Kaitiaki are rarely resourced to respond to the many requests for their time and expertise.

If this view be correct there must have been a great difference in the sedimentation of the two areas, as the thick beds consist of alternations of flaggy sandstone with occasional true sandstone, almost pure limestones, calmstones, and few or no real flagstones.

Why should I go gadding and fizgigging after firking flantado amphibologies?

Your borderline remarks about my aunt's dress destroyed my evening.