Gotowe bibliografie tematyczne / Banks Peninsula

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Gotowa bibliografia na temat „Banks Peninsula”

Autor: Grafiati

Data publikacji: 4 czerwca 2021

Data aktualizacji: 31 stycznia 2023

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Artykuły w czasopismach na temat "Banks Peninsula"

Garnock-Jones, PJ. "Plant life on Banks Peninsula." New Zealand Journal of Botany 52, no. 3 (July 3, 2014): 386–87. http://dx.doi.org/10.1080/0028825x.2014.885454.

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Slooten, Elisabeth, William Rayment, and Steve Dawson. "Offshore distribution of Hector's dolphins at Banks Peninsula, New Zealand: Is the Banks Peninsula Marine Mammal sanctuary large enough?" New Zealand Journal of Marine and Freshwater Research 40, no. 2 (June 2006): 333–43. http://dx.doi.org/10.1080/00288330.2006.9517425.

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Boren, L. J., C. G. Muller, and N. J. Gemmell. "Colony growth and pup condition of the New Zealand fur seal (Arctocephalus forsteri) on the Kaikoura coastline compared with other east coast colonies." Wildlife Research 33, no. 6 (2006): 497. http://dx.doi.org/10.1071/wr05092.

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Abstract.Since its near extermination by sealing, the New Zealand fur seal (Arctocephalus forsteri) has been recolonising areas of its former range throughout New Zealand and Australia. This study examined fur seal population growth over four breeding seasons spanning 2002–05 at the Ohau Point and Lynch’s Reef colonies in Kaikoura and the Horseshoe Bay and Te Oka Bay colonies on Banks Peninsula, on the east coast of New Zealand. Estimates of pup numbers were made using mark–recapture techniques and condition indices were used to assess the body condition of pups in each colony. We found that t

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Khalil-Oliwa, Oliwia. "Review of Risks and Risk Management Systems in the Largest Islamic Banks of the Arabian Peninsula." Annales Universitatis Mariae Curie-Skłodowska, sectio H – Oeconomia 55, no. 1 (May 11, 2021): 19. http://dx.doi.org/10.17951/h.2021.55.1.19-29.

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Theoretical background: The specificity of Islamic principles, on the basis of which Islamic banking was created, as well as the nature of its financial instruments, means that Islamic banks may be exposed to greater risks than conventional banks.Purpose of the article: The aim of the article is to define key risks identified by Islamic banks and to define risk management systems in the 13 largest banks of the Arabian Peninsula region. The article analyses the annual reports submitted by the supervisory board

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Pharo, Emma, and Bryony H. Macmillan. "Checklist of the Mosses of Banks Peninsula, New Zealand." Bryologist 101, no. 2 (1998): 352. http://dx.doi.org/10.2307/3244213.

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Reynolds‐Fleming, Janelle V., and Jason G. Fleming. "Coastal circulation within the Banks Peninsula region, New Zealand." New Zealand Journal of Marine and Freshwater Research 39, no. 1 (March 2005): 217–25. http://dx.doi.org/10.1080/00288330.2005.9517301.

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Perrie, Leon R., Patrick J. Brownsey, and John D. Lovis. "Tmesipteris horomaka, a new octoploid species from Banks Peninsula." New Zealand Journal of Botany 48, no. 1 (March 2010): 15–29. http://dx.doi.org/10.1080/00288251003640010.

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Wilson, Hugh D. "Regeneration of native forest on Hinewai Reserve, Banks Peninsula." New Zealand Journal of Botany 32, no. 3 (July 1994): 373–83. http://dx.doi.org/10.1080/0028825x.1994.10410480.

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Griffin, Sammy, Travis W. Horton, and Christopher Oze. "Origin of warm springs in Banks Peninsula, New Zealand." Applied Geochemistry 86 (November 2017): 1–12. http://dx.doi.org/10.1016/j.apgeochem.2017.09.013.

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Cameron, Claire, Richard Barker, David Fletcher, Elisabeth Slooten, and Stephen Dawson. "Modelling Survival of Hector's Dolphins around Banks Peninsula, New Zealand." Journal of Agricultural, Biological, and Environmental Statistics 4, no. 2 (June 1999): 126. http://dx.doi.org/10.2307/1400593.

