03-07
SU311093	—	Unfavourable Recovering	16.16	2023-03-07
SU312026	—	Unfavourable Recovering	5.24	2010-11-08
SU312028	—	Unfavourable Recovering	37.58	2009-12-18
SU312090	—	Unfavourable Recovering	197.78	2016-02-11
SU313026	—	Unfavourable Recovering	0.63	2010-11-08
SU313152	—	Unfavourable No Change	0.72	2016-07-11
SU314066	—	Unfavourable Recovering	36.21	2016-02-11
SU314074	—	Favourable	5.99	2011-09-28
SU314075	—	Unfavourable Recovering	76.99	2017-03-14
SU315110	—	Favourable	236.79	2017-05-23
SU316072	—	Unfavourable Recovering	6.14	2013-03-05
SU316090	—	Favourable	5.99	2011-09-28
SU317050	—	Unfavourable Recovering	396.16	2012-11-21
SU317073	—	Favourable	5.99	2011-09-28
SU317076	—	Favourable	542.25	2017-07-13
SU317089	—	Favourable	57.65	2017-05-29
SU318028	—	Unfavourable Recovering	23.16	2011-09-28
SU318073	—	Favourable	5.99	2011-09-28
SU318100	—	Unfavourable Recovering	6.32	2013-10-12
SU318107	—	Unfavourable Recovering	197.78	2016-02-11
SU318154	—	Unfavourable Declining	26.61	2017-02-09
SU318157	—	Unfavourable Declining	0.5	2009-02-26
SU319034	—	Unfavourable Recovering	128.94	2011-09-28
SU319069	—	Unfavourable No Change	15.85	2015-01-30
SU319084	—	Favourable	87.52	2017-02-13
SU319104	—	Unfavourable No Change	16.8	2021-10-01
SU321063	—	Unfavourable Recovering	50.66	2016-02-11
SU321089	—	Favourable	542.25	2017-07-13
SU321092	—	Favourable	57.65	2017-05-29
SU321100	—	Unfavourable Recovering	197.78	2016-02-11
SU321112	—	Unfavourable Recovering	32.49	2016-02-12
SU322015	—	Favourable	31.76	2011-09-28
SU322031	—	Unfavourable Recovering	10.98	2020-07-02
SU322095	—	Unfavourable Recovering	40.73	2009-11-26
SU324034	—	Unfavourable Recovering	6.3	2017-02-13
SU324043	—	Favourable	7.4	2017-09-19
SU325080	—	Favourable	18.92	2012-07-06
SU325082	—	Favourable	542.25	2017-07-13
SU326021	—	Unfavourable Recovering	62.39	2016-02-11
SU326027	—	Unfavourable Recovering	130.17	2013-12-06
SU326070	—	Unfavourable Recovering	37.63	2015-01-30
SU326072	—	Unfavourable Recovering	21.78	2023-03-07
SU326089	—	Favourable	542.25	2017-07-13
SU326092	—	Favourable	38.32	2021-08-04
SU327069	—	Unfavourable Recovering	37.63	2015-01-30
SU327087	—	Favourable	87.52	2017-02-13
SU327096	—	Favourable	57.65	2017-05-29
SU328064	—	Unfavourable Recovering	75.76	2020-10-23
SU329018	—	Unfavourable Recovering	11.98	2012-08-31
SU329019	—	Favourable	1104.18	2017-05-18
SU329021	—	Favourable	1104.18	2017-05-18
SU329043	—	Unfavourable Recovering	119.86	2012-11-21
SU329104	—	Unfavourable Recovering	20.31	2013-12-05
SU331054	—	Favourable	3.49	2016-05-18
SU331055	—	Favourable	1.67	2011-10-10
SU331075	—	Unfavourable Recovering	3.26	2017-05-13
SU332034	—	Favourable	16.81	2017-02-10
SU332074	—	Favourable	542.25	2017-07-13
SU332093	—	Favourable	40.33	2011-09-28
SU332098	—	Unfavourable No Change	11.13	2017-07-13
SU333053	—	Unfavourable Recovering	1.85	2016-05-18
SU333058	—	Favourable	96.38	2016-02-11
SU333077	—	Favourable	27.43	2021-06-10
SU333083	—	Favourable	18.97	2012-07-06
SU333087	—	Favourable	542.25	2017-07-13
SU334020	—	Unfavourable Recovering	41.03	2017-05-12
SU334066	—	Unfavourable No Change	10.59	2017-05-12
SU334101	—	Favourable	3.97	2020-07-30
SU335000	—	Favourable	6.28	2017-02-10
SU335025	—	Favourable	1104.18	2017-05-18
SU335075	—	Unfavourable Recovering	160.11	2015-01-30
SU336039	—	Unfavourable Recovering	128.94	2011-09-28
SU336071	—	Unfavourable Recovering	160.11	2015-01-30
SU337102	—	Favourable	312.15	2012-10-31
SU338027	—	Unfavourable No Change	2.69	2009-03-26
SU338029	—	Favourable	14.15	2016-02-11
