6 Human Activity - Mangawhai-Pakiri Flashcards

1
Q

Background

A
  • Both beaches located on New Zealand’s North Island
  • Pacific coast of Northlands Peninsula, 50km north of Auckland
  • Sand high quality and suitable for the construction industry
  • Haukari Gulf is site of the biggest seabed mining operations in NW waters
  • Rules on seabed mining less restrictive eg illegal in UK to extract landward of the 19m depth or within 600m of shore
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2
Q

Need for sand: What is sand an essential mineral source for?

A

Construction, concrete, glass manufacture, beach replenishment

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3
Q

Need for sand: How much is the sand sold for?

A

approv NZ$50/m3, or which the NZ government takes NZ$1.70/m3 in royalties

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4
Q

Need for sand: What was announced in the 2016 Unitary Plan?

A

In the 2016 Unitary Plan, Auckland City Council announced plans to build 422000 extra houses over the next 25 year - same number built over the previous 160 years
Needs 2.5x greater construction rate than achieved in the previous 25 years

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5
Q

Need for sand: How much did Auckland’s population increase by?

A

1995-2016
Increased by 20000/year - fastest ever period of growth

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6
Q

Need for sand: How much did Auckland’s GDP grow by?

A

2000-2018
NZ$52 billion to NZ$93 billion

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7
Q

Need for sand: What has the sand mined from Mangawhai-Pakiri used for?

A

Replenishing Auckland’s tourist beaches (Mission Bay, Kohimarama and St Heliers)

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8
Q

Need for sand: What is Aucklands and what is its significance?

A
  • New Zealand’s largest urban area (pop 1.5 million - 1/3 of the population)
  • Accounts for 37% of GDP and 35% of its workforce
  • 235% larger than the next largest urban area (Wellington)
  • Home to thriving financial and high tech industries as well as tourism, centred around the outstanding coastal amenities
  • 2015, 2.3million foreign visitors
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9
Q

Offshore sand mining/sediment budget: What system could the coastal sediment budget be classed as?

A

Essentially a closed system
Outputs from sand mining exceed the inputs from rivers and offshore sources by a factor 5

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10
Q

Offshore sand mining/sediment budget: How long has the nearshore sand dredging been occurring?

A
  • On the 20km coastline between Mangawhai and Pakiri beaches has been taking place for over 70 years
  • Between 1994 and 2004, 165000m3/year was extracted using suction dredging from water 5-20m deep
  • Extraction at Mangawhai ended in 2005, but continues at Pakiri at rates of 76000m3/year
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11
Q

Offshore sand mining/sediment budget: What did the NZ’s Environment Court grant in 2006?

A

2 extraction permits for Pakiri, lasting until 2020, despite strong opposition on environmental grounds from Auckland Regional Council and Friends of Pakiri

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12
Q

Offshore sand mining/sediment budget: Why is there little fluvial sediment input and what does this mean?

A

Few sizeable rivers
With input<outputs, the effect of mining is to deplete the sand stores (dunes, beaches and sea bed up to 2km offshore)

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13
Q

Offshore sand mining/sediment budget: Where does the beach and nearshore sediment at Mangawhai-Pakiri originate from?

A

Dates from the last 9000 years (the Holocene)
Pushed up from offshore sources by rising sea levels (the Flandrian Transgression) was Warth’s climate warmed in the late Pleistocene/early Holocene
This process and sediment input ended c.6000BP, when sea levels stabilised

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14
Q

Offshore sand mining/sediment budget: Where does the Holocene sand lie?

A

6-10m deep in the dunes at the back of the beaches, 2-6m deep on the beach and only 0.3m deep in the offshore zone
Underlain by older Pleistocene sand, but this is of less value due to iron impurities

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15
Q

Offshore sand mining/sediment budget: Why is the sand extraction unsustainable?

A

Sand is non-renewable resource along this coastline and extraction at current rates is unsustainable

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16
Q

Offshore sand mining/sediment budget: Why is the rate of erosion increasing along the beaches and dunes?

A

The deeper water created by dredging allows higher energy waves to approach the shoreline

17
Q

Impact on coastal landforms: What is the impact on beaches?

A

Beaches starved of sediment. come wider and flatter and are less effective at absorbing wave energy

18
Q

Impact on coastal landforms: Why is there more erosion of landforms?

A

Higher energy waves can erode landforms such as dunes and spits

19
Q

Impact on coastal landforms: What is the prediction for erosion rates?

A

ARC predict rates will increase due to declining natural protection, eustatic sea level rise and more frequent storm events

By 2100, 35m of retreat along the Mangawhai-Pakiri coastline is expected, vulnerable to erosion between 48-111m. Higher than any of the other Auckland regions other 123 beaches

20
Q

Impact on coastal landforms: How has dredging and groin construction been used to restore some equilibrium?

A

In 1978, storms caused a 28m breach at the base of Mangawhai spit
Altering tidal currents and increased sedimentation in Mangawhai Harbour
Shallower water in the harbour –>threat to boat navigation and seafront properties with flooding
Restored some equilibrium after this

21
Q

Impact on coastal landforms: What is undercut by wave action and what does this lead to?

A

Foredone ridge
Creates steep seaward-facing scarps and loss of vegetation cover makes them vulnerable to wind erosion

22
Q

Other impacts: What is the impact on fisheries?

A

Reduction in quality of local surf and harmful impact on fisheries