.Literature review of Porirua Harbour and catchmentAppendix 2: Annotated BibliographyKingsbury, P. G. (1990). Ponyun Calch"teni Landslip Hazard Assessi, lent. Porirwo Piloi SIMdy.Technical Report LR1990/3. Land Resources Department, <strong>Welling<strong>to</strong>n</strong> Regional CouncilDescribes and maps landslip hazard for the POTirua catchmentlandforms including fieldmapping of currentlandslips and seepage. Indicates potential problems in the catchmentif future urban development occurs within a high landslip hazard classLearny, M. L. (1958). PIGis<strong>to</strong>cene shorelines at Portrua Harbour, near <strong>Welling<strong>to</strong>n</strong>, New Zealand.New ZealandJournalofGeology und Geop/?ysics I: 95-102A basic description of some of the Qualernary terraces at POTirua. Interprets terraces asmarine interglacial deposits, and attempts <strong>to</strong> correlate them with terraces describedglobalIy. Refutes Adkins (1921) evidence of a coseismic uplift in POTirua caused by the1855 earthquakeMCFadgen, B. G. (1980). Maori PIaggen Soils in New Zealand; their origin and properties.Journal o11he Royalsocieiy QINew Zealand 70: 3-9Describes the prehis<strong>to</strong>ric cultivated soils (Maori PIaggen soils) containing sand/graveltransported by inari for agriculture. Describes a PIaggen soil at Pauatahanui from ~440BP at Police PointMildenhall, D. C. (1993). Last glacialion/postglacial pollen record for POTirua, near <strong>Welling<strong>to</strong>n</strong>,New Zealand. runmra 32: 22-27Pollen record taken from exposed diggings at present site of K-Mart in POTirua. Pollendiagram gives indication of vegetation species assemblages from 21,000 BP <strong>to</strong> presentIn the glacial period the area was a swamp with moving fresh water, gradually silling anddrying, until around 9,500BP when pollen assemblages changed indicating a climaticchange <strong>to</strong> moister, warmer conditionsNorthey, R. (1974). Soils o1 Ihe PawuiahunuiArea, Welling10n, New Zealand. New Zealand SoilBureau, DSU^., Scientific Report 13.Report was part of a 1970 study on microzoning for earthquake effects in Panatahanuiarea. Report on soils updated <strong>to</strong> assist in <strong>to</strong>wn planning of area considered for urbandevelopment.Pillans, B. , M. MCGlone, A. Palmer, D. Mildenhall, B. Alloway and G. Berger (1993). The lastglacial maximum in central and southern North Island, New Zealand: a paleoenvironmentalreconstruction using the Kawakawa Tephra Formation as a chronostratigraphic marker.Palueogeography, Primeoc!line<strong>to</strong>logy, Po!aeoec0!o8y 101(3-4): 283-304Study of Kawakawa tephra, its distribution and occurrence in depositional sedimentsPollen analysis at sites which contain this <strong>to</strong>phra, which occurred ~22.6 thousand yearsago, are used <strong>to</strong> interpret climate and vegetation distributions. A site at POTirua isincluded.Quennell, A. (1938). PITysiography und Laie SII'MCIwrul/n^lory o11he urea drained by Ihe PonyuuSired1713/10wing 11/10 Porii'uu Horbo!, r near Well^^g!on, New Zeniund. , Unpublished Msc thesis,Vic<strong>to</strong>ria University of <strong>Welling<strong>to</strong>n</strong>A geographical and nthological description of POTirua, summarising early geologicalstudies and interpreting the landscape using brosion cycle' explanations for geography (aschool of thought which has since been abandoned). Large collection of original pho<strong>to</strong>sfrom the period. Black and white shots of PIimmer<strong>to</strong>n, Pauatahanui, Judgeford, Maria,Whineria, Tawa and POTirua Valley. Shots of inlet and of catchments. All pho<strong>to</strong>s show aReportfor Porirua City Council & <strong>Welling<strong>to</strong>n</strong> City CouncilBlaschke and Rutherford Environmental ConsultantsFebruary 20108
Literature review of Porirua Harbour and catchmentAppendix 2: Annotated Bibliographycompletely denuded landscape, only trees obvious are lone conifers. Evidence of bankerosion and creep erosionSuneson, N. H. (1993). The geology of the Torlesse Complex along the <strong>Welling<strong>to</strong>n</strong> area coast,North Island, New Zealand. New Z, a<strong>to</strong>lld Journal of Geology and Geophysics 36(3): 369-384Describes the geology between Paekakariki and Pencarrow Head focusing on the lateTriassic Torlesse Terrane strata. This basement rock of greywacke and argillite weredeposited as turbidites, strike NNE and dip steeply and face west. Maps major folds,faults and characteristics. Reconstructs deposition and folding and faulting events basedon described characteristicsWebby, B. D. (1958). The geology of Poriru" districi. Unpublished Msc. thesis, GeologyDepartment. <strong>Welling<strong>to</strong>n</strong>, Vic<strong>to</strong>ria University.Very detailed geological description of the POTirua area. Includes rock types andfeatures, discussion of how the greywacke (turbidites) formed as deep sea depositsDetailed description of folding and faulting. Described the PIGis<strong>to</strong>cene and Holocenedeposits and terracesWilliams, D. N. (1975). 0hariu fault zone at POTirua Harbour, <strong>Welling<strong>to</strong>n</strong>, New Zealand. NewZealand JournnlofGeology und Geop/?ysics 18. . 659- 665Geological description of the Ohariu fault zone. At Porirua, the Ohariu fault splits in<strong>to</strong> awide fault zone (~ 500 in wide) that passes through POTirua and aligns with each side ofthe Oriono<strong>to</strong> ArmTerrestrial biodiversity and catchmentland useBagnall. R. G. (1979). A study of human impact on an urban forest remnant: Redwood Bush,Tawa, near <strong>Welling<strong>to</strong>n</strong>, New Zealand. New Zealand lorryridl of Boloiiy 17. . 1/7-26Study of the impact of human activity on a 9.3 ha stand of kohekohe-lawa forest at Tawa(Redwood Bush). Documents rapid rate of loss of forest area and shift from kohekohetawaco-dominance <strong>to</strong> kohekohe dominance, resulting from fragmentation and edgeeffects associated with residential development, and damage associated with uncontrolledrecreational useBML (2001). 111venioiy of ecological sires ill Folly!Ia City. Boffa Miskell Ltd, prepared forPOTirua City CouncilExtensive ecological survey of whole of POTirua City (extends beyond the catchment ofPorirua Harbour). Surveys and assesses ecological areas in terms of species rarity andrepresentation in the Forirua area. Flora and fauna of each site is documented. Classifiesthe region in<strong>to</strong> four ecodomains, which are mapped and the climate, soils vegetation andcanopy structure of each domain described. Outlines threats and obstacles <strong>to</strong> retainingand enhancing vegetation in each domain, and ranks each ecological area in terms ofmanagement priority. Appendix of flora and fauna speciesBML and WRC (1999) Welling10/1 Regional Norive PIuni Guide. Boffa Miskell and <strong>Welling<strong>to</strong>n</strong>Regional Council. <strong>Welling<strong>to</strong>n</strong>, <strong>Welling<strong>to</strong>n</strong> Regional Council.ECodomain framework and recommended native plantlisls for the Welling10n Region.Report for Porirua City Council & <strong>Welling<strong>to</strong>n</strong> City CouncilBlaschke and Rutherford Environmental ConsultantsFebruary 20109
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