1912
DOI: 10.5962/bhl.title.6874
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The depths of the ocean : a general account of the modern science of oceanography based largely on the scientific researches of the Norwegian steamer Michael Sars in the North Atlantic

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Cited by 6 publications
(6 citation statements)
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“…In the classic work by Menard and Smith [1966], the world ocean hypsometry was analyzed using the most recent Russian and U.S. bathymetric maps available at the time of the study. They concluded that their derived hypsometric curve differed little from that published by Murray and Hjort [1912]. This is somewhat surprising considering that 54 years passed between these studies and that major discoveries on the ocean floor morphology had been published [e.g., Heezen, 1960;Heezen and Ewing, 1961] during this time interval.…”
Section: Hypsometry Of the World Oceanmentioning
confidence: 91%
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“…In the classic work by Menard and Smith [1966], the world ocean hypsometry was analyzed using the most recent Russian and U.S. bathymetric maps available at the time of the study. They concluded that their derived hypsometric curve differed little from that published by Murray and Hjort [1912]. This is somewhat surprising considering that 54 years passed between these studies and that major discoveries on the ocean floor morphology had been published [e.g., Heezen, 1960;Heezen and Ewing, 1961] during this time interval.…”
Section: Hypsometry Of the World Oceanmentioning
confidence: 91%
“…Such a curve is commonly used as a base for description of a region's morphology and geological evolution. With the very limited information available at the beginning of the twentieth century, the world ocean hypsometry was calculated by Murray and Hjort [1912]. The maps underlying their study were compiled by Murray from all available soundings that, at the time, amounted to 5962.…”
Section: Hypsometry Of the World Oceanmentioning
confidence: 99%
“…Therefore, deep sea data gathering is reflected in a few pieces of a puzzled map of discoveries. Tentative exploration of the deep sea is thought to have begun in 1521 with Fernão de Magalhães attempting to sound the Pacific Ocean between two coral islands (Murray and Hjort 1912). Yet, despite recent technological developments, it is still difficult to sample this inaccessible environment due to strong currents, rough bottoms and high costs.…”
Section: Introductionmentioning
confidence: 99%
“…Murray et al. () described the formation of highly silicified resting spores in L. danicus and Gran () reported that these resting spores develop directly from auxospores. Subsequently, Davis et al.…”
mentioning
confidence: 99%