SU339080	—	Favourable	542.25	2017-07-13
SU339086	—	Unfavourable Recovering	3.0	2010-09-16
SU339090	—	Unfavourable Recovering	45.89	2013-12-06
SU340045	—	Unfavourable Recovering	124.96	2016-02-11
SU340085	—	Favourable	542.25	2017-07-13
SU340088	—	Unfavourable Recovering	37.58	2009-12-18
SU340098	—	Unfavourable Recovering	72.93	2016-02-11
SU341064	—	Unfavourable Recovering	160.11	2015-01-30
SU342022	—	Unfavourable Recovering	63.92	2016-02-11
SU342036	—	Unfavourable Recovering	37.58	2009-12-18
SU342063	—	Favourable	542.25	2017-07-13
SU342077	—	Unfavourable Recovering	160.11	2015-01-30
SU342082	—	Unfavourable Recovering	160.11	2015-01-30
SU343052	—	Unfavourable Recovering	68.25	2013-12-05
SU343072	—	Unfavourable Recovering	160.11	2015-01-30
SU343080	—	Unfavourable Recovering	160.11	2015-01-30
SU344057	—	Favourable	542.25	2017-07-13
SU344092	—	Unfavourable Recovering	88.15	2016-02-11
SU345083	—	Favourable	1257.06	2017-08-29
SU346034	—	Unfavourable Recovering	169.8	2016-02-11
SU346066	—	Favourable	542.25	2017-07-13
SU347048	—	Favourable	542.25	2017-07-13
SU347070	—	Unfavourable Recovering	37.58	2009-12-18
SU348075	—	Favourable	5.99	2011-09-28
SU349092	—	Unfavourable Recovering	45.89	2013-12-06
SU350030	—	Favourable	60.99	2017-09-19
SU350077	—	Favourable	1257.06	2017-08-29
SU351092	—	Favourable	1257.06	2017-08-29
SU351096	—	Favourable	1.9	2020-10-23
SU352003	—	Favourable	1104.18	2017-05-18
SU352047	—	Favourable	1257.06	2017-08-29
SU352054	—	Favourable	1257.06	2017-08-29
SU352070	—	Favourable	312.15	2012-10-31
SU352073	—	Unfavourable Recovering	56.99	2015-02-09
SU353061	—	Favourable	1257.06	2017-08-29
SU354077	—	Unfavourable Recovering	56.99	2015-02-09
SU354085	—	Unfavourable Recovering	134.84	2011-09-29
SU355024	—	Unfavourable Recovering	155.05	2016-02-11
SU355045	—	Unfavourable Recovering	18.81	2013-12-06
SU355051	—	Favourable	50.27	2015-01-30
SU356074	—	Unfavourable Recovering	5.82	2010-07-23
SU356092	—	Unfavourable Recovering	7.43	2013-12-05
SU357075	—	Unfavourable Recovering	5.82	2010-07-23
SU358019	—	Unfavourable Recovering	11.83	2013-12-06
SU358069	—	Favourable	312.15	2012-10-31
SU359043	—	Favourable	1257.06	2017-08-29
SU361042	—	Favourable	312.15	2012-10-31
SU361066	—	Favourable	312.15	2012-10-31
SU361077	—	Favourable	312.15	2012-10-31
SU362041	—	Favourable	312.15	2012-10-31
SU362042	—	Unfavourable Recovering	88.15	2016-02-11
SU362073	—	Favourable	5.99	2011-09-28
SU363034	—	Favourable	242.87	2011-09-28
SU363048	—	Favourable	242.87	2011-09-28
SU363084	—	Favourable	1257.06	2017-08-29
SU364013	—	Unfavourable Declining	32.02	2013-11-19
SU364023	—	Unfavourable Recovering	26.4	2013-12-06
SU364037	—	Favourable	312.15	2012-10-31
SU365011	—	Unfavourable Declining	32.02	2013-11-19
SU365076	—	Favourable	8.74	2017-02-16
SU366026	—	Favourable	312.15	2012-10-31
SU366054	—	Favourable	242.87	2011-09-28
SU367065	—	Favourable	1257.06	2017-08-29
SU367069	—	Favourable	312.15	2012-10-31
SU368001	—	Unfavourable Recovering	7.23	2013-12-06
SU368045	—	Favourable	1257.06	2017-08-29
SU369052	—	Unfavourable Recovering	85.01	2012-11-01
SU370072	—	Favourable	1257.06	2017-08-29
SU370077	—	Unfavourable Recovering	49.59	2013-12-06
SU371045	—	Favourable	312.15	2012-10-31
SU374017	—	Unfavourable Recovering	0.13	2011-03-29
SU374057	—	Favourable	1257.06	2017-08-29
SU375060	—	Favourable	44.33	2019-09-12
SU375065	—	Favourable	1257.06	2017-08-29
SU375079	—	Favourable	312.15	2012-10-31
SU376050	—	Favourable	1257.06	2017-08-29
SU380064	—	Favourable	47.78	2011-09-28
SU381059	—	Favourable	5.99	2011-09-28
