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      3 General description

    The name "cursus" was first used in an archaeological context by
    William Stukeley in the early 18th century to describe a linear
    enclosure to the north of Stonehenge, Wiltshire, which he likened to
    a racecourse. When similar monuments were identified as cropmarks in
    the upper Thames Valley (Leeds 1934) it was suggested that the word
    cursus be used as a suitable term to describe these too (Crawford
    1935). Known examples of the newly defined class were discussed by
    Stone in 1940, and by 1960 some 16 sites were included in a list
    published by the Royal Commission on Historical Monuments (RCHM
    1960). In the last 10 years or so a number of cursus have been
    investigated in some detail, including Springfield, Essex (Hedges &
    Buckley 1981), Maxey, Cambridgeshire (Pryor & French 1985), and the
    Dorset Cursus, Dorset (Bradley 1986).

    The most distinctive feature of any cursus is its perimeter
    earthwork. This almost always comprises a simple bank and ditch, but
    in Scotland a number of cursus are defined by a row of closely-set
    pits or postholes. Because the pit-edged cursus are, according to
    present evidence, confined to Scotland they are not described in
    detail in this paper.

    The scale of the ditches surrounding cursus vary greatly. At Rudston
    A, North Yorkshire, the ditch had a maximum width of 4.0m, and
    although most cursus ditches are within the range 2.0m - 3.0m across
    some can be as little as 1.5m. wide. The Dorchester-on-Thames cursus
    ditch had a maximum depth of a little less than 2.0m, but at Maxey,
    Cambridgeshire, the ditch was only 0.6m deep. In cases where several
    sections across the ditches of a single cursus have been studied it
    is clear that the size of the ditches increase significantly towards
    the terminals. Ditches are generally U-shaped in cross section.

    Most investigated cursus show either earthwork evidence, or silting
    profiles in the ditches, which suggest the presence of an internal
    bank along all four sides of the monument (ie. side banks). In some
    cases these may have been revetted by turf walls and stood anything
    from 1.5m to 3.0m high. In some cases a berm separates the bank from
    the ditch. There are, however, exceptions. At Aston, Derbyshire, an
    outer bank is postulated, and at Thornborough, North Yorkshire, both
    inner and outer banks may have been present. At Scorton, North
    Yorkshire, the spoil from the side ditches seems to have been dumped
    in the area between the ditches to form a low mound or platform
    along the whole length of the enclosure (ie. centre bank).

    Access to the interiors of cursus was greatly restricted.
    Entranceways occur most often near one end of the long sides, but
    may also be found in the centre of the long sides or at the ends.
    The Dorset cursus appears to have had only two entrances, both of
    them 900m from its northern end.

    Cursus vary in size enormously. Short examples, sometimes known as
    minor cursus, range from about 250m to about 900m long, whereas the
    larger examples, or major cursus, may be anything up to 5.6km long.
    The Dorset cursus is often cited as being about 10km in length, but
    this monument is in fact two cursus joined together, one of 5.6km
    and the other of 4.3km. Other long cursus may also result from
    several shorter examples being set end-to-end. Cursus width varies
    roughly proportionally with length in the sense that the longest
    cursus are also the widest, but in no cases does the width of a
    cursus exceed 130m; most are in the range 20-60m.

    In outline, the long sides of a cursus are roughly parallel to one
    another, but when examined in detail most show slight variations in
    width and alignment. Often, one of the long sides is fairly straight
    while the other has a more uneven course. This has led to the
    suggestion that one side was ranged out while the other was
    determined by a series of offsets from the first line. Other
    explanations are equally likely, however, and at Springfield, Essex,
    excavations have shown that a kink in the south side was orientated
    on an earlier pit which was cut by the cursus ditch, while elsewhere
    pre-existing monuments may have been the cause of deviations.

    The greatest variations in ground-plan occur at the terminals, and
    on the basis of terminal shape Loveday has proposed the following
    simple sub-division of the class:

        * A. Round-ended types in which the terminals have curved
          earthworks across the ends either semi-circular or
          semi-elliptical in plan.

        * B. Square-ended types in which the terminals have straight
          earthworks across the end set either at right-angles to the
          side ditches or obliquely to form a bevelled end.

    A selection of simplified ground-plans illustrating examples of
    these two main types is given on Figure 1.

    Cursus are rarely straight. Most have a slight curve in their main
    axis, and some of the longer examples contain distinct changes in
    alignment along their course. In some cases this may be due to the
    amalgamation of several individual cursus to form a single much
    larger structure, but mostly these changes in axis seem to have been
    part of the initial design. Bradley (1986, 4) has suggested that in
    the case of the Dorset cursus the changes in alignment were made to
    incorporate existing monuments of other classes.

    Cursus have no common orientation, and while it has been claimed
    that they were built as celestial observatories there is no firm
    evidence for this, and any correspondence with major risings or
    settings of the sun or moon may be coincidental. Cursus often run
    across valleys, and their setting and scale can only be fully
    appreciated by standing at the terminals which are usually
    intervisible. It has frequently been pointed out that many cursus
    have their terminals close to water courses or run across an
    interfluve between two rivers. This is especially true of many
    valley-situated cursus, and it may also be noted that because of
    their proximity to rivers some cursus are wholly or partly covered
    by alluvium. Whether the activities undertaken at cursus were in any
    way connected with water or water-courses is not known.

    Few cursus have been excavated on a sufficient scale to allow much
    insight into the nature and variety of internal features; even large
    excavations at cursus have only examined a small percentage of the
    overall monument. Bedrock-cut features are often found at or near
    one or other of the terminals. At Springfield, Essex, internal
    features included a circular setting of upright posts and a variety
    of pits and scoops containing burnt soil and cremated bone. These
    were concentrated at the east terminal, and in contrast very little
    was found at the western end. Elsewhere, for example at
    Thornborough, North Yorkshire, burials have been found within the
    enclosure or in the ditches. At Drayton, Oxfordshire, two pits
    containing human bone were recorded.

    Blank areas are certainly present in most cursus, but whether any
    sites totally lacked internal features is not known.

    Flintworking debris has been found in the fills of many excavated
    ditches, or in the immediate vicinity of the site. Pottery is
    generally scarce at cursus sites, and seems more frequent in the
    upper ditch fills than in primary silting.

    In most cases, ditches silted-up naturally, but occasionally signs
    of back-filling and recutting have been reported. At Maxey,
    Cambridgeshire, the excavator suggested that the cursus ditches were
    dug over a long period as a series of alignments with a similar
    orientation and that for this reason the ditches were never all open
    at the same time.

    Surface surveys around Maxey, Cambridgeshire, showed that there was
    no increase in the density of flintwork over the cursus and that
    phosphate levels showed no enhancement within the cursus.

    Cursus have been interpreted in various ways since their initial
    identification as a class of monument. The name itself is the latin
    term for a race-track and this was one of the possible functions
    suggested by Stukeley. More recently a ritual/ceremonial role has
    been assigned to cursus, particularly in the light of evidence for
    the burning of animal (and perhaps human) bodies, and the
    associations (see below) with burial monuments of various classes.
    Pryor (1985, 301) has suggested that three kinds of cursus can be
    identified on the basis of their form and the duration of usage: (1)
    Monumental or continuously used sites, eg. the Dorset cursus; (2)
    Short-lived, single period sites, eg. Springfield, Essex; and (3)
    Long-lived episodic ditched alignment sites, eg. Maxey, Cambridgeshire.