玛瑙
发表于 2025-3-23 10:44:04
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湿润
发表于 2025-3-23 13:51:29
The Relationship between Wave Incidence, Wind Direction and Beach Changes at Marsden Bay, County Dufile during part of the period at two selected points and were used to correlate beach changes with variations of wind force and direction, wave characteristics and other relevant data. The paper is presented in four parts:
aesthetic
发表于 2025-3-23 20:03:08
Book 1971This volume is a collection of papers, preceded by an introductory essay, on coastal physiography.
Abutment
发表于 2025-3-24 00:07:51
https://doi.org/10.1007/978-1-349-15422-7Coast; development; geography; physical geography
摇晃
发表于 2025-3-24 02:47:25
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habitat
发表于 2025-3-24 06:31:21
978-0-333-11041-6Palgrave Macmillan, a division of Macmillan Publishers Limited 1971
SEEK
发表于 2025-3-24 11:52:18
Overview: This volume is a collection of papers, preceded by an introductory essay, on coastal physiography.978-0-333-11041-6978-1-349-15422-7
filicide
发表于 2025-3-24 15:43:00
The Main Post-glacial Raised Shoreline of Western Scotland from the Firth of Lorne to Loch Broom,ir height variation throughout the area is of interest, therefore, not only in relation to the particular problems of the isostatic readjustment of formerly glaciated regions and the associated eustatic changes in sea-level, but also as a contribution to the understanding of the development of the coastal landforms of the area in question.
轻触
发表于 2025-3-24 19:15:00
Trend-Surface Mapping of Raised Shorelines,: the shorelines are depicted by lines or zones on the diagram, which in some cases are calculated best-fit regression lines to the series of points representing a given shoreline; in other cases they have been fitted by eye.
Grievance
发表于 2025-3-25 02:28:31
The Influence of Rock Structures on Coastline and Cliff Development around Tintagel, North Cornwall local geological structure. The southern stretch of the coast is sub-parallel to seaward-dipping normal faults which have been stripped of their hanging walls. Such a cliff-line is dominantly a fault-line scarp which has suffered slight retrogression.