Diagrams of Deposition & History Kimberlites are most commonly found as carrot-shaped pipes, or less
commonly, as dykes or as sills. There are three main zones associated
with kimberlite pipes: the crater, diatreme, and hypabyssal root zones. The presence and degree of preservation of these zones depends upon the level of erosion, the abundance of volatiles in the erupting magma, and the stability of the country rock. The kimberlites in Fort a la Corne have undergone very little erosion and glaciers have not scraped off the crater facies pyroclastics. This results in massive tonnenage deposits in which most of the deposit is tabular in shape which leads to very low waste to ore stripping ratios. In contrast, the Kimberley and Jagersfontein pipes are smaller and have been eroded down to the diatreme. Diagram of a Fort a la Corne Kimberlite
The following diagram emphasizes the size contrast (and potential ore tonnage) between a Fort a la Corne Kimberlite and a "pipe only" (Northwest Territories or South Africa) style Kimberlite.
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