Selected Mesozoic and Cenozoic faunas and landscapes, North Island of New
Zealand
29 June - 4 July 2002
Pre-Meeting Field Excursion 5 of the First International Palaeontological
Congress 2002
led by Austin Hendy and Penelope Cooke
with Peter Kamp, Adam Vonk & Chris Hendy
all from University of Waikato, Hamilton
Photos copyrighted 2002 by Don Chesnut, unless otherwise
indicated
Day One (29 June)
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Stop 1, Auckland city and its basalt volcanoes, Mt. Eden (One Tree Hill)
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monument at One Tree Hill
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view from One Tree Hill
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Maori fortifications (earthenworks) constructed
during war with the British
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view from One Tree Hill
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another view from the Hill
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field trip participants and leaders
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Stop 3, Kawhia Harbour, Jurassic marine strata
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landscape in the area, I forget the significance
of this photo
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another view
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roadcut with Jurassic marine strata exposed
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Stop 5, Taumatototara Road, Jurassic marine strata, Kawhia Series
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bivalves, probably the inoceramid
Retroceramus
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view (through the rain), note dipping beds of an
anticline to the left and right
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view of same area
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same view
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Stop 6, Magnetite-sand mine (not in guidebook)
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mine area. Sand is very magnetite rich, a result
of concentration by coastal processes. The source of the magnetite is from
volcanoes to the south. I collected a sample of the sand, but it was confiscated
at Australian Immigration and Customs.
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Stop 7, Waitomo Caves (not in guidebook). We had a special night tour and
boat ride in the famous glow worm cave. Glow worms are actually larvae of
the "gnat" Arachnocampa luminosa. They each dangle a sticky thread
to catch other insects attracted to the light.
Day Two
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Stop 1, Kiritehere Beach, Late Triassic marine strata, Balfour Series
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exposures of Triassic strata during low tide
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view of rugged coastline from the beach
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slab with abundant bivalve fossils, chiefly
Monotis
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same slab
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another slab with fossils
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same slab
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View of the coast through the rain
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Stop 3, Marakopa Falls, formed at indurated Mesozoic conglomerate
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view of Falls through the rain
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another view
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yet another view
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walk through very dark and wet tree-fern forest
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forest of abundant and diverse tree ferns
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Stop 2, Mangapohue Natural Bridge, Late Oligocene, Orahiri Limestone, Te
Kuiti Group. Most of the landforms in this area are karstic. This natural
bridge is a remnant of and extensive cave system. Most of the cave ceiling
had collapsed.
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climbing through the natural bridge
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looking up through the bridge
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looking back down at the stream
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another view of stream
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karst landscape on other side of natural bridge
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one of the limestone outcrops, I forget the
significance.
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View of sheep-covered hills,
another view of same hills
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Stop 4, Ruakuri caves and forest walk, karst topography of the Te Kuiti Group
limestones
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giant Moa toe bones, found in nearby cave deposits
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overlook onto rapids
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swinging bridge
Day Three
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Stop 1, Otorohanga Kiwi House, here we saw several
types of kiwis and the primitive tuatara reptile, Sphenodon, and other,
mostly avian wild life.
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Stop, Mangaogaki Gorge, not in guidebook.
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looking at outcrop
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vista
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another vista
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Stop 2, Awakino Gorge
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roadcut near the Awakino tunnel, sandstone is Tertiary
Te Kuiti Group
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Stop 4, Mokau, lunch stop, view overlooking Mokau River and cliffs of Late
Miocene sandstones and mudstones of the Mt. Messenger Formation. This is
a tidally influenced river mouth; we saw the tidal bore traveling upstream
during lunch.
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view of surf and river
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another view
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Stop 5, Mohakatino River mouth
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view of Mt. Messenger sandstone overlying mudstone
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Stop 6, Kaway Pa, Mt. Messenger Fm. sandstones
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view of exposure with rugged surf
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another view
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yet another view, Carl "Surf's Up" Brett on the
right
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Stop 7, Tongaporutu River mouth, Mt. Messenger Fm.
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view of the cliffs at the river mouth
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Stop, Methanex Plant, not in guidebook
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Distant view of Mt. Taranaki, a snow-covered volcano
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Stop 8, New Plymouth coast, volcanic plugs of the Sugar Loaf Islands
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view of Sugar Loaf Islands
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view 2
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view 3
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view 4
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view 5
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view 6
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view 7
Day Four
Day Five
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View of Pleistocene terrace; terrace begins at fence,
early morning
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Stop 1, Castlecliff coastal section, Pleistocene cyclothems of the Wanganui
Basin
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foot path and footbridge to the beach cliff exposures
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fallen block containing shell bed
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beach cliff exposure
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Pleistocene bivalves
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Pleistocene gastropod, I don't know the species
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Pinnid bivalves, Pleistocene; don't know the species
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ripple-bedded sandstone, Pleistocene, hammer for
scale
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Stop 2, Rangitikei River, section through Pliocene strata of the Wanganui
Basin
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vista 1, unreal green
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vista 2
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vista 3
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Stop 3, Tongariro National Park, volcanic centers, volcanoes too clouded
over to see
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Volcanoclastic deposits from volcanic centers,
pyroclastic flows?
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Stop 4, Taupo caldera, Lake Taupo was formed in the caldera which was created
in an eruption about 26,000 years ago.
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view 1, lake in background, cinder cone in midground
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view 2
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view 3
Day Six
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Overlook near Taupo city, edge of caldera
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view 1 with bit of a rainbow
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view 2
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view 3
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Wairakei Park, Huka Falls
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view of falls and rapids
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another view of falls
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yet another view
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pumice deposit from the Taupo ignimbrite, ca 200
AD
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Stop 1, Craters of the Moon, Wairakei Park, bubbling mud pools and steam
vents
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Craters of the Moon
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steam vents (and clouds)
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large steam vent, new vent pits are occasionally
created explosively.
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another large steam vent
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Stop, Aratiatia Dam, Wairakei region
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Lord of the Rings film crew, robotic camera to descend
steel cable into gorge below dam
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release of water from the dam
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increasing flow
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released water beginning to fill gorge pool
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pool filling 2
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pool filling 3
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pool filling 4
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water surging in rapids below pool
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view of filled pool and rapids
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Stop, Wairakei Power Station, New Zealand's oldest geothermal power station
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view 1
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view 2
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view 3
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Stop, Whakamaru Dam
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power station
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downstream from power station, cliffs are entirely
200,000-year-old ignimbrite deposits
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lake upstream from power station, cliff probably
dacite volcanic plug in rhyolite host
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Stop, Hauraki Peat mine, Moanatuatua peat was a raised peat bog (ombrogenous).
The deposit is about 1 meter above sea level, but the peat is about 20 meters
thick. It is being mined for potting soil.
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the mine
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the peat
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Stop 4, Mirand, on the Thames estuary,
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beach or chenier ridge separating mangrove tidal
flats to the right and the Firth of Thames to the left.
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close-up photo of the shell accumulation on the
narrow strand; shells mostly bivalves.
References
All information came from the field trip leaders and from the following
guidebook:
Cooke, P.J. and Hendy, A., 2002, Selected Mesozoic and Cenozoic faunas and
landscapes, North Island of New Zealand, 20 June - 4 July 2002. First
International Palaeontological Congress, IPC2002 - Australasia, Pre-5 Field
Excursion Guidebook. Macquarie University, Sydney, 20 p.
All misinformation can be entirely attributed to me and I welcome corrections.
Thank you. Don Chesnut
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