SU382055	—	Favourable	47.78	2011-09-28
SU383055	—	Favourable	47.78	2011-09-28
SU383073	—	Favourable	10.08	2019-03-26
SU386071	—	Favourable	1257.06	2017-08-29
SU389049	—	Unfavourable Recovering	22.1	2011-09-28
SU390053	—	Favourable	312.15	2012-10-31
SU390056	—	Unfavourable Recovering	25.07	2023-03-07
SU390067	—	Unfavourable Recovering	90.14	2012-10-31
SU390074	—	Unfavourable Recovering	29.49	2013-12-06
SU393051	—	Unfavourable Recovering	14.42	2011-09-28
SU394075	—	Favourable	1257.06	2017-08-29
SU395048	—	Favourable	312.15	2012-10-31
SU395061	—	Unfavourable Recovering	25.76	2012-10-31
SU395068	—	Favourable	1257.06	2017-08-29
SU396062	—	Favourable	1257.06	2017-08-29
SU396065	—	Favourable	1257.06	2017-08-29
SU396073	—	Favourable	312.15	2012-10-31
SU396074	—	Unfavourable Recovering	29.49	2013-12-06
SU397051	—	Favourable	23.23	2012-11-01
SU397052	—	Unfavourable Recovering	16.0	2013-12-05
SU398074	—	Unfavourable Declining	1.42	2022-10-17
SU399058	—	Favourable	23.23	2012-11-01
SU399074	—	Unfavourable Recovering	1.14	2023-03-31
SU401067	—	Favourable	312.15	2012-10-31
SU404044	—	Favourable	1257.06	2017-08-29
SU405057	—	Unfavourable Recovering	92.77	2013-12-06
SU409024	—	Unfavourable Recovering	4.86	2013-12-06
SU409029	—	Unfavourable Recovering	41.3	2013-12-06
SU410049	—	Favourable	1.23	2012-10-31
SU412043	—	Favourable	312.15	2012-10-31
SU412053	—	Unfavourable Recovering	55.67	2013-12-06
SU415043	—	Favourable	1257.06	2017-08-29
SU415050	—	Unfavourable Recovering	51.1	2013-12-06
SU416046	—	Favourable	1257.06	2017-08-29
SU417027	—	Unfavourable Recovering	18.75	2013-12-06
SU418055	—	Unfavourable Declining	0.96	2023-03-31
SU419054	—	Unfavourable Recovering	2.21	2023-03-31
SU419056	—	Unfavourable Recovering	3.9	2023-03-31
SU420054	—	Unfavourable No Change	0.77	2023-03-31
SU421032	—	Favourable	312.15	2012-10-31
SU421033	—	Unfavourable Declining	2.2	2011-11-11
SU421034	—	Favourable	2.3	2012-12-10
SU421043	—	Unfavourable No Change	7.04	2011-11-14
SU422027	—	Unfavourable Recovering	16.42	2013-12-05
SU422049	—	Unfavourable Recovering	55.67	2013-12-06
SU423043	—	Unfavourable Declining	1.47	2009-03-23
SU424042	—	Unfavourable Declining	0.5	2009-03-23
SU425028	—	Favourable	1257.06	2017-08-29
SU425041	—	Favourable	2.83	2009-06-14
SU426019	—	Unfavourable Recovering	68.1	2011-09-28
SU426037	—	Unfavourable Recovering	3.55	2011-11-14
SU431026	—	Unfavourable Recovering	1.14	2011-03-30
SU431052	—	Unfavourable No Change	2.13	2019-04-26
SU432014	—	Favourable	0.9	2020-12-08
SU433050	—	Favourable	8.16	2019-04-26
SU433052	—	Unfavourable Declining	3.11	2019-04-26
SU434010	—	Favourable	1257.06	2017-08-29
SU434012	—	Favourable	12.85	2016-02-11
SU434017	—	Favourable	312.15	2012-10-31
SU434052	—	Favourable	8.16	2019-04-26
SU435013	—	Favourable	312.15	2012-10-31
SU435017	—	Favourable	1257.06	2017-08-29
SU439012	—	Favourable	312.15	2012-10-31
SU439017	—	Favourable	312.15	2012-10-31
SZ170999	—	Favourable	6.48	2011-11-22
SZ173996	—	Favourable	0.7	2011-11-22
SZ175995	—	Unfavourable No Change	0.74	2011-11-14
SZ176991	—	Unfavourable Recovering	1.86	2014-01-31
SZ176999	—	Unfavourable No Change	6.26	2011-11-14
SZ188993	—	Favourable	5.68	2022-10-25
SZ188995	—	Favourable	7.11	2022-10-25
SZ188998	—	Favourable	6.92	2008-07-10
SZ191987	—	Unfavourable No Change	16.67	2012-12-19
SZ191990	—	Unfavourable No Change	16.67	2012-12-19
SZ191992	—	Favourable	6.22	2022-10-25
SZ191996	—	Favourable	15.45	2022-10-25
SZ192990	—	Unfavourable No Change	3.92	2012-12-19
SZ192999	—	Favourable	3.0	2008-07-10
