Eruptions of kimberlite volcanoes are a poorly-understood phenomena, as
there have been no historical eruptions of kimberlite, and primary
deposits and edifices of kimberlite volcanoes are rarely preserved. In
particular, the styles of explosion, magma fragmentation, and primary
deposition of kimberlite remain unclear. This thesis comprises field and
laboratory study of five kimberlite deposits within the A154N kimberlite
volcano at Diavik, NWT, Canada. These studies provide critical
descriptive and semi-quantitative data on the geometries, component
variations, and relative age relationships of deposits. These data are
used to associate volcanic deposits with kimberlite eruption processes.
Finally, these volcanic processes are shown to have direct implications
for the distribution of diamonds within kimberlite pipes.