Skip to content

Boulder Bank (Earthcache) EarthCache

Hidden : 12/19/2008
Difficulty:
1 out of 5
Terrain:
1.5 out of 5

Size: Size:   not chosen (not chosen)

Join now to view geocache location details. It's free!

Watch

How Geocaching Works

Please note Use of geocaching.com services is subject to the terms and conditions in our disclaimer.

Geocache Description:

This cache will take you to a geological feature which is world-renowned.


View towards Mackay Bluff (the source) from the lighthouse.
 

 

Geology

The Boulder Bank is a natural reef made of granodiorite (an intrusive igneous rock similar to granite), more specifically: cable granodiorite, and through continuous action by the sea’s waves are shaped into smooth boulders, the largest being about 1.2m in diameter, and in average around 20cm. The sea continually hitting this natural barrier slams the boulders together, further shaping this bank which has produced a natural harbour for Nelson (Nelson Haven). The Boulder Bank is the largest natural reef in the Southern Hemisphere. The rocks in the bank are thought to have come – by most researchers - from the Mackay Bluff and Peppin Island at the Northern end over a period of approximately 6000 years. A minority of scientists, such as Dr Warren Dickson at Victoria School of Geography, Environment and Earth Sciences propose that the wave action isn’t sufficient to account for the movement of rocks from the point of erosion at Mackay Bluff along the bank, and suggests the rocks may be eroded from the nearby sea floor. The Bank is approximately 6m above mean sea level and stretches for 13km from Mackay Bluff in the North to The Cut in the South. The Cut is a man-made entry through the bank into Nelson Haven, which is 50m wide at low tide. During the ice ages 12,000 years ago the Tasman Bay seabed was dry. Rocks falling off Mackay Bluff, part of the Flaxmore Fault, collected in a fan below it. When the ice melted 9,000 years ago the sea level rose steadily and eroded the boulders out of the fan. The boulders and associated debris were carried South forming the Bank - a process that continues to this day. The top of the Bank is migrating Eastward leaving a succession of ridges behind it.

 

Ecology 

Despite its robust appearance, the Boulder bank is a delicately balanced habitat for rare species of plants and animals. In addition, it is a nesting place for colonies of gulls, and a resting place for seals and dozens of species of coastal migratory birds including the Variable and South Island Oyster Catchers. At least once every few years, the Boulder Bank is the final resting place for a whale, dolphin, squid or other sea creature which automatically become a source of further research.


Access

The coordinates of this Earth Cache take you close to the source of the Boulder Bank near Mackay Bluff and an information sign that holds the answer to the logging question. From this point you have immediate access to the Boulder Bank, and if you want, quite a long walk along the length of it to the lighthouse (13km) which is the 2nd oldest permanent lighthouse in New Zealand (after Wellington’s Pencarrow Lighthouse). The Bank at this stage is still part of the mainland. Alternatively, make your way to S 41° 13.023 E 173° 19.802 and take Boulder Bank Drive to S 41° 12.184 E 173° 19.401, where you can park and access the Boulder Bank also. From here the walk to the lighthouse is approximately 2-3 hours one-way (8km), and it is also where the Boulder Bank spit starts, which encloses Nelson Haven. You can also access the Southern end of the Boulder Bank by kayak or boat. A ferry service is available which can take you to the Boulder Bank and Haulashore Island at times, duration and in a sequence you yourself request. (Contact: Haulashore island Ferry, Wakefield Quay, Ph 027 437 5259 – fee payable). Using this ferry service also gets you access to a key which allows you to enter the light house (December 2008).

 

History

The Boulder bank has a natural opening at its Southern end, near Arrow (Fifeshire) Rock. This opening is quite narrow and, as can be seen at low tide, has sharp rock jutting from the sea floor making this entry into Nelson harbour quite treacherous. Countless vessels were damaged here. So in 1906, a new entrance to Nelson Haven was blasted into the Boulder Bank, producing two new distinct features: The Cut (the entrance) and Haulashore Island, which used to be the Southern-most tip of the Boulder Bank. The shelter offered by the Boulder Bank was a major factor in choosing the site of Nelson. In 1848 a beacon was erected near the end of the bank. Across The Cut from Haulashore Island you find the white iconic cast iron lighthouse that replaced the beacon. It was originally established in 1862, automated in 1915, and operated as recently as 1982. Only the grounds around the lighthouse are accessible to the public, although the lighthouse is accessible by arrangement with Port Nelson Ltd. During the Second World War, in 1942, the lighthouse light was extinguished due to the perceived threat of a Japanese invasion. The light was re-established in May 1943. There are six permanent batches (cribs/shanty holiday homes) on the Boulder Bank. Controversy ensues each time the (Government) Department of Conservation (DOC) suggests they should be removed to return the Bank to its “natural state”, but to locals, their presence is as natural as the Bank itself, and thus far DOC has failed to achieve their aim of returning that part of the Boulder Bank to its natural state. The Cut is periodically dredged as sand and and boulders continue to build up.