SZ194991	—	Unfavourable No Change	3.92	2012-12-19
SZ194993	—	Unfavourable Recovering	7.76	2022-10-25
SZ194996	—	Unfavourable Recovering	11.69	2022-10-25
SZ196998	—	Unfavourable Recovering	3.44	2022-10-25
SZ205949	—	Unfavourable No Change	1.34	2012-03-02
SZ205989	—	Favourable	2.27	2008-08-22
SZ207989	—	Unfavourable Declining	3.26	2016-07-07
SZ211996	—	Favourable	192.05	2017-05-30
SZ214994	—	Favourable	192.05	2017-05-30
SZ214998	—	Favourable	192.05	2017-05-30
SZ215997	—	Favourable	192.05	2017-05-30
SZ216992	—	Unfavourable No Change	19.15	2017-07-13
SZ219985	—	Favourable	1104.58	2017-08-07
SZ223985	—	Unfavourable Recovering	18.07	2015-02-04
SZ224995	—	Favourable	11.76	2017-02-14
SZ226988	—	Unfavourable Recovering	38.15	2015-02-04
SZ237996	—	Unfavourable Recovering	138.72	2011-09-28
SZ238992	—	Unfavourable Declining	1.99	2009-03-26
SZ242986	—	Favourable	75.68	2017-09-21
SZ242998	—	Unfavourable Recovering	19.22	2011-09-28
SZ250973	—	Destroyed	2.46	2009-02-26
SZ252996	—	Unfavourable Recovering	23.6	2013-12-06
SZ253991	—	Unfavourable Recovering	71.94	2016-02-11
SZ255987	—	Favourable	7.98	2017-02-14
SZ256996	—	Favourable	33.29	2017-02-13
SZ257986	—	Favourable	1104.58	2017-08-07
SZ262984	—	Favourable	1104.58	2017-08-07
SZ263987	—	Unfavourable Recovering	13.72	2015-02-04
SZ265983	—	Unfavourable No Change	1.68	2012-02-27
SZ265994	—	Unfavourable Recovering	97.26	2012-11-21
SZ267983	—	Favourable	1.43	2009-02-26
SZ279992	—	Unfavourable No Change	4.98	2017-04-05
SZ284997	—	Favourable	6.31	2015-02-04
SZ287994	—	Unfavourable Recovering	37.58	2009-12-18
SZ289985	—	Favourable	98.37	2012-08-31
SZ290997	—	Favourable	1104.58	2017-08-07
SZ292992	—	Unfavourable Recovering	35.47	2015-02-04
SZ293985	—	Favourable	2.54	2011-09-28
SZ293987	—	Favourable	1104.58	2017-08-07
SZ294954	—	Unfavourable Recovering	2.03	2011-11-14
SZ295996	—	Unfavourable Recovering	37.58	2009-12-18
SZ296986	—	Unfavourable Recovering	4.02	2013-12-06
SZ297953	—	Unfavourable Recovering	13.13	2012-11-08
SZ298954	—	Unfavourable Recovering	5.32	2010-07-29
SZ299952	—	Unfavourable Recovering	13.13	2012-11-08
SZ299992	—	Favourable	13.37	2013-12-06
SZ299998	—	Favourable	1104.58	2017-08-07
SZ300951	—	Unfavourable Recovering	13.13	2012-11-08
SZ300952	—	Unfavourable Recovering	13.13	2012-11-08
SZ300953	—	Unfavourable Recovering	13.13	2012-11-08
SZ303952	—	Unfavourable Recovering	13.13	2012-11-08
SZ303999	—	Unfavourable Recovering	20.24	2009-11-26
SZ304950	—	Unfavourable Recovering	10.12	2012-11-08
SZ304953	—	Unfavourable Recovering	10.12	2012-11-08
SZ306952	—	Unfavourable Recovering	10.12	2012-11-08
SZ310992	—	Unfavourable Recovering	2.12	2012-01-24
SZ310994	—	Unfavourable Recovering	2.91	2009-02-26
SZ312993	—	Unfavourable Recovering	0.37	2010-12-07
SZ313993	—	Unfavourable Recovering	1.59	2009-02-26
SZ334988	—	Favourable	1104.18	2017-05-18
SZ336992	—	Favourable	10.73	2017-02-10
SZ342985	—	Favourable	4.87	2012-09-21
SZ346994	—	Unfavourable Recovering	38.14	2013-12-06
SZ348978	—	Unfavourable Recovering	13.5	2013-12-06
SZ352983	—	Unfavourable Recovering	66.42	2016-08-02
SZ353978	—	Favourable	1104.18	2017-05-18
SZ354991	—	Favourable	33.86	2013-12-06
SZ358984	—	Favourable	22.36	2017-05-04
SZ358997	—	Favourable	24.3	2016-08-23
SZ364978	—	Favourable	22.36	2017-05-04
SZ364987	—	Favourable	9.93	2012-09-21
SZ365984	—	Favourable	22.36	2017-05-04
SZ366982	—	Favourable	1104.18	2017-05-18
SZ367969	—	Favourable	3.02	2012-12-18
SZ395999	—	Unfavourable Declining	2.53	2012-12-17
SZ396976	—	Unfavourable Declining	33.6	2020-12-15