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Rozprawy doktorskie na temat "Banks Peninsula"

Parker, S. K. "The hydrogeology of the Diamond Harbour region, Banks Peninsula." Thesis, University of Canterbury. Geology, 1989. http://hdl.handle.net/10092/5501.

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The study area comprises an area of about 40 km2 and includes the township of Diamond Harbour located on the sourthern side of Lyttelton Harbour. The area is broken up into two valley systems (Orton Bradley and Purau Valleys) separated by a gently northward dipping slope known as the Diamond Harbour ‘Dip-slope’. Pressure on a water reticulation pipeline due for repair or replacement, combined with an increasing population) formed the basis for this investigation. It was hoped that local groundwater resources could at least supplement the domestic supply coming from Lyttelton. Drill hole and g

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Sanders, R. A. "Hydrogeological studies of springs in Akaroa County, Banks Peninsula." Thesis, University of Canterbury. Geology, 1986. http://hdl.handle.net/10092/5504.

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Akaroa County, which is situated on the eroded remnant of the basaltic Akaroa Volcano, is developing as a tourist and recreational area, with consequent increasing demands on water supplies. Improved utilisation of the springwater resource of the area is a possible solution to these demands and this thesis develops hydrogeological models for the springs to assist in their future management. Methods used in this study include detailed hydrogeological mapping of two specific areas, isotope and chemical analyses of springwater, and spring discharge monitoring over a one year period. Groundwater

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Hughes, Terrence Jon. "A detailed study of Banks Peninsula loess shear strength." Thesis, University of Canterbury. Geology, 2002. http://hdl.handle.net/10092/10021.

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This thesis project has examined the moisture dependency of shear strength in the loess soils of Banks Peninsula. These dominant silt materials are generally regarded as having an angle of internal friction between 25 and 30°, and cohesion of zero, when the soil is saturated. However, soil behaviour in terms of slope stability would appear to support a cohesion value higher than zero as vertical cliffs of loess can be seen to stand indefinitely. It is agreed that loess soils upon saturation do show very low shear strengths, but these soils rarely become saturated due to their low permeability

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Smith, Susan Leslie. "Distribution, movements and abundance of Hector's dolphin around Banks Peninsula." Thesis, University of Canterbury. Department of Zoology, 1992. http://hdl.handle.net/10092/2801.

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New Zealand's first Marine Mammal Sanctuary was established around Banks Peninsula in 1988, to protect Hector's dolphins from entanglement in gillnets. Understanding distribution and movements of Hector's dolphins inhabiting Banks Peninsula has important implications for their effective management. The need to assess the effectiveness of restricting gillnetting also underscores the need for ongoing estimates of the size of the Banks Peninsula Hector's dolphin population. I analysed spatial and temporal movements of distinctive Hector's dolphins identified around Banks Peninsula. A substantial

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Nikoloff, Megan Helena. "Seed and microsite limitation in Clematis vitalba on Banks Peninsula." Thesis, University of Canterbury. Biological Sciences, 2011. http://hdl.handle.net/10092/6730.

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Clematis vitalba, introduced to New Zealand from Europe in the early 1900s, is an invasive weed which poses a high risk to native forest remnants, particularly in the central North Island and upper and central South Island. Its dispersal techniques and rate of spread make it a particular challenge for managers attempting to control its range expansion. Is the population abundance and distribution of C. vitalba on Banks Peninsula seed or microsite limited? I tested the presence of seed limitation in three populations of C. vitalba at two sites by measuring seed dispersal and checking for the pr

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Livermore, Andrew B. "Cinder cones of the Lyttelton Volcano, Banks Peninsula, New Zealand." Thesis, University of Canterbury. Geology, 1999. http://hdl.handle.net/10092/6858.

