The first Post in this Series is here.
Day 23, Thursday 11 March – Leithfield Beach and Kaikoura Coast. I spent nearly three hours on Leithfield Beach this morning on a cloudy day threatening rain, but the rain moved across to the north of me.
I always walk southwards from where I park the car at Leithfield Beach to fossick around these old stormwater pipes. The person near them provides scale.
Looking out to sea over the old stormwater pipes.
Leithfield Beach stones this morning, looking north. There is rain in the distance which fortunately did not come my way.
Leithfield Beach stones.
Probably a spotted shag.
Here are seven jaspers found on Leithfield Beach – I especially like the yellow in them. The seven go from the most to the least yellow, the least red to the most red. These stones are often less smooth than the ones I collect at Gemstone Beach and Kakanui, reflecting the state of most stones on the beach.
And another four stones from this morning:
Small stone. likely to have a lot of chaceldony (agate) in it.
It has been suggested that this is rhyolite.
Very unusual circular pattern on this stone.
I also found an unusual sea-weed like stuff on the beach and posted photos of it on the “New Zealand Lapidary, Rocks, Minerals, Fossils” Facebook Group (see first two photos below).
Found on Leithfield Beach.
Among the stones on Leithfield Beach.
Found on Leithfield Beach.
Found on Leithfield Beach.
Stan Wen, a Group member, did some research on it and eventually identified it as the strobila of a certain kind of jellyfish, part of its asexual reproductive process, as illustrated in this diagram from the Seattle Aquarium.

The Aquarium information states: “When a [jellyfish] polyp strobilates—segmenting its body to reproduce—it releases tiny ephyra into the water. Within a few weeks, a bell appears and the ephyra are considered medusa [adults].”
I then drove to Kaikoura and, in the late afternoon, spent about 40 minutes on the beach near my motel. Here are six stones from that fossick, the first of which has dendrites in it. A dendrite forms when a mineral, starting from a point of origin in the stone, migrates and branches outward.
The beach near my motel, looking back towards the Kaikoura Peninsula.
Kaikoura beach stones, late afternoon.
Dendrites in a stone.
Limestone. Likely to be too soft to polish.
Limestone. Likely to be too soft to polish.
Day 24, Friday 12 March, Last Day – Kaikoura Coast and Ward Beach. I often stop at a little spot on the Kaikoura Coast between Kekerengu and the Waima/Ure River mouth. I am especially interested in the stones there with zoophycos trace fossils. As noted on page 64 of “A Photographic Guide to Fossils in NZ” by H. Campbell et al. (2013), these trace fossils can be found in Muzzle Group geological strata in Marlborough, in fine-grained limestone, marl, mudstone and siltstone, laid down in deep water (over 150 metres), the traces due to burrowing activity by something like an echinoderm (see first photo below for this extract). The stones in the photos below are examples of the range of types of traces I found today, both at my Kaikoura Coast spot and at Ward Beach just over 20 kilometres north. These stones are likely to be too soft to tumble polish well so I left many of them on the beach.
Page 64 of “A Photographic Guide to Fossils of New Zealand” by Hamish Campbell et al. (2013).
Zoophycos trace fossil. The nested curving chevron-shaped trace is one I find particularly attractive.
Another zoophycos trace fossil from the Kaikoura coast.
Stone from Ward Beach.
Parallel zoophycos.
Another Ward Beach zoophycos.
Intersecting trace fossils.
Less organised and less well-defined, but traces probably as well.
A Ward Beach stone with a variety of zoophycos trace fossils.
Ward Beach stone, where the zoophycos traces are harder than the surrounding stone material so are slightly raised.
Some more photos from my stop on the Kaikoura Coast between Kekerengu and the Waima/Ure River mouth:
The beach between Kekerengu and the Waima/Ure River mouth. Looking south.
The stones on the beach. The white limestone(?) stones stand out.
Gorgeous green stone, maybe quartzite?
This stone looks like one where the burrowing that produced the zoophycos traces ended up producing actual holes in the stone (or the burrows were petrified with softer material and eroded away). Or maybe the burrows were made by a different animal. The other side of this stone is equally interesting (see next photo).
The other side of the previous stone.
About 12 kilometres further north on State Highway 1 is the small village of Ward. Ward Beach is about six kilometres off the main road, to the east, set among spectacular scenery – high hills with steep slopes and a coastline with interesting rock formations. The Ward Beach boulders (concretions) are not far from the car park (maybe 10 minutes walk north), although I did not visit them today. The beach was uplifted by the 2016 Kaikoura earthquake, unveiling the boulders.
The Ward Beach boulders – photo taken during an earlier visit.
Ward Beach boulder.
Ward Beach boulder.
When I arrived, there were about 6 to 8 people from the WSP company (formerly Opus), a Design, Engineering and Environmental Services Consultancy, picking up rubbish as a community service. One of them showed me a mannikin leg he had found, and I gave him a florescent light tube I had found. For a sense of the beach and its setting, see this web page.
Scenes from Ward Beach today:
Looking towards the Ward Beach car park.
Ward Beach stones.
Ward beach in front of the carpark, lowish tide.
White-faced heron on Ward Beach.
A surfer in high seas, just in front of the car park.
Five of the stones I found today on Ward Beach:
Gorgeous little stone I found at Ward Beach. Could be a quartzite.
Other side of previous stone.
Treasure
My trip back over Cook Strait the next day was uneventful in stark comparison to the sailing of nearly four weeks previously!