Climate exposure

This is about exposure to a nationwide pressure this habitat type carries — not a verdict on this site's own management.

Habitats

Blanket bog, Bracken scrub, Carr, Fast flowing river and stream, Lowland dry heath, Lowland fen, Lowland heath, Lowland meadow and pasture, Lowland wet heath, Mixed scrub, Montane scrub, Purple moor grass and rush pasture, Upland acid grassland, Upland mixed ash wood, Upland spring flush, Upland wet heath, Valley mire

Geology & landscape

Geological Period: Paleogene, Quaternary · Rock Type: Chalk, Flint

Landscape processes: Fluvial, Glacial, Peatland / Mire

Birds & fish recorded

Birds

Species	Season
curlew	Breeding
curlew	Wintering
dartford warbler	Breeding
dartford warbler	Wintering
hen harrier	Breeding
hen harrier	Wintering
lapwing	Breeding
lapwing	Wintering
nightjar	Breeding
redshank	Breeding
redshank	Wintering
redstart	Breeding
redstart	Roosting
ringed plover	Breeding
ringed plover	Wintering
snipe	Breeding
snipe	Wintering

Description

Area,28,947.37 hectares 71,528.95 ac Description The New Forest embraces the largest area of 'unsown' vegetation in lowland England and includes the representation on a large scale of habitat formations formerly common but now fragmented and rare in lowland western Europe. They include lowland heath, valley and seepage step mire, or fen and ancient pasture woodland, including riparian and bog woodland. Nowhere else do these habitats occur in combination and on so large a scale. There are about 4,600 hectares of pasture woodland and scrub dominated by oak, beech and holly; 11,800 hectares of heathland and associated grassland; 3,300 hectares of wet heath and valley mire fen and also 8,400 hectares of plantations dating from various periods since the early 18th century. Within this matrix of habitats are a range of acid to neutral grasslands where the vegetation owes much to the local geology and continuous grazing, a situation which is uncommon in lowland England. Scattered around the New Forest and throughout the small pockets of enclosed farmland are a series of unimproved meadows which have similarities with these open forest grasslands. A network of small streams draining the system form an unusual community which results from the combination of nutrient poor, acid waters and outcrops of neutral enriched soils. There are many ponds of varying sizes and water chemistry including several ephemeral ponds. This wide range of habitats support an assemblage of nationally rare and scarce plants and a nationally important assemblage of rare and scarce invertebrates. The area supports internationally important breeding populations of certain bird species and the wintering population of another as well as an assemblage of birds associated with specific habitats such as old woodland or wetlands. Within the New Forest there are seven sites which are of special geological or physiographic interest including valley mires, the headwaters of the Highland Water, stream sections with exposures of fossil bearing strata and a gravel pit rich in palaeolithic artefacts. The New Forest is probably sufficiently large to ensure the long term survival of the characteristic flora and fauna within the wide range of habitats. Smaller isolated examples of the component habitats are vulnerable to biological impoverishment but here in the New Forest has survived largely because of the persistence of a pastoral economy based on the exercise of common rights of grazing and mast together with protection afforded by Crown ownership. This and the management of vegetation in the open forest through burning and cutting programmes, administered by the Forestry Commission on the Crown Lands, maintains the quality of the grazings, ensures the prevention of natural succession and encourages local diversity in plant communities. The pastoral economy in turn depends on the continued existence of a small community of commoners who make up a discrete social unit and this combination of natural and cultural elements contributes to the maintenance of the New Forest habitats. Geomorphologically the Forest comprises a series of eroded terraces capped with flint gravel, brick earth and other superficial deposits. The terraces are highest and most fragmented by erosion in the north and lowest and most complete in the south. Erosion has exposed the underlying Tertiary strata, in wide valleys and hollows separating the terraces. Soils are mainly acid, poor in nutrients, susceptible to leaching and only slowly permeable. Locally, however, there are enriched areas such as the exposed Headon Beds in the south which support relatively species rich grassland or mire floras. The forest's streams, mires and abundant wet flushes along slope spring lines help to create a humid microclimate which, in the woodlands in particular, provides the right conditions for epiphytic lichens, bryophytes and ferns, a situation which has become rare elsewhere. The unenclosed woodlands are dominated by oak and beech in varying proportions. Oak is generally dominant on the heavier soils and some areas comprise nearly monospecific oak woods, whereas the beech tends to dominate on sandy knolls and well drained terrace edges. Holly is the dominant shrub layer species. The number of tree species is higher in linear riverine woodland where ash is abundant and carr of alder, sallow and holly are common. Age structure of the woodland is closely related to past fluctuations in herbivore densities. The oldest generation of trees still standing are oaks and beeches of early 17th century origin. A high proportion of these and later 17th century trees are pollarded. The main younger generations have arisen since about the mid 19th century. Older trees support the richest known woodland lichen flora in lowland Europe and an exceptionally species rich dead wood fauna, mainly beetles Coleoptera, including