Mudeford Spit
Looking back along the Spit to Mudeford Quay. The strip of water in between is the entrance to Christchurch Harbour from the Atlantic Ocean.
Historically part of Christchurch, Mudeford Spit was sold to Bournemouth Borough Council in 1935. It is the larger of the two features, the other being the Haven, that almost enclose Christchurch Harbour, leaving its water to rise and fall through a narrow channel known as The Run. Formed by sand and shingle brought around Hengistbury Head by longshore drift and pushed towards the shore by waves from the east, the spit is the most mobile of Dorset's geographical features. Prior to the construction of the long groyne at Hengistbury Head in 1938, it tended to grow steadily in a north-easterly direction and on occasion stretched as far as Steamer Point and Highcliffe Castle; most notably in 1880. It has been breached a number of times naturally; 1883, 1911, 1924, 1935 and once deliberately in the 17th century when an attempt was made to construct another entrance to the harbour. After the last breaching in 1935, the end of the spit broke off and drifted towards the section of eastern beach known as Friars Cliff where it formed a lagoon. The groyne built in 1938 to protect Hengistbury Head from erosion had an adverse effect on the spit as it prevented movement of material around it. The spit began to erode due to wave action from the east and many attempts have been made since to stabilise the situation. Small seawalls were constructed on the spit in the 1960s and a large number of rubble groynes were put down during the 1980s.
Beach huts on Mudeford Spit can be reached on foot from the main part of Bournemouth Bay, or by ferry from Mudeford Quay. On the spit is the "Black House", a local landmark – in various local smuggling legends, it was built in 1848 for the manager of the Hengistbury Head Mining Company, and therefore these tales are unlikely to be true.
Text courtesy of Wikipedia.
Mudeford Spit
Looking back along the Spit to Mudeford Quay. The strip of water in between is the entrance to Christchurch Harbour from the Atlantic Ocean.
Historically part of Christchurch, Mudeford Spit was sold to Bournemouth Borough Council in 1935. It is the larger of the two features, the other being the Haven, that almost enclose Christchurch Harbour, leaving its water to rise and fall through a narrow channel known as The Run. Formed by sand and shingle brought around Hengistbury Head by longshore drift and pushed towards the shore by waves from the east, the spit is the most mobile of Dorset's geographical features. Prior to the construction of the long groyne at Hengistbury Head in 1938, it tended to grow steadily in a north-easterly direction and on occasion stretched as far as Steamer Point and Highcliffe Castle; most notably in 1880. It has been breached a number of times naturally; 1883, 1911, 1924, 1935 and once deliberately in the 17th century when an attempt was made to construct another entrance to the harbour. After the last breaching in 1935, the end of the spit broke off and drifted towards the section of eastern beach known as Friars Cliff where it formed a lagoon. The groyne built in 1938 to protect Hengistbury Head from erosion had an adverse effect on the spit as it prevented movement of material around it. The spit began to erode due to wave action from the east and many attempts have been made since to stabilise the situation. Small seawalls were constructed on the spit in the 1960s and a large number of rubble groynes were put down during the 1980s.
Beach huts on Mudeford Spit can be reached on foot from the main part of Bournemouth Bay, or by ferry from Mudeford Quay. On the spit is the "Black House", a local landmark – in various local smuggling legends, it was built in 1848 for the manager of the Hengistbury Head Mining Company, and therefore these tales are unlikely to be true.
Text courtesy of Wikipedia.