Seafloor Mapping of the Atlantic Ocean by GMT


Book Description

The study presents the insights of the tectonic development and geological settings of the Atlantic Ocean supported by cartographic visualization in Generic Mapping Tools (GMT). The aim is to study geologic situation and trends in the tectonic development of the Mid-Atlantic Ridge and Atlantic Ocean seafloor. The objective is to find out impact of various factors (such as volcanic, tectonic, hydrothermal and sedimentary processes) that sculpt seafloor geomorphology, and correlation between early history of crust formation, geological processes and present submarine landforms. Other assignments in this work refer to mutual comparison of raster grids on sedimentation, topography, geology, seafloor fabric and highlighting similarities among the landforms and sediment thickness. Asymmetry in crustal accretion is explained by the tectonic history of the lithosphere formation. Correlation between plate subduction and development of the submarine landforms is explained by the Earth's crust extension resulting in formation of cracks, elongations, faults, rifts. Ocean seafloor geomorphology is shaped by a variety of factors that impact its form at different scales. These drivers (tectonic evolution, oceanic currents, hydrology, sedimentation) have effects on geomorphic landforms of the seafloor in context of historic geological development and during Quaternary. Technical part of this work was performed by GMT scripting toolset with all maps plotted in American polyconic projection. The results are received by overlay, cartographic analysis and synthesis of the multi-source geodata through mapping and interpreting grids (ETOPO1, EGM96, GlobSed, crustal age). This work contributes to expand the knowledge on geological and tectonic development of the Atlantic Ocean seabed in order to complete the view of its submarine geomorphology.










Regional Geology and Tectonics: Principles of Geologic Analysis


Book Description

Regional Geology and Tectonics: Principles of Geologic Analysis, 2nd edition is the first in a three-volume series covering Phanerozoic regional geology and tectonics. The new edition provides updates to the first edition’s detailed overview of geologic processes, and includes new sections on plate tectonics, petroleum systems, and new methods of geological analysis. This book provides both professionals and students with the basic principles necessary to grasp the conceptual approaches to hydrocarbon exploration in a wide variety of geological settings globally. Discusses in detail the principles of regional geological analysis and the main geological and geophysical tools Captures and identifies the tectonics of the world in detail, through a series of unique geographic maps, allowing quick access to exact tectonic locations Serves as the ideal introductory overview and complementary reference to the core concepts of regional geology and tectonics offered in volumes 2 and 3 in the series




Novel Approaches to Seafloor Mapping in the Northwest Atlantic


Book Description

Although oceans cover nearly three-quarters of the earth, studies estimate that only a fraction of the seafloor has been mapped at a resolution higher than 1km2. On the continental shelf and in nearshore regions, there are significant gaps in information about the seafloor, including sediment and habitat distribution data. Surveying frequently in these regions can be costly, dangerous, and inefficient without the use of uncrewed vehicles. Furthermore, the cost of surveying infrequently is a lack of understanding geophysical or ecological dynamics and processes in these environments. In this thesis, novel uncrewed vehicles are utilized to evaluate whether the data they collect could be used to increase the resolution or accuracy of maps. The design, construction, and testing of an autonomous hovercraft are outlined in Chapter 2. The hovercraft's autonomy was tested via four autonomous flight paths and the desired path was compared to both the observed heading and direction of motion. Although the accuracy is variable, most headings and direction of motion of the hovercraft were within 50 degrees of the desired direction. The hovercraft was then used to map an eelgrass bed in Cole Harbour, Nova Scotia in Chapter 3. Eelgrass was identified visually through sonar imagery and analytically through a classification algorithm. The eelgrass bed was thickest close to the shore of the tidal flat in the very shallow subtidal/intertidal zone and became patchier with deeper water further from the shore. In Chapter 4 seafloor returns from a glider-mounted single-beam echo sounder were used to create maps of the surficial sediment in Roseway Basin. While these gliders are typically deployed to track whales and copepod distributions in the water column, the backscatter from seafloor returns has not yet been used for ground discrimination. Effective scattering coefficients and density-based clustering were used to characterize the surficial sediment, and these results agreed with other seafloor datasets. Each of the chapters in this thesis describes a novel way of using uncrewed data collection platforms for seafloor mapping. By creatively utilizing data collected by these platforms, spatial or temporal gaps created from infrequent monitoring could be filled, which can strengthen our understanding of coastal and shelf waters.




The Morphostructure of the Atlantic Ocean Floor


Book Description

The study of the topography and structure of the ocean floor is one of the most important stages in ascertaining the geological structure and history of development of the Earth's oceanic crust. This, in its turn, provides a means for purposeful, scientifically-substantiated prospecting, exploration and development of the mineral resources of the ocean. The Atlantic Ocean has been geologically and geophysically studied to a great extent and many years of investigating its floor have revealed the laws governing the structure of the major forms of its submarine relief (e. g. , the continental shelf, the continental slope, the transition zones, the ocean bed, and the Mid-Oceanic Ridge). The basic features of the Earth's oceanic crust structure, anomalous geophysical fields, and the thickness and structure of its sedimentary cover have also been studied. Based on the investigations of the Atlantic Ocean floor and its surrounding continents, the presently prevalent concept of new global tectonics has appeared. A great number of works devoted to the results of geomorphological, geolog ical, and geophysical studies of the Atlantic Ocean floor have appeared. In the U. S. S. R. , such summarizing works as The Geomorphology of the Atlantic Ocean Floor [34], Types of Bottom Sediments of the Atlantic Ocean [24], The Geology of the Atlantic Ocean [38], and, somewhat earlier, Geophysical Studies of the Earth's Crust Structure in the Atlantic Ocean [13], have been published.




Imaging the Sea Floor


Book Description







The Charting of the Oceans


Book Description

Mastery of the sea has been crucial in the quest for power and riches; the transition from the medieval to the modern world was marked by the emergence of European ships from their home waters out into the Atlantic, Indian and Pacific oceans. In their maps and charts the maritime nations have left a unique visual record of their response to the challenge of the sea. This book traces the history of the charts, not as technical documents, but as eloquent witnesses to the discovery of the world beyond Europe, and to man's evolving knowledge of the oceans.




The Floors of the Oceans, V1


Book Description

Text To Accompany The Physiographic Diagram Of The North Atlantic. The Geological Society Of America Special Paper, No. 65.