“In the bay in which we landed, we found two or three miserable primitive Maori cabins, inhabited by half-a-dozen helpless old creatures and a few diseased children — forming a pa named Rapaki.”…
Beach ridge stratigraphy can provide an important record of both sustained coastal progradation and responses to events such as extreme storms, as well as evidence of earthquake induced sediment pulses. This study is a stratigraphic investigation of the late Holocene mixed sand gravel (MSG) beach ridge plain on the Canterbury coast, New Zealand. The subsurface was imaged along a 370 m shore-normal transect using 100 and 200 MHz ground penetrating radar (GPR) antennae, and cored to sample sediment textures. Results show that, seaward of a back-barrier lagoon, the Pegasus Bay beach ridge plain prograded almost uniformly, under conditions of relatively stable sea level. Nearshore sediment supply appears to have created a sustained sediment surplus, perhaps as a result of post-seismic sediment pulses, resulting in a flat, morphologically featureless beach ridge plain. Evidence of a high magnitude storm provides an exception, with an estimated event return period in excess of 100 years. Evidence from the GPR sequence combined with modern process observations from MSG beaches indicates that a paleo storm initially created a washover fan into the back-barrier lagoon, with a large amount of sediment simultaneously moved off the beach face into the nearshore. This erosion event resulted in a topographic depression still evident today. In the subsequent recovery period, sediment was reworked by swash onto the beach as a sequence of berm deposit laminations, creating an elevated beach ridge that also has a modern-day topographic signature. As sediment supply returned to normal, and under conditions of falling sea level, a beach ridge progradation sequence accumulated seaward of the storm feature out to the modern-day beach as a large flat, uniform progradation plain. This study highlights the importance of extreme storm events and earthquake pulses on MSG coastlines in triggering high volume beach ridge formation during the subsequent recovery period.
KIRITAPU ALLAN to the Minister of Finance: What recent reports has he seen on the New Zealand economy? Hon PAULA BENNETT to the Prime Minister: Does she stand by all her Government’s statements, policies, and actions? Hon AMY ADAMS to the Minister of Finance: Does he stand by all of the Government’s decisions, statements, and actions in relation to his portfolio? Hon RUTH DYSON to the Minister for Courts: What recent announcements has he made about settling long-standing insurance disputes following the Canterbury earthquakes? Hon JUDITH COLLINS to the Minister of Housing and Urban Development: Is the KiwiBuild programme delivering good value for money for New Zealand taxpayers? Hon PAUL GOLDSMITH to the Minister of Transport: Does he stand by all his statements, policies, and actions? GINNY ANDERSEN to the Minister of Police: What recent announcements has he made about the firearms buy-back scheme? Hon MICHAEL WOODHOUSE to the Minister of Health: How is the wellbeing of cancer patients in New Zealand affected by the Government’s policies and actions in health? TAMATI COFFEY to the Minister for Whānau Ora: What recent announcements has he made about Whānau Ora? MARK PATTERSON to the Minister of Internal Affairs: What recent announcement has she made regarding recognition of Fire and Emergency New Zealand volunteers? Hon NIKKI KAYE to the Associate Minister of Education: How many of the 600 learning support coordinators she promised does she estimate will be working in schools by the beginning of term 1 of the 2020 school year? ANDREW BAYLY to the Minister of Revenue: What concerns, if any, does he have regarding the operation of the latest phased rollout of the IRD Business Transformation Programme, especially in relation to KiwiSaver PIE tax arrangements?