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Cinder cones are common on Banks Peninsula and this study concentrates on eleven sites situated on the Lyttelton Volcano. The study focuses on the structure, petrology and geochemistry of cinder cones and discusses their eruptive history. Lyttelton volcanism began in the Miocene (10.8 Ma) with early (L1) activity centred near "Head of the Bay". Constant replenishment of the main chamber caused L1 lavas to be dominantly basaltic with limited differentiation. The development of a large cone resulted in distension which caused the development of horizontally fed radial dikes. Initial dike activi

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Goldwater, Stefan. "Slope Failure in Loess. A detailed investigation Allandale, Banks Peninsula." Thesis, University of Canterbury. Geology, 1990. http://hdl.handle.net/10092/9378.

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This study investigates a slope failure complex in loess at Allandale, Lyttelton Harbour. Literature relevant to the slope stability and strength of Banks Peninsula loessial soils is reviewed. Laboratory and in situ strength testing shows that both C and P layer loess in a partially saturated state displays a significant reduction in undrained shear strength with increasing degree of saturation. Strength reduction can be attributed to reduced pore water tension due to capillary suction which results from an increased degree of saturation. The moisture controlled strength component in partially

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Hay, Robert Bruce. "Sense of place: Cross-cultural perspectives from Banks Peninsula, New Zealand." Thesis, University of Canterbury. Geography, 1990. http://hdl.handle.net/10092/4704.

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Sense of place is an important dimension in many people's lives. Through long residence in a region a person tends to become attached to that place, expressing both territoriality and affection for it. Bonding to a place is largely subconscious, however. If a person gains perspective by being distant from his or her place, a greater awareness of place bonds can build upon his or her sense of place, making it even stronger. Cultural influences can also build a sense of place, especially among indigenous people. Previous sense of place research has seldom been empirically based, and has tended

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Dorsey, C. J. "The geology and geochemistry of Akaroa volcano, Banks Peninsula, New Zealand." Thesis, University of Canterbury. Geological Sciences, 1988. http://hdl.handle.net/10092/7524.

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This thesis presents a detailed geological, petrological and geochemical study of Akaroa Volcano, Banks Peninsula, New Zealand. The Akaroa Volcanic Group is defined as comprising all the volcanic products of central, flank and parasitic vent eruptions in the south-eastern two-thirds of Banks Peninsula, which collectively form Akaroa Volcano. Field mapping has shown that the lavas and pyroclastics of which Akaroa Volcano is constructed can be grouped into an Early Phase and a Main Phase. Early Phase rocks (?11-9 Ma) are restricted in outcrop to the inner shoreline of Akaroa Harbour. The oldes

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Fraser, Iain. "The effects of forest fragmentation on stream invertebrate communities on Banks Peninsula." Thesis, University of Canterbury. Biological Sciences, 2006. http://hdl.handle.net/10092/1353.

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The removal of indigenous forest and associated fragmentation of habitats has probably had significant impacts on the diversity of stream communities in New Zealand. In this study I investigated the effects of forest fragmentation on stream invertebrate communities on Banks Peninsula. Six catchments were investigated, three with continuous indigenous forest in the riparian zone and three with fragmented indigenous riparian forest. An extensive benthic survey was conducted at three sites in each river catchment, one downstream on the mainstem of the river and two sites in different headwater tr

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Książki na temat "Banks Peninsula"

Boyum, Burton H. The Peninsula Bank, 1887-1987. Ishpeming, Mich: Peninsula Financial Corp., 1987.

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John, Wilson. City and peninsula: The historic places of Christchurch and Banks Peninsula : Ōtautahi and Horomaka. Christchurch, N.Z: Christchurch Civic Trust, 2007.

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Jacomb, Chris. Panau: The archaeology of a Banks Peninsula Māori village. Christchurch, N.Z: Canterbury Museum, 2000.

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Macmillan, B. H. Checklist of the mosses of Banks Peninsula, New Zealand. Lincoln, Canterbury, New Zealand: Manaaki Whenua Press, 1996.

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Office, Great Britain Hydrographic. China Sea pilot: The west side of the South China Sea from Tanjung Lompat on the eastern side of Peninsula Malaysia to Zhelang Jiao in China; Pulau-Pulau Anambas, Hainan Dao, and the islands and banks bordering the main route from Singapore Strait to Hong Kong. 5th ed. Taunton, Somerset: United Kingdom National Hydrographer, 2001.

