Zobrazeno 1 - 10
of 141
pro vyhledávání: '"R M Kirk"'
Publikováno v:
Geomorphology. 344:1-9
Using micro-erosion meters (MEM) and traversing micro-erosion meters (TMEM), surface lowering rates of shore platforms on Kaikōura Peninsula, South Island, New Zealand have been measured over a total of 43 years. This record is the longest monitored
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::1aea171fc21025728fb57213736370f5
https://doi.org/10.1016/j.geomorph.2019.07.012
https://doi.org/10.1016/j.geomorph.2019.07.012
Publikováno v:
Geomorphology. 121:266-273
Using long-term data sets of erosion rates for the shore platform at Kaikoura it is possible to assess the relationships between erosion rates over two and ten years. Erosion rates do not tend to vary significantly between the two measurement periods
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::c03d9d379dde6647a72332d4ccc80951
https://doi.org/10.1016/j.geomorph.2010.04.023
https://doi.org/10.1016/j.geomorph.2010.04.023
Publikováno v:
Geomorphology. 114:22-29
Knowledge of the long-term rates of erosion of shore platforms are needed to assist modeling platform development, understand rates and modes of development and decipher issues of inheritance from former sea level. Few studies report rates from more
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::2a97280a86fea83f3a9839af52c9725d
https://doi.org/10.1016/j.geomorph.2008.10.013
https://doi.org/10.1016/j.geomorph.2008.10.013
Geography in the ‘Real World’: Coastal Management and the Role of the Geographer in Landuse Planning
Autor:
R. M. Kirk
Publikováno v:
New Zealand Journal of Geography. 93:6-11
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::3f58f1138d741848202046781a132596
https://doi.org/10.1111/j.0028-8292.1992.tb00305.x
https://doi.org/10.1111/j.0028-8292.1992.tb00305.x
Publikováno v:
Earth Surface Processes and Landforms. 27:207-220
This paper examines the morphology and processes governing the development of shore platforms at Lake Waikaremoana, North Island, New Zealand. Shore platforms at Lake Waikaremoana are recent features, and were formed when a new sequence of shoreline
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::ef65d1fe0e7e0cbc5700397abb1e373d
https://doi.org/10.1002/esp.315
https://doi.org/10.1002/esp.315
Autor:
R. M. Kirk
Publikováno v:
Journal of Anatomy. 199:625-628
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::288604ca9ac2c037908964aa6eecc7c5
https://doi.org/10.1046/j.1469-7580.2001.199506252.x
https://doi.org/10.1046/j.1469-7580.2001.199506252.x
Autor:
R. M. Kirk, Wayne J. Stephenson
Publikováno v:
Geomorphology. 41:5-21
This paper reports the occurrence of swelling of coastal bedrock measured with a traversing micro-erosion meter (TMEM) on inter-tidal mudstone and limestone shore platforms. While numerous micro-erosion meter (MEM) studies have been made, only a smal
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::988f2a7c10ca7042fd9c635f011b788c
https://doi.org/10.1016/s0169-555x(01)00100-3
https://doi.org/10.1016/s0169-555x(01)00100-3
Autor:
R. M. Kirk
Publikováno v:
Journal of Anatomy. 199:369-372
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::ddbfd164e21a0100978e216d3cd7e1e5
https://doi.org/10.1046/j.1469-7580.2001.199303693.x
https://doi.org/10.1046/j.1469-7580.2001.199303693.x
Autor:
R. M. Kirk, Wayne J. Stephenson
Publikováno v:
Geomorphology. 32:21-41
The role of waves in shore platform development has been investigated on Kaikoura Peninsula by direct measurement of waves in deep water and on platforms at high tide. This showed that the deepwater wave environment off the Kaikoura Peninsula is very
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::22ce0fe1d8a939834c08ca6706003340
https://doi.org/10.1016/s0169-555x(99)00061-6
https://doi.org/10.1016/s0169-555x(99)00061-6