Logging requirements

DO NOT LOG THIS CACHE UNTIL YOU RECEIVE APPROVAL BY EMAIL. Send an email to geocachingnz.@ .gmail.com with the following information: name the process that has created the Boulder Bank. Also email a photo of yourself holding your GPSr and the Bank clearly visible behind you.

 

Further information

Nelson Boulder Bank, New Zealand
M. R. Johnston
New Zealand Journal of Geology and Geophysics, 2001, Vol. 44: pp79-88
Available as a PDF from here: http://www.rsnz.org/publish/nzjgg/2001/8.php

Owners Value Ageing Harbour Icons
NZ Historic Places Trust,
Summer 2003 issue
Available online from here: http://www.historic.org.nz/magazinefeatures/2003summer/2003_summer_boulderbank.htm

Art. XXVI.—On the Nelson Boulder Bank.
W. F. Worley.
Transactions and Proceedings of the Royal Society of New Zealand, 1899, Vol 32: pp221-225
[Read before the Nelson Philosophical Society, 13th November, 1899.]
Available as a PDF from here: http://rsnz.natlib.govt.nz/volume/rsnz_32/rsnz_32_00_003640.htm

The Historic Places Trust Register
Boulder Bank Lighthouse
Register Number: 41
Registration Type: Historic Place - Category I
Date Registered: 23/06/83
http://www.historic.org.nz/Register/ListingDetail.asp?RID=41&sm=

 

 

Maori history

(Entry below provided by isis58 in her log. Asked and received permission to make it part of the permanent cache page so when the log no longer appears on the cache page, this valuable and interesting information is retained for others to read.) - "This [earth cache] has a very long cache description but three other important viewpoints about the process on how the Boulder Bank was formed have been overlooked. First is how Kereopa who was being persued by Kupe, after kidnapping one of his daughters, offered karakia (incantation, prayer, blessing, ritual chant) which caused the boulders at Horoirangi (Mackay's Bluff) to begin to move and form a barrier, so no matter how hard Kupe's crew paddled the Boulder Bank also grew and in the end they abandoned their chase. Another is about Tu Ariki who put a strange looking fish called Tutaeporoporo (which turned out to be a taniwha (monster)) into a deep pool at Whakatu (Nelson). As it grew from his daily feedings it enlarged the pool and moved the rocks and boulders and created the Haven and the Boulder Bank - the legend continues but isn't so relevant to this cache. The other claim is the Chief Te Maia, a tohunga (skilled person, chosen expert, priest), arrived and could find no safe place to anchor his canoe so walked up to the port hills and performed certain rites and said karakia to give the bay a harbour. He then went home to the north and when he and his hapu (subtribe) returned they entered, past the rock into what they considered the perfect harbour. Each of the 4 [descriptions] has a plausible explanation given your point of view." Citation: Hilary and John Mitchell - Te Tau Ihu o Te Waka

Contemporary events

To many people, the Boulder Bank is just a ridge of boulders that lies there, and nothing much is going on. This is somewhat deceiving.

Restoration work is currently underway to return the lighthouse to operating condition. A special bulb is being sourced and soon Nelson’s naval sentinel will be back in operation. (December 2008)

A privately owned research company, the Cawthron Institute, has gained permission (Resource Consent) to build a direct road to the Boulder Bank (September 2008) to gain access to their Glenhaven aquaculture site at the Northern end. Cawthron had originally intended to build a road adjacent to the Boulder Bank but failed to gain resource consent after concerns were raised about possible environmental and landscape damage.

Just before Christmas 2007, a man in a kayak, who was quite drunk at the time, climbed Arrow (Fifeshire) Rock to remove the lone wild native Cabbage Tree (Cordyline australis/ Ti kouka) as a prank. This caused two quite separate responses. One was some legal hand wringing as to who exactly has legal ownership of the Southern-most feature off the Boulder Bank, and would therefore be the entity to lay a complaint against the trespasser. All that was established was who was not the owner, including Nelson City Council, the Harbour Board, and the Department of Conservation. Before this administrative matter could be settled, the significant public outcry against the prankster was so severe, that with genuine remorse (and by now quite sober) “the tree butcher” had returned to plant a replacement Cabbage Tree on the rock. The public were concerned that the domestically cultivated tree would not withstand the exposed conditions, but one year later, it seems to be flourishing.

Additional Hints (No hints available.)