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Wilson, Hugh. Natural History of Banks Peninsula. Canterbury University Press, 2010.

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Ogilvie, Gordon. Banks Peninsula: Cradle of Canterbury. CP Books, 1990.

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Wilson, Hugh. Natural History of Banks Peninsula. Canterbury University Press, 2021.

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Chetwynd, Jane. Cloud Farm: High on Banks Peninsula. Longacre Press, 2004.

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Land Very Fertile Banks Peninsula In Poetry And Prose. Canterbury University Press, 2009.

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Części książek na temat "Banks Peninsula"

Michiguchi, Yoko, and Yujiro Ogawa. "Dark Bands in the Submarine Nankai Accretionary Prism – Comparisons with Miocene–Pliocene Onshore Examples from Boso Peninsula." In Accretionary Prisms and Convergent Margin Tectonics in the Northwest Pacific Basin, 229–46. Dordrecht: Springer Netherlands, 2011. http://dx.doi.org/10.1007/978-90-481-8885-7_11.

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Kelly, Ashley Scott, and Xiaoxuan Lu. "Northern Scientific Knowledge and Indigenous Knowledge." In Critical Landscape Planning during the Belt and Road Initiative, 193–249. Singapore: Springer Singapore, 2021. http://dx.doi.org/10.1007/978-981-16-4067-4_8.

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AbstractThis chapter features three planning proposals focused on the ideological friction between Northern scientific knowledge and indigenous knowledge. Northern scientific knowledge has enabled and legitimized various territorialization projects since the establishment of the Lao PDR. Over the past decade, the application of such knowledge has diversified and expanded along with Laos’s increasing integration into the socio-economic geography of the China-Indochina Peninsula Economic Corridor. Unlike World Bank-funded green-neoliberal development that dominated Laos in the 1990s and 2000s, some China-funded projects are furthering the green neoliberal valuation of ecosystems in monetary terms and these ecosystems’ conservation by means of market dynamics. These ecosystem territories inevitably overlap with the country’s indigenous territories and their natural resource-dependent communities. The three planning proposals featured in this chapter foreground Laos’s remarkable human diversity and local communities’ valuable traditional ecological knowledge and practices. These planning proposals are situated in a diverse range of socio-ecological contexts, namely Nam Ha National Protected Area, a protected forest in Luang Prabang, and agricultural land within the capital Vientiane. Collectively, these proposals focus on agrarian populations influenced by old or new forms of land enclosure, investigating possible scenarios that may lead to more equal power relationships between the scientific and indigenous knowledge regimes.

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Elisabete Duarte Neves, Maria, Joana Monteiro, and Carmem Leal. "Determinants of Banking Profitability in Portugal and Spain: Evidence with Panel Data." In Banking and Accounting Issues. IntechOpen, 2022. http://dx.doi.org/10.5772/intechopen.103142.

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This article aims to study the determinants of banking performance in the countries of the Iberian Peninsula, Portugal and Spain. To achieve the proposed objective, the methodology of panel data was used, specifically the estimation method Generalized Method of Moments (GMM-system). An unbalanced panel of 267 banks was used, of which 122 belong to the Portuguese banking sector and 145 to the Spanish banking sector. Two variables were used as performance measures, the average return on total assets (ROAA) and the average return on equity (ROAE). The results show that bank profitability is generally influenced by internal variables, and not so much by sector-specific or macroeconomic variables. Therefore, the results suggest that management decisions are the ones that most influence performance. We conclude that bordering countries, despite having different economies, have very similar influences on bank profitability.

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Hughes, G. WyN. "The Great Pearl Bank Barrier of the southern Arabian Gulf- A possible analog for the Aptian rudist banks of the Arabian Peninsula." In Quaternary Deserts and Climatic Change, 565–82. CRC Press, 2020. http://dx.doi.org/10.1201/9781003077862-57.

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Cody, Martin L., and Enriqueta Velarde. "Land Birds." In Island Biogeography in the Sea of Cortés II. Oxford University Press, 2002. http://dx.doi.org/10.1093/oso/9780195133462.003.0016.

