The main theoretical issues in the study of the history of the Archaea
n Controversy in Britain, which arose in the first three papers of the
present series, are summarized and discussed-in particular the proble
m of stratigraphical work in rocks where no fossils can be discerned.
The 'Archaean' geologists showed some leanings towards Neo-Neptunism a
nd this, together with the fact that their work challenged the Murchis
on/Survey view of British geology, was one of the reasons for the cont
roversy. At a deeper level, however, the question concerned the doctri
ne of uniformitarianism: Were metamorphic rocks to be found at any par
t of the stratigraphical column, or were they confined to the earliest
period of the Earth's history? The establishment of the concept of Pr
ecambrian rocks and a suitable stratotype boundary is essentially a so
cial question that has to be determined within the geological communit
y. Some of the social processes whereby these matters are decided inte
rnationally are considered, and it is noted that the best location of
the 'Golden Spike' for the Precambrian/Cambrian boundary has only just
been settled (by vote). The paper also explores some nineteenth-centu
ry ideas about the nature of metamorphism, and the early conditions of
the world.