the stag beetle Lucanus cervus and now rare in Europe and flies Diptera. The lichen flora includes two rare species, Megalaria laureri and Parmelia minarum Sch. 8**. The woods are also rich in fungi that are specific to pasture woodland such as Hericium erinaceus, Mycena picta, Hericium cirrhatum and Flammulaster limulatus. The woodland ground flora varies according to soil type but grazing often gives the impression of it being impoverished. On base rich soils, however, species diversity increases with grazing whereas on more acid soils the vascular plants may be reduced but bryophytes become more extensive and diverse. Woodland species such as Dicranum majus, Rhitidia delphus loreus and Leucobryum juniperoideum can be common whilst rarer species include Bassania trilobuta and Saccogyna viticulosa. The vascular plants include about 60 species associated with old woodland. These older trees also support a high density of hole nesting, insectivorous birds, such as redstart Phoenicurus phoenicurus and provide roost sites for several species of bat including the very rare Bechstein's bat Myotis bechsteinii**. The sylvicultural enclosures include 40 percent broad leaved trees, mainly oak and beech, which, with the unenclosed woods, comprises the largest tract of native broad leaved woodland in southern England. The inclosures include many fragments of former pasture woods totalling about 285 hectares and these are relatively unmodified by enclosure. Much of the remaining broad leaved component comprises mature oak plantation which when in proximity to unenclosed woodland can take on the characteristics of pasture woodland. In South Bentley Inclosure the epiphytic flora has developed with similar species to the adjacent unenclosed Anses Wood. Some of the inclosures have only low grazing pressure and the ground flora then provides food plants for certain invertebrates, such as silver washed fritillary Argynnis paphia and white admiral Limenitis camilla. The heathlands, including grass heaths and acid grasslands comprise a series of plant communities, the composition of which is related to soil structure and permeability and the effects of grazing. Dry heath dominated by heather Calluna vulgaris and bell heather Erica cinerea and bristle bent Agrostis curtisii grades into humid heath in which cross leaved heath Erica tetralix and purple moor grass Molinia caerulea are constant species. The humid heath on slowly permeable and often seasonally waterlogged soils is spatially dominant here although only recognised as a transitional community elsewhere. On the wetter humic soils heather becomes less frequent and typically deer grass Trichophorum cespitosum, heath rush Juncus squarrosus and the 'smaller' Sphagnum species Sphagnum compactum and S. tenellum become frequent. The heathlands have well developed lichen rich communities in which a number of Cladonia species are present. These include the nationally scarce C. incrassata and an abundance of species such as C. strepsilis and Pycnothelia papillaria. Other lowland plants occur such as the rare dung fungus Poronia punctata which grows on pony dung. Within the heathland mosaic, on pockets of richer soils, acid grassland occurs. These areas can change from grass to heath depending on the grazing intensity. They are dominated by bristle bent and purple moor grass with varying amounts of heather, gorse Ulex europaeus and bracken Pteridium aquilinum. The acid to neutral grasslands are strongly influenced by the underlying geology and by grazing. The naturally infertile soils support herb rich vegetation communities on the drier brown earths and stagnogleys and a complex range of wet acid grasslands on gleys and peats. The acid grasslands are often quite extensive, relatively species rich and comprise two main elements: a. species which benefit from heavy grazing and are mostly prostrate or are able to survive in dwarf form; and b. species which are less palatable. The former includes rosette forming species such as hawkbits Leontodon, cat's ear Hypochaeris radicata, mouse ear hawkweed Pilosella officinarum and yarrow Achillea millefolium and a profusion of small herbs with low growth forms such as tormentil Potentilla erecta, heath bedstraw Galium saxatile, lousewort Pedicularis sylvatica, self heal Prunella vulgaris, eyebrights Euphrasia, squirrel tail fescue Vulpia bromoides, all seed Radiola linoides and numerous sedges. The less palatable species with a more upright growth form include yellow centaury Cicendia filiformis which is nationally scarce, common centaury Centaurium erythraea, field gentian Gentianella campestris and moonwort Botrychium lunaria. The more neutral grasslands known locally as 'lawns' occur as linear features following many of the small streams, roadside verges around settlements village greens and as glades in association with pasture woodland. They are influenced by such factors as soils, topography, the nutrient quality of flood water and frequency of numbers of grazing animals. Typical species on the wetter lawns are velvet bent Agrostis canina and an abundance of wetland sedges, rushes and herbs. The drier communities around settlements are dominated by common bent grass Agrostis capillaris with some perennial rye grass Lolium perenne, crested dog's tail Cynosurus cristatus, daisy Bellis perennis and most distinctively mats of abundant chamomile Chamaemelum nobile, which is nationally rare and declining. Associated with these settlement edge lawns that are seasonally poached and heavily grazed are an assemblage of nationally rare and scarce plants. They include small fleabane Pulicaria vulgaris and penny royal Mentha pulegium both RDB* Sch 8**. Slender marsh bedstraw Galium constrictum RDB* and coral necklace Illecebrum verticillatum, which is nationally scarce, also occur. Hampshire purslane Ludwigia palustris RDB* occurs in the poached