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Very few of the early scientific explorers in the Gulf of California had much to say about the land birds. There might be two reasons for this: first, the land birds in arid, desert regions are sparse and in general unbecoming, and second, the species encountered are by and large those seen in the much more accessible regions of southwestern North America. Chapter 1 introduced János Xántus, who is recognized as the pioneer ornithologist (or at least bird collector) in the cape area of Lower California, whose contributions (e.g., 1859, in which the first description of the Gray Thrasher, Toxostoma cinereum, was published) are appropriately commemorated in the Xantus Hummingbird, the most spectacular endemic on the peninsula. Lawrence (1860) first described the species as Amazilia xantusi (thence Hylocharis xantusii, and now Basilinna xantusii), and P. L. Sclater announced the discovery to Ibis readers in the same year. By the end of the nineteenth century, several ornithologists had collected in the southern peninsula and reported their findings (e.g., Baird 1870; Belding 1883; Bryant 1889; Ridgway 1896), but very little of this work referred to the islands in the gulf. Brewster’s (1902) report on the cape region avifauna was the most comprehensive of the earlier studies. Serious attention was first paid to the gulf island birds by Maillard (1923) and Townsend (1923), and the latter’s 1911 island-hopping trip in the Albatross served as a model for many similar expeditions later. The first distributional synthesis of their work, and especially that of Nelson (1921), Lamb (e.g., 1924), and Thayer (e.g., 1907), was published by Joseph Grinnell in 1928 in a monograph that is still the standard reference for the peninsula and gulf area. The last 50 years have seen little progress beyond the accumulation of further distributional records and the description of new subspecies (e.g., van Rossem 1929, 1932; Banks 1963a,b,c, 1964, 1969). The island birds remain rather poorly known; even species lists are likely to be incomplete, and ecological studies of the island populations have scarcely begun. In this chapter we report on the results largely of our own field work.

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Ezcurra, Exequiel, and Luis Bourillón. "Ecological Conservation." In Island Biogeography in the Sea of Cortés II. Oxford University Press, 2002. http://dx.doi.org/10.1093/oso/9780195133462.003.0023.

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In 1973, George Lindsay, one of Baja California’s most eminent botanists, visited the islands of the Sea of Cortés together with Charles Lindbergh, Joseph Wood Krutch, and Kenneth Bechtel. Lindbergh, one of the most celebrated popular heroes of the twentieth century, had become by that time a committed conservationist, interested in the preservation of whales and in the conservation of nature at large. Joseph Wood Krutch, a naturalist, had written The Forgotten Peninsula, one of the first natural history descriptions of Baja California. George Lindsay had helped organize a series of scientific explorations into the Sea of Cortés and the peninsula of Baja California, first from the San Diego Natural History Museum, and later from the California Academy of Sciences (Banks 1962a,b; Lindsay 1962, 1964, 1966, 1970; Wiggins 1962). Kenneth Bechtel, a philanthropist from San Francisco, had given financial support to the Audubon Society in the 1950s and 1960s to study the sea bird rookery at Isla Rasa, which had been decreed a protected area by the Mexican government in 1962. Bechtel was interested in showing the Sea of Cortés to people who might be aroused by its astounding natural beauty and who might help to protect it. For this purpose, he organized the trip and invited Lindbergh to visit the region. The group flew a chartered Catalina flying-boat that allowed them to get to small and remote islands. They landed in the water and then piloted up to the beach so they could have shade under the wing. They visited many of the islands, starting from Consag north of Bahía de los Ángeles, and ending up in Espíritu Santo, east of the Bay of La Paz. It was a wonderful and memorable trip. Two or three months later, both Lindbergh and Lindsay traveled to Mexico City to watch the Mexican premiere of a documentary film on the Sea of Cortés by the California Academy of Sciences that Kenneth Bechtel had sponsored (see chap. 1). Taking advantage of the opportunity, and also of his immense popularity, Charles Lindbergh requested to see the president of Mexico, Luis Echeverría.

