Lake Disappear

BY BRUCE HAYWARD (GEOLOGIST)
Accessibility: EASY
Lake Disappear viewed from Kawhia Rd.
Possibly the longest/largest polje lake in New Zealand. Polje is a flat-floored valley surrounded by limestone with no surface stream outlet.
Large sinkhole in limestone on west side of Kawhia Rd, opposite Lake Disappear.
Lake Disappear is in the valley of Pakihi Stream. This valley was dammed by a basalt lava flow in the Early Quaternary, about 2 million years ago. Kawhia Rd runs along on top of this flow which forms a natural dam. At the eastern side of the lava flow the stream flows into a limestone sinkhole and flows underground for about 2 km before re-emerging and flowing down into Aotea Harbour. After the lava flow was emplaced, the stream found a new route through an underground cave. After heavy rain the cave system is not large enough to carry all the water and a lake forms extending for 2 km or more back up the valley. In dryer weather the lake drains away completely.
Lake Disappear
If you stop and look up the valley, is the lake present or absent during your visit?
How do you think the underground cave through limestone was formed?
Across the road just west of some farm buildings there is a large funnel shaped hole in the ground - how do you think it formed and why is it not full of water?
Directions/Advisory

From Hamilton-Raglan highway, take signposted route to Bridal Veil Falls (Te Mata Rd then Kawhia Rd) and views of Lake Disappear are on the east (left) about 2.5 km south of Bridal Veil Falls.

Beware of traffic although this is not a main road. Find somewhere wide and safe to pull off the road.

Google Directions

Click here for Google driving directions

Accessibility: EASY

View from side of road. Best seen by getting out of car and walking to look over fence across farmland.

Features
Sedimentary Landform
Geological Age
Oligocene rocks, Quaternary aged landform.
Zealandia Evolution Sequence
Pākihi Supergoup: 5 million years ago – present