The Ordnance Survey project to produce the first national maps of England and Wales
at one inch
to the mile was launched in 1825 and by 1838 the survey of Wales was almost complete as well as
English counties south of the Wash. The triangulation of Great Britain and Ireland was completed in
1841.
In 1836 Parliament passed the Tithe Commutation Act. This provided for the payment
of tithes in
goods, such as crops, to be converted into the payment of a tithe rent, to be paid in money. Under
the Act, accurate maps were needed to show the apportionment of rent to land and the
circumstances were thought by the Ordnance Survey to merit government authority to produce the
necessary a large-scale survey of England and Wales. However, funds were being raised locally,
with individual parishes bearing a charge based on acreage. The Ordnance Survey pointed out that
it would be just as easy to make a complete survey of the country rather than a piecemeal survey,
and that the resulting maps 'instead of being wasted for all other public purposes, shall be so
expended as to be the means ... of supplying all the wants of the Nation as connected with survey'.
Private estates, at this time, were commonly mapped at 1 inch to 3 chains (26% inches
to 1 mile,
or 1 : 2376) and the Tithe Commissioners agreed that this was 'the smallest which can faithfully
show all the detail required'.
Although the Tithe Commissioners were convinced about the overwhelming merits of a
national
survey, the Select Committee set up to consider the issue was not . They concluded that not only
was a general survey not required, but that it would be unfair on the landowners to insist that they
should pay for the survey of areas not affected by the Tithe Act. The tithe surveys went ahead and
were carried out by contracted surveyors whose charges were levied on the parishes. This enabled
them to pay higher wages than the Ordnance Survey who lost many experienced men to the tithe
surveys and had to introduce a 'working pay' allowance to try and minimise losses of staff.
The passing of the Enclosure Act in 1845 also generated a need for maps and it was
here that the
false economy of the 'cheap' tithe survey was exposed. Only a small proportion of the tithe maps
were found to be accurate enough for the later enclosure survey and most areas had to be
resurveyed. Again Ordnance Survey staff were attracted away by higher wages paid by contractors.
It was not until 1870 that the mapping of England and Wales on a 1 inch scale was
complete. The
first edition of the 1:2500 and 6 inch maps were made available to the public in 1853 and 1858
respectively. These maps describe local boundaries in great detail as required under the the
Ordnance Survey Act of 1841.
The Hundred Boundaries of course are simply the joined up sections of the relevant
parishes at the
boundary, and were not consistently emphasised. From time immemorial boundaries were never
written down or plotted on a map, and we shall never know how close the first maps come to giving
the accurate disposition of these folk divisions. As far as Suffolk is concerned the only map to
show the hundred boundaries was that produced for the county by Hodgkisson in 1783. It is this
map that will be used as the base line for tours around the Hundreds.
With respect to mapping
natural resources, in the 1980s new impetus was given to the definition of natural
regions by the designation of 'Environmentally Sensitive Areas' by the Ministry of Agriculture, three
of
which are partly in Suffolk. In 1996 the Countryside Commission and English Nature produced a map
entitled The Countryside of England, landscape, wildlife and natural features, which identified
seven
'Character Areas' in Suffolk. Based on this, English Nature has defined the following six 'Natural Areas'.
1. Wet peat-based soils
of the Fens and river valleys
2. Soils derived from
chalk
3. Mixtures of peat,
chalk and sand in the Fen 'skirtland'
4. The sandy soils
of Breckland and the Sandlings
5. Clay loams derived
from chalky boulder clay, sandier in the east than in the west. Young's 'Strong Loam'
6. Loamy soils, mainly
in river valleys
7. Loamy soils derived
from loess, overlying sands and gravels. Young's 'Rich Loams'
8. Wet alluvial soils
in coastal and river marshes