If your route allows, stop the bus at a point on the Havelock North flats where the full ridgeline is visible: the Te Mata Road area or the Tukituki River bridge approach both work. Students sketch the silhouette of the ridge from a distance. This is the view of the giant. Ask: what shape does the ridge make? This sketch is returned to at step 6.
Before anything else, establish the edge protocol clearly: a designated safe zone for approaching the cliff edge, a maximum proximity rule, and no running near the cliff. Identify where paragliders are operating and establish the clear zone around the launch area. Then orient students: which direction is north, where is the coast, where is the Tukituki River.
Facing north, south, east, and west in turn, students identify and record what is visible: the Heretaunga Plains, the Tukituki River and its course to the coast, the Kaweka and Ruahine Ranges, Napier and the harbour, the Māhia Peninsula on the northern horizon, Cape Kidnappers / Te Kauwae-a-Māui to the south. Name each feature before recording it. The viewshed sketch should show direction, distance, and land use type for each quadrant.
The rock at Te Mata is Awapapa Limestone, about 3.5 million years old. Examine the tilted bedding planes: these layers were once horizontal seabed, now raised and angled by tectonic uplift that continues today. Look for the alternating bands of harder grey limestone and softer orange layers, which record ice age sea level cycles. Search exposed rock surfaces for fossil outlines: oysters, scallops, barnacles, brachiopods, and bryozoans are all present. Sketch what you find and note its location. Do not remove material from the rock.
Note wind direction using the feel on the skin and movement of any vegetation. Estimate wind strength using the Beaufort scale descriptions introduced before the visit. Record the difference between conditions at the summit and at the base. This connects to the geography of the ridge as a wind accelerator and to the paragliding activity visible at the site.
On the return journey, stop again at the viewpoint used in step 1. Students retrieve their sketch and compare it with notes made while standing on the ridge. The question from before the visit is now answerable: what does the ridge look like from inside the legend, versus from the distance at which the legend was first told? This comparison is the mātauranga Māori teaching moment.
| Direction | Key features |
|---|---|
| North | Heretaunga Plains, Napier, Hawke's Bay, Māhia Peninsula on the distant horizon |
| East | The cliff face dropping to the eastern slopes, the coast, and the open Pacific |
| South | Tukituki River valley, Cape Kidnappers / Te Kauwae-a-Māui, the coast to the south |
| West | Kaweka and Ruahine Ranges, the upper Tukituki catchment, and the inland hill country. These ranges were the ancient coastline when the Awapapa Limestone beneath your feet was being laid down as seabed. |
Every prompt below is anchored in something students collected, sketched, or experienced at Te Mata: a viewshed sketch, field notes on tilted rock beds, a description of the wind on the ridge, or a question opened by the legend encountered in the place where it happened. The field record is the starting point. AI output without that anchor is not part of this framework.
You know the name Te Mata o Rongokako. Tell a gen AI chatbot the name and ask what it means. Compare the answer with what you learned before or during the visit. Ask the AI to explain the legend in simple words. Did it match the version you were told? What was different?
Describe the limestone you saw at the summit to a gen AI chatbot: pale, hard, sometimes with shell shapes in it, found in tilted layers. Ask what limestone is made of and how it forms. Ask the chatbot what was at Te Mata Peak a very long time ago, before there was a peak at all. Does the answer surprise you?
You felt the wind on the ridge. Tell a gen AI chatbot where you were standing and ask it to explain why ridge tops are windier than the land below. Ask it to explain why paragliders choose a ridge like Te Mata to launch from. Does the explanation match what you observed and felt at the summit?
Use your viewshed sketch from the summit to describe to a gen AI chatbot what you could see and in which direction. Ask it to explain why you could see so much further from the top of Te Mata than you can from the school playground. What does the word "viewshed" mean and where do geographers use it?
Using your observations of the Awapapa Limestone at the summit, including the tilted bedding planes, the alternating hard and soft layers, and any fossils you found, ask a gen AI chatbot to explain how sedimentary rock that was once a shallow offshore seabed 3.5 million years ago can end up as a steeply tilted ridge 399 metres above sea level. What tectonic forces are at work in Hawke's Bay? Verify key claims against a GNS Science source and note any discrepancies.
Using your annotated viewshed sketch, ask a gen AI chatbot to explain how the Heretaunga Plains formed: why the land is flat, why the river follows the course it does, why the alluvial plain supports intensive horticulture. Ask how the plains might look in 100 years if sea level rises 50 centimetres. Does the AI engage with that question carefully or confidently? What does the difference indicate?
The legend of Te Mata o Rongokako accounts for a real landform. Ask a gen AI chatbot: what geographic or geological knowledge is embedded in the legend, and what does it tell us about how Māori described and recorded their environment? Compare the AI answer with an iwi endorsed account. Where does the AI understand the relationship between story and landscape? Where does it miss something important?
You observed paragliders launching from the summit and felt the ridge lift yourself. Ask a gen AI chatbot to explain the physical geography of ridge lift: why ridges accelerate wind, how paragliders use this, and what the relationship is between landform shape and air movement. Connect the explanation to your Beaufort scale observations from the summit.
