RETAIL PARK 5,000 Sq Ft to 20,000 Sq Ft

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• 100,000 sq ft of Retail & Leisure • Immediately adjacent to SLEAFORD the town centre • Unit availability of between RETAIL PARK 5,000 sq ft to 20,000 sq ft • Opening 2019 NG34 7HH LOCATION Minting LINCOLN Bardney A158 The Lincolnshire market town of Sleaford is situated 10 Branston Horncastle Sutton North miles north-east of Grantham, 16 miles west of Boston on Trent Hykeham and 17 miles south of Lincoln. A46A46 A15A15 Collingham Woodhall Spa Witham St Hughs The proposed Sleaford Retail Park will be located A16 immediately adjacent to the town centre, at the Navenby Coningsby NEWARK - Stickney southern end of Southgate, the towns principal ON - TRENT A17A17 SLEAFORD retail pitch. The scheme will be accessed via a new RETAIL PARK link road off Boston Road, which is the main route into the town from the east. Caythorpe Long BOSTON Bennington Ancaster A17A17 Heckington A15A15 LINCOLN Wyberton Fishtoft Belton Bottesford Swineshead R OAD A52A52 Kirton GRANTHAM A52A52 Donington B1517 A607 A15A15 Surﬂeet Bulby Corby Glen Pinchbeck Colsterworth Holbeach Spalding South Witham Bourne Stapleford Holbeach AD St Johns RETAIL PARK BOSTON RO SLEAFORD CASTLE THE HANDLEY MONUMENT 50,000 RAILWAY STATION people within BASS 20minutes GRANTHAM ROAD MALTINGS drive time ONDON ROAD L DESCRIPTION Sleaford Retail Park will comprise a total of 100,000 sq ft of retail and leisure space, immediately adjacent to the town centre. PLANNING The site has planning consent for 70,000 sq ft of ﬂoorspace for food retailing, however a revised application for outline consent will be submitted in May 2018 for the proposed scheme. TIMING Anticipated handover to tenants in Q4 2019. AVAILABILITY Unit availability of between 5,000 sq ft to 20,000 sq ft will exist, with other sizes deliverable subject to planning Misrepresentation Act: These particulars are produced in good faith and believed to be correct, however McMullen Wilson, GL Hearn or their client guarantees their accuracy nor are they intended to form any part of a contract. No person within McMullen Wilson’s orGL Hearn’s employment has authority to give any representation or warranty in respect of this property. May 2018. G IING N E OWLINGOWL GREEGREEN B S UB OWLSOWL L B C D OA RROA ON RICHARD GARSIDE GARDEN DD 020 7851 4956 BOSTONBOST CENTENTRERE M 07775 836759 [email protected] 7K NFR 20K+5K MEZZZANINEANINE OUND 3K 3K P POUND M M COM COM C FOOD RRETAILETAIL NIT NIT U U 11K+6K MEZZANINMEZZANINEE 4.7K 4.7K THROUGH THROUGH ADAM DE SWARTE A3/A5 A3/A5 A3/A5 A3/A5 DD 020 7851 3759 DRIVE DRIVE DRIVE DRIVE M 07557 433386 G NFR [email protected] NGN 7.5KK+7.+7.5K MEZZANINE SPACES T LIVI N 60K NFR ARK SPACES 7.5K+7.57.5K+7.5KK REMEN MEZZANINZANINEE RETIRETIREME 300 CAR PPARK NFR 6k+4k+4kk MEZZMEZZANINEANINE NFR D D D 5K OA OA N R N ON O T OST BOSTON R BOSTON BO BOS MASTERPLAN BRADLEY SMITH DD: 0203 058 0206 M: 07808 479 267 [email protected] For further details contact.

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Groundwater in Jurassic Carbonates
Groundwater in Jurassic carbonates Field Excursion to the Lincolnshire Limestone: Karst development, source protection and landscape history 25 June 2015 Tim Atkinson (University College London) with contributions from Andrew Farrant (British Geological Survey) Introduction 1 The Lincolnshire Limestone is an important regional aquifer. Pumping stations at Bourne and other locations along the eastern edge of the Fens supply water to a large population in South Lincolnshire. Karst permeability development and rapid groundwater flow raise issues of groundwater source protection, one of themes of this excursion. A second theme concerns the influence of landscape development on the present hydrogeology. Glacial erosion during the Middle Pleistocene re-oriented river patterns and changed the aquifer’s boundary conditions. Some elements of the modern groundwater flow pattern may be controlled by karstic permeability inherited from pre-glacial conditions, whereas other flow directions are a response to the aquifer’s current boundary conditions. Extremely high permeability is an important feature in part of the confined zone of the present-day aquifer and the processes that may have produced this are a third theme of the excursion. The sites to be visited will demonstrate the rapid groundwater flow paths that have been proved by water tracing, whereas the topography and landscape history will be illustrated by views during a circular tour from the aquifer outcrop to the edge of the Fenland basin and back. Quarry exposures will be used to show the karstification of the limestone, both at outcrop and beneath a cover of mudrock. Geology and Topography The Middle Jurassic Lincolnshire Limestone attains 30 m thickness in the area between Colsterworth and Bourne and dips very gently eastwards.
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194947 Wood Farm.Indd
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«Apn Id» «Decn Level»
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