muddy pools and is confined in England to the New Forest area. The unimproved meadows in and around the Forest have similarities with the acid to neutral grasslands within the Open Forest. The frequent spring lines and infertility of the soils have hindered agricultural improvement and these meadow communities are now rare or scarce in England. The main vegetation types are herb rich, permanent pastures on the drier brown earths and stagno gleys and a complex range of wet acid grasslands on gleys and peats. The former could be described as the typical grassland of grazed hay meadows usually dominated by common bent Agrostis capillaris and red fescue Festuca rubra but containing a high proportion of herbs. The character of the wet grassland is more complex. Moderately grazed, rush dominated stands are mostly dominated by sharp-flowered rush Juncus acutiflorus and accompanied by soft rush Juncus effusus but the other associates can be quite diverse. Lightly grazed grassland dominated by Molinia caerulea is especially variable with both heathy, fen meadow and mire communities present. Pony grazed grasslands lack any tall dominants and consist of a species rich mixture of velvet bent Agrostis canina and sedges, much like the wetter Open Forest lawns. Within these vegetation types there are pockets containing diverse herb rich communities. Very dry soils, for instance, support parched acid grassland which is typically hard grazed and disturbed and provides suitable habitat for spring annuals such a subterranean clover Trifolium subterraneum. In contrast the wettest parts of spring lines often support mire communities typical of the Open Forest with Sphagnum species dominant and scarce plants present such as brown beak sedge Rhynchospora fusca. Much rarer are the base rich mire communities which occur in close juxtaposition with acid communities such as the small, marshy flushes at Upper Pennington Common. The Forest contains about 90 clearly separable valley mires, or fen, within about 20 different valley systems. This is thought to be more than survive in the remainder of Britain and Western Europe. This suite of mires sits within a relatively unpolluted catchment and for this reason the greater part of the New Forest has been designated as an internationally important wetland, a Ramsar site. The mires receive the products of leaching from the higher ground and are thus comparatively base enriched. Structurally they comprise a distinctive sequence of plant communities arranged laterally to the axis and exhibiting increased enrichment from the outer margin to the centre. Similarly, the mires tend to become progressively base enriched with progress downstream from the valley head and this also influences the complex arrangement of plant communities. The zonation from enriched fen along the axes of many mires, to acid mire at the outer margins, gives rise to a great diversity of plant species. The richest mires have in excess of 150 species including many locally distributed and rare plants. Slender cotton grass Eriophorum gracile RDB* Sch.8*** is confined in England to sites in the New Forest and one in Surrey. The list of nationally scarce plants found on mires and their heathy margins include pillwort Pilularia globulifera, bog orchid Hammarbya paludosa, bog hair grass Deschampsia setacea, marsh gentian Gentiana pneumonan the, marsh clubmoss Lycopodiella inundata, brown beak sedge and marsh fern Thelypteris palustris*. Of the many ponds within the Forest the less acidic ponds support important populations of amphibians, including the rare great crested newt Triturus cristatus Sch.5**. The wetland habitats collectively form probably the most important single suite of habitats for dragonflies Odonata in Britain. Twenty seven species breed in the New Forest including the rare southern damselfly Coenagrion mercuriale RDB*. The temporary ponds that dry out in the summer provide ideal conditions for some specially adapted invertebrates including fairy shrimps Chirocephalus diaphanus and one such pond is the only known British locality for the tadpole shrimp Triops cancriformis both RDB* Sch.5**. The plant community associated with the streams is restricted almost exclusively to the New Forest. The only other stream of this type is the River Fowey on Bodmin Moor. This is because of the combination of nutrient poor acid waters and outcrops of neutral enriched soils. The Lymington River is the largest stream system within the Forest showing all the typical characteristics. The tributary known as the Ober Water is recognised in the Nature Conservation Review as a lowland base poor stream with a very diverse flora. Surveys of the Forest streams have recorded twenty of the fifty four British species of fish and a wide variety of invertebrates. Some streams are used by otters, a species which has declined and which is fully protected through Schedule 5**. The Forest supports populations of nine rare and twenty five nationally scarce vascular plants*. Of the rare plants five have been mentioned above. Dorset heath Erica ciliaris occurs at two locations and the wild gladiolus Gladiolus illyricus Sch.8**, which is confined to the New Forest in Britain, is present in many of the bracken stands where it is normally associated with bluebells and wood anemones. Heath lobelia Lobelia urens is only found at one locality, as is the early gentian Gentianella anglica which occurs in association with imported chalk! The New Forest supports nationally important breeding populations of birds as listed in Annex 1 of the EU Directive on the Conservation of Wild Birds including, nightjar Caprimulgus europaeus, woodlark Lullula arborea, Dartford warbler Sylvia undata and kingfisher Alcedo atthis. The Forest also supports a wintering population of hen harrier Circus cyaneus which is also listed on Annex 1. Other breeding birds include