Using your field observations of the limestone bedding, the ridge asymmetry, and the cliff face profile, ask a gen AI chatbot to construct a geomorphic process account of how the Te Mata ridge reached its current form. Identify which claims are geologically defensible, which require verification against a GNS Science source or peer reviewed geology, and where the AI introduces imprecision about the tectonic setting of Hawke's Bay.
The legend of Te Mata o Rongokako encodes landform observation, spatial orientation, and a relational account of how people and landscape are connected. Ask a gen AI chatbot to evaluate the legend as a form of geographic knowledge: what it encodes, how it is transmitted, and what it can and cannot do that Western scientific geography can and cannot do. Write a critical response to the AI account drawing on the iwi endorsed version of the legend you were introduced to before the visit.
Your annotated viewshed sketch documents the current land use of the Heretaunga Plains. Ask a gen AI chatbot to describe how the Plains have been modified since European settlement and what the major drivers of change have been. Then ask it to project two future scenarios: one in which current land use intensifies, one in which restoration and freshwater management are prioritised. Evaluate the plausibility of each scenario against what you observed in the viewshed.
Choose one observable feature of the Te Mata landscape: the rate of cliff face erosion on the eastern face, the vegetation cover on the limestone ridge, or the extent of native bush in the park. Ask a gen AI chatbot to help you design a repeat monitoring protocol for it. Specify what you would measure, what equipment is needed, how often sampling would occur, and what change in the data would indicate that intervention was needed. Evaluate the protocol for scientific rigour and for its applicability within a park managed under a trust arrangement.
| Level | Years 0–6 | Years 7–10 | Years 11–13 |
|---|---|---|---|
| 1 | Student names the peak as Te Mata o Rongokako, can point to it from the plains, and knows the name comes from a story connected to the shape of the ridge. Identifies at least one feature from their viewshed sketch and can describe what the wind felt like on the ridge compared to the base. | Student names the three curriculum lenses engaged at the site, produces an annotated viewshed sketch with at least four named features, can describe the limestone bedding as evidence of geological process rather than simply as rock, and identifies at least one genuine physical demand the terrain placed on their movement. | Student produces a complete field record: an annotated viewshed sketch with direction and land use noted by quadrant, field notes on the bedding geometry of the limestone at the summit, a Beaufort wind observation, and at least one question per curriculum area opened by the visit that is not answerable from a secondary source alone. |
| 2 | Student links each observation to an explanation: the limestone was once seabed; the wind was stronger on the ridge because of the way the landform shapes airflow; the name Te Mata o Rongokako connects the shape of the ridge to a story told about this specific place. Can explain in simple terms why the ridge looks different when you are standing on it compared to when you are looking at it from Havelock North. | Student explains the tectonic process that produced the limestone ridge, connects the viewshed features to the geomorphic history of the Heretaunga Plains, explains why ridge topography accelerates wind, and articulates what the legend of Te Mata o Rongokako encodes about the relationship between this community and this landscape. | Student constructs a connected account linking the tectonic and geomorphic history of the ridge, the current land use of the Heretaunga Plains as read from the viewshed, the cultural landscape encoded in the legend and in te reo place names visible from the summit, and their own physical experience of the terrain as a record of genuine engagement with the place. |
| 3 | Student compares what a gen AI chatbot said about the legend or the limestone with what they observed or were told at the site. Can say in simple terms where the AI was right, where it was wrong or incomplete, and which answer they trust more for this particular question. | Student documents a comparison between a gen AI chatbot response and an authoritative source (GNS Science for the geology, an iwi endorsed account for the legend) on at least one specific claim from the visit, identifies the nature of any discrepancy, and explains what the discrepancy reveals about how the AI generates its responses. | Student evaluates gen AI responses across at least two of the three curriculum areas against field-collected evidence and named authoritative sources, drawing conclusions about the conditions under which AI output is reliable, where it introduces imprecision without flagging it, and what the implications are for using AI tools in geographic and cultural inquiry. |
| 4 | Student explains in their own words what the visit to Te Mata provided that no classroom resource could: the wind on the ridge, the view of the plains laid out below, the experience of standing on the giant and then seeing the giant from the road. Names one thing they now know that belongs to them because they were there. | Student articulates why field-collected observations from Te Mata (their viewshed sketch, rock notes, wind data) are more valuable for a claim about this specific place than any secondary source: independently collected, location-specific, and time-stamped. Explains why the reversal between standing on the ridge and viewing it from the plains is not available to anyone who has not made both journeys. | Student reflects on what it means to engage with a site that is simultaneously a geological formation, a working landscape readable from a viewshed, a physical terrain that places real demands on movement and judgement, and a wāhi tapu whose meaning is held in a living knowledge system. Articulates what each of those readings requires of a learner who engages with the place in good faith. |
| 5 | Student generates one question they would like to investigate at Te Mata in a different season or from a different vantage point, and can say what they would look for to help answer it. Can name one te reo place name visible from the summit and explain what it means. | Student formulates a testable monitoring question arising from the visit: what they would measure on a return visit, how often sampling would need to occur to detect meaningful change, and what shift in the data would indicate that the condition of the site had changed. The question is specific enough to be acted on, not only discussed. | Student designs a field-based inquiry that could be conducted on a return visit, specifying the research question, data collection method, analysis approach, and intended audience. The design reflects all three curriculum areas present at Te Mata and is grounded in the field record produced during the visit. |