Geology of the Andover area: Concealed strata
This page is part of a category of pages providing a summary of the geology of the Andover district (British Geological Survey Sheet 283), which extends over approximately 600 km2 of north-west Hampshire and a small part of eastern Wiltshire. Links to other pages in this category can be found at the foot of the page. Authors: J Thompson, K A Lee, P M Hopson, A R Farrant, A J Newell, R J Marks, L B Bateson, M A Woods, I P Wilkinson and N J Smith. |
There are six deep hydrocarbons boreholes, within or adjacent to the Andover district, which provide evidence of the strata encountered at depth. Figure P807821 shows the location of the boreholes and the Stratal thickness table details the stratal thicknesses within each. Seismic sections show that Ordovician to Carboniferous strata form the basement beneath the area.
Strata | Kingsclere | Egbury 1 | Upper Enham 1 | Ham 1 | Hurstbourne Tarrant | Carnarvon Arms |
Borehole number | SU45NE 1 | SU45SW 46 | SU35SE 23 | SU36SW 1 | SU35SE 27 | SU45NE 3 |
Grid reference | 49840 58200 | 44484 52364 | 36598 50430 | 33100 62470 | 36032 53500 | 45720 59450 |
Palaeogene | Absent | Absent | Absent | Absent | Absent | 124.6 |
White Chalk
Subgroup |
Absent | 170.6 | Absent | Absent | 217.6 | 12.5+ |
Grey Chalk
Subgroup |
Absent | 68.4 | Absent | 18.3 | ||
Upper Greensand
Formation |
33.8 | 70.0 | 57.7 | 42.7 | 62.8 | |
Gault Formation | 86.6 | 41.0 | 58.7 | 84.1 | 55.5 | |
Lower Greensand
Group |
13.7 | 10.5 | 11.3 | 4.8 | 10.4 | |
Wealden ‘Group’ | 178.9 | 118.5 | 127.1 | 11.0+ | 125.9 | |
Purbeck Group | 164.3 | 43.5 | 53.8 | 36.3 | ||
Portland Group | 43.6 | 46.0 | 53.4 | 50.0 | ||
Kimmeridge Clay
Formation |
284.4 | 187.5 | 203.2 | 218.2 | ||
Corallian Group | 53.6 | 58.0 | 57.5 | 125.0 | ||
Oxford Clay
Formation |
95.1 | 117.3 | 132.7 | 25.0 | ||
Kellaways Formation | 9.1 | 10.5 | 14.0 | 14.0 | ||
Great Oolite Group | 85.0 | 93.9 | 108.1 | 61.0 | ||
Inferior Oolite
Group |
109.4 | 48.3 | 75.9 | 118.3 | ||
Lias Group† | 360.9+ | 377.7 | 495.5 | 38.4+ | ||
Penarth Group | 9.3 | 28.5+ | ||||
Permo-Triassic | Absent | |||||
Ordovician to Carboniferous | 29.0+ |
Notes:
†The Lias Group undivided encompasses the old divisions of Lower, Middle and Upper Lias. Modern terminology that can be
applied to the strata encountered in these boreholes is discussed on the Jurassic page.

Additional data in nearby deep wells such as Farley South, Stockbridge, Lockerly and Humbly Grove can be found in Hopson et al. (2007)[1], Booth (2002)[2] and Farrant (2002)[3].
References
- ↑ Hopson, P M, Farrant, A R, Newell, A J, Marks, R J, Booth, K A, Bateson, L B, Woods, M A, Wilkinson, I P, Brayson, J, and Evans, D J. 2007. Geology of the Salisbury district. Sheet Explanation of the British Geological Survey. Sheet 298 (England and Wales).
- ↑ Booth, K A. 2002. Geology of the Winchester district. Sheet Explanation of the British Geological Survey.Sheet 299 (England and Wales).
- ↑ Farrant, A R. 2002. Geology of the Alresford district. Sheet Explanation of the British Geological Survey.Sheet 300 (England and Wales).