an assemblage of waders comprising lapwing Vanellus vanellus, redshank Tringa totanus, curlew Numenius arquata, snipe Gallinago gallinago and ringed plover Charadrius hiaticulata which all depend to a great extent on the Forest's wetland habitats. Populations of all Britain's native reptiles are present in the New Forest including sand lizard Lacerta agilis Sch.5* and smooth snake Coronella austriaca Sch.5, which both occur in suitable localities throughout the heathland. The wide range of habitats within the New Forest and its large size, make it an important site for populations of several groups of invertebrates. Of the 2,500 species of British butterflies and moths Lepidoptera, nearly half have been recorded from the Forest and over a third of the British species of beetle have been recorded as well as many species from other invertebrate groups. Many of these species are recorded in the Red Data Book and even more are considered notable. For some of these species, such as the New Forest Cicada Cicadetta montana, the New Forest is the only or main centre of distribution in Britain. The seven sites of special geological or physiographic interest are as follows, Studley Wood stream section is a prolific Tertiary locality exposing the only complete exposure of the silty Huntingbridge Formation of the Bracklesham Group. This is also the stratotype for the Studley Wood Member of the Formation. This series of units forming the top of the Bracklesham beds is remarkable for its molluscan faunas and the number of species limited to the Formation. Numerous corals, scaphopoda, bivalves and gastropods occur here. This is an outstanding Eocene locality of great interest in studies of Tertiary stratigraphy and palaeontology within the Hampshire Basin and across north western Europe. Shepherd's Gutter stream section has been known to geologists since at least the middle of the 19th century and this locality is renowned for its rich Tertiary marine faunas. It shows a section through the Selsey Formation of the Bracklesham Group, of Middle Eocene age and includes several mollusc rich horizons and one kind of Nummulites correlatable with the Isle of Wight and Bracklesham sections. This is a key locality for its correlations between the classic Eocene localities of the Hampshire Basin and for its prolific molluscan faunas. Parkhill Enclosure ditch section is the only exposure in England outside the Isle of Wight to show upper middle Headon Bends. The occurrence of a fauna of Cerithidea ventricosa and other mollusca in the Headon clays here allows correlation with the type sections of the Isle of Wight. The fauna of well preserved shells and fish remains makes this one of the richest Tertiary faunal localities on the mainland. It is an important site for its palaeontology and for correlations within the Hampshire Tertiary Basin. Woodgreen gravel pit exposes Pleistocene gravel, deposited by the River Avon, rich in Palaeolithic artefacts. Palaeolithic assemblages provide major evidence for the subdivision of the terrace sequence in The Solent Basin, where they are particularly important owing to a dearth of palaeontological sites. The Woodgreen pit has yielded over 400 artefacts, making it one of the most prolific in The Solent catchment. This is an important site which has significant potential to further elucidate the complex history of the River Avon gravels and the evolution of The Solent river. Mark Ash Wood is a valley mire complex of considerable importance for palynological and palaeoecological studies. Peat growth at the site dates from the early part of the Devensian late glacial to the sub Atlantic period. Mark ash Wood contains the oldest post glacial peats in the New Forest area and is exceptional for high accumulation rates during late glacial times. Macrofossil and pollen analyses have yielded some of the earliest British post glacial records of bryophytes. Mark Ash Wood is also of importance in tracing the early post glacial immigration and expansion of plant species and has been used as a reference site for correlation in southern England. Cranes Moor is a large mire complex, set in a shallow basin containing significant peat accumulations dating back to Devensian late glacial times. It is a key reference site for palynological studies in southern England. It is also unusual for the apparently rapid accumulation of peat in the Boreal period and is therefore particularly important in the study of the early immigration and expansion of flora in post glacial times. Several studies of vegetational history have been carried out in the post war period at a number of sub sites within the basin including, most recently, an integrated investigation of macrofossils, pollen and other microfossils, together with radio-carbon correlation of cores. Highland Water is a unique area demonstrating a combination of low management and low human impact on fluvial processes. It is particularly important on two accounts. First, it provides a valuable opportunity to study the role and influence of vegetation in hydrological and fluvial processes. Second, it is of exceptional value for the study of debris dams which have a significant effect on channel processes, travel times of flood hydrographs, channel roughness and flow resistance. The hydrological and fluvial characteristics of the Highland Water are typical of those that formerly occurred in much of southern England. * Nationally rare species are equivalent to those listed in the British Red Data Book which include those considered endangered, vulnerable or rare. Nationally notable/scarce species are estimated to occur in 16,100 10km grid squares in Britain. ** Species as listed under Schedule 5 or Schedule 8 of the Wildlife and Countryside Act,1981, as amended.

Species mentioned

Show the 77 species mentioned in the description, with red-list status ▾

Plant communities