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Slater, Jerome. "Peace with Egypt and Jordan." In Mythologies Without End, 171–81. Oxford University Press, 2020. http://dx.doi.org/10.1093/oso/9780190459086.003.0011.

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From 1947 onward, Egypt sought to avoid wars with Israel. Many compromise peace offers were rejected by Israel, mainly because of its expansionist objectives in Egyptian-held territory in the Negev, Gaza, and the Sinai peninsula. Had Israel accepted the Egyptian overtures, almost certainly the 1948, 1956, 1967, and 1973 wars would have been averted. The Egyptian-Israeli peace treaty of 1979, which has held up ever since, was made possible when Israel agreed to withdraw all Egyptian territory it had conquered in the 1967 and 1973 wars. Similarly, from 1947 onward Jordan sought to avoid war with Israel, and after 1967, King Hussein offered to reach a formal peace treaty, provided Israel return the West Bank which it had conquered in the 1967 war. Israel refused, but in the early1990s, Hussein decided to renounce Jordanian sovereignty over the West Bank, resulting in the Israeli-Jordanian peace treaty of 1994.

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Stanislawski, Michael. "8. Nationalism and messianism, 1967–1977." In Zionism: A Very Short Introduction, 81–94. Oxford University Press, 2016. http://dx.doi.org/10.1093/actrade/9780199766048.003.0008.

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The most consequential event in Israel’s history in the second half of the twentieth century was its victory in the Six Day War of June 1967 and its occupation of the West Bank, the Golan Heights, the Gaza Strip, the Sinai Peninsula, and East Jerusalem. “Nationalism and messianism: 1967–1977” outlines the effects of this war and the 1973 Yom Kippur War on Israel and Zionism. Two historic developments were the dilution of the socialist component of Mapai’s labor Zionism in favor of a more centrist economic and social politics and the de-marginalization and embrace of Menachem Begin’s Herut Party as full members of Israel’s political establishment.

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Gerard, Philip. "Wilmington Falls." In The Last Battleground, 292–97. University of North Carolina Press, 2019. http://dx.doi.org/10.5149/northcarolina/9781469649566.003.0041.

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The U.S. Army marches on Wilmington in two wings, one up the eastern peninsula and other up the west bank of the Cape Fear. Ironclad monitors provide artillery support form the river itself. Nine regiments of USCT attack the entrenched line at Sugar Loaf, but cannot breach it. Across the river, local blacks act as scouts, and under their guidance 6,500 troops commanded by Maj. Gen Jacob D. Cox are able to flank the rebel positions at Fort Anderson and Town Creek, forcing an evacuation of the Sugar Loaf position directly across the river as well. On Washington’s Birthday, Wilmington surrenders to US. troops.

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Misbari, S., and M. Hashim. "VARIATION OF LIGHT ATTENUATION OF SEAGRASS HABITAT IN PENINSULAR MALAYSIA FROM SATELLITE-BASED ESTIMATION." In Construction Engineering and Management. PENERBIT UNIVERSITI MALAYSIA PAHANG, 2022. http://dx.doi.org/10.15282/cem.1.04.2022.02.06.

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Light deprivation into the water column depends on the water clarity. Seagrass habitat is sparsely identified along the coastal area of Peninsular Malaysia.Seagrass density is affected by the amount of attenuated light into the water column, as light is essentially used for the growing process. Water along the west coast is more turbid than the south and east coast of Peninsular Malaysia.Blue spectral band (450 nm−510 nm) of Landsat 7 ETM+ satellite image that has strong penetrative power and red band (640 nm−670 nm) that is sensitive to subtle changes on seafloor features are useful to estimate variability of light penetration. A set of sampling points for both spectral bands was plotted with coastal depth.It is found that the east coast has 25% higher light penetration compared to south and west coastal regions. This condition is favourable for seagrass habitat. However, low light in deeper sea bottom and strong waves from South China Sea are among limitations imposed by east coast seagrass meadows to constantly survive.

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Streszczenia konferencji na temat "Banks Peninsula"

Carter, Sarah Dumars. "LATE PLEISTOCENE REWORKED LOESS IN PA BAY, BANKS PENINSULA." In GSA Annual Meeting in Denver, Colorado, USA - 2016. Geological Society of America, 2016. http://dx.doi.org/10.1130/abs/2016am-284503.

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Garofalo, Kathleen Rose, Diego Velasquez, and Samuel J. Hampton. "GEOLOGIC CONTROL ON PLANT BIODIVERSITY IN BANKS PENINSULA, SOUTH ISLAND, NEW ZEALAND." In GSA Annual Meeting in Phoenix, Arizona, USA - 2019. Geological Society of America, 2019. http://dx.doi.org/10.1130/abs/2019am-339299.

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Saux, Juliette, Brooke Carlson, Marlene C. Villeneuve, and Samuel J. Hampton. "PETROPHYSICAL AND MECHANICAL PROPERTIES OF BURIED VOLCANIC ROCKS ON BANKS PENINSULA, NEW ZEALAND." In GSA Annual Meeting in Phoenix, Arizona, USA - 2019. Geological Society of America, 2019. http://dx.doi.org/10.1130/abs/2019am-337834.

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Nellis, Caroline H., Josh W. Borella, Josh W. Borella, and Josh W. Borella. "IDENTIFICATION OF ALLUVIAL FANS PRONE TO DEBRIS-FLOW HAZARD IN NORTHWESTERN BANKS PENINSULA." In GSA Annual Meeting in Phoenix, Arizona, USA - 2019. Geological Society of America, 2019. http://dx.doi.org/10.1130/abs/2019am-338208.

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Rubin, Margaret, Josh Borella, Chris Grimshaw, and Samuel J. Hampton. "PHYTOLITH RECONSTRUCTION OF THE ENVIRONMENT SURROUNDING THE KAWAKAWA TEPHRA IN BANKS PENINSULA, SOUTH ISLAND." In GSA Annual Meeting in Seattle, Washington, USA - 2017. Geological Society of America, 2017. http://dx.doi.org/10.1130/abs/2017am-299111.

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Milando, Lea, Josh W. Borella, and Sharyn Goldstien. "ESTABLISHMENT OF HILLSLOPE FOREST CHARACTERISTICS IN BANKS PENINSULA: IMPLICATIONS FOR ROCKFALL MODELING AND RUNOUT." In GSA Annual Meeting in Indianapolis, Indiana, USA - 2018. Geological Society of America, 2018. http://dx.doi.org/10.1130/abs/2018am-322424.

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Jaffe, Micah, Samuel J. Hampton, and Samuel J. Hampton. "CHANGES IN SEDIMENT SOURCES SINCE EUROPEAN COLONIZATION IN PORT LEVY, BANKS PENINSULA, NEW ZEALAND." In GSA Annual Meeting in Indianapolis, Indiana, USA - 2018. Geological Society of America, 2018. http://dx.doi.org/10.1130/abs/2018am-322438.

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Chandler, Jakob, and Samuel J. Hampton. "ERUPTION, INTRUSION, AND PRESERVATION OF A COASTAL SCORIA CONE: RED BAY, BANKS PENINSULA, NZ." In GSA Annual Meeting in Seattle, Washington, USA - 2017. Geological Society of America, 2017. http://dx.doi.org/10.1130/abs/2017am-301994.

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Pontifex, Trevor Sides, Samuel J. Hampton, and Samuel J. Hampton. "GO WITH THE FLOW: MAPPING RECHARGE ZONES OF PERCHED SPRINGS ON BANKS PENINSULA, NEW ZEALAND." In GSA Annual Meeting in Seattle, Washington, USA - 2017. Geological Society of America, 2017. http://dx.doi.org/10.1130/abs/2017am-297519.

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Wiseman, Matthew B., Josh W. Borella, and Harry M. Jol. "GEOMORPHIC MAPPING AND SUBSURFACE CHARACTERIZATION OF A DEBRIS FLOW COMPLEX IN BANKS PENINSULA, NEW ZEALAND." In GSA Annual Meeting in Phoenix, Arizona, USA - 2019. Geological Society of America, 2019. http://dx.doi.org/10.1130/abs/2019am-335174.

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