An essay on currents at sea: By which it appears, There is Reason to apprehend, that the Sea is not a Fluid in a State of Rest, except those Motions which are caused by the Impulse of Winds, and that known by the Name of Tides: And consequently, That this Earth is not of a uniform Density, according to the Supposition of Sir Isaac Newton; but that the Currents of the Gulph of Florida, also on the Coast of Brasil, and the Northern In-Draught on this Western Coast, are Currents of Circulation, kept up by different Densities in this Earth, and its Motion round its Axis. By Joseph Mead
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1. Verfasser: | |
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Format: | Elektronisch E-Book |
Sprache: | English |
Veröffentlicht: |
London
printed for J. Marshall, in St. Clement's Church-Yard, in the Strand
M,DCC,LVII. [1757]
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Schlagworte: | |
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language | English |
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spelling | Mead, Joseph 1707-1799 Verfasser aut An essay on currents at sea By which it appears, There is Reason to apprehend, that the Sea is not a Fluid in a State of Rest, except those Motions which are caused by the Impulse of Winds, and that known by the Name of Tides: And consequently, That this Earth is not of a uniform Density, according to the Supposition of Sir Isaac Newton; but that the Currents of the Gulph of Florida, also on the Coast of Brasil, and the Northern In-Draught on this Western Coast, are Currents of Circulation, kept up by different Densities in this Earth, and its Motion round its Axis. By Joseph Mead London printed for J. Marshall, in St. Clement's Church-Yard, in the Strand M,DCC,LVII. [1757] Online-Ressource ([4],48Seiten,plate) 8° txt rdacontent c rdamedia cr rdacarrier English Short Title Catalog, T18686 Reproduction of original from British Library With a half-title, and an errata slip pasted on the verso of the titlepage Online-Ausg Farmington Hills, Mich Cengage Gale 2009 Eighteenth Century Collections Online Electronic reproduction; Available via the World Wide Web |2009|||||||||| Ocean currents http://nl.sub.uni-goettingen.de/id/0646500800?origin=/collection/nlh-ecc Verlag Volltext |
spellingShingle | Mead, Joseph 1707-1799 An essay on currents at sea By which it appears, There is Reason to apprehend, that the Sea is not a Fluid in a State of Rest, except those Motions which are caused by the Impulse of Winds, and that known by the Name of Tides: And consequently, That this Earth is not of a uniform Density, according to the Supposition of Sir Isaac Newton; but that the Currents of the Gulph of Florida, also on the Coast of Brasil, and the Northern In-Draught on this Western Coast, are Currents of Circulation, kept up by different Densities in this Earth, and its Motion round its Axis. By Joseph Mead Ocean currents |
title | An essay on currents at sea By which it appears, There is Reason to apprehend, that the Sea is not a Fluid in a State of Rest, except those Motions which are caused by the Impulse of Winds, and that known by the Name of Tides: And consequently, That this Earth is not of a uniform Density, according to the Supposition of Sir Isaac Newton; but that the Currents of the Gulph of Florida, also on the Coast of Brasil, and the Northern In-Draught on this Western Coast, are Currents of Circulation, kept up by different Densities in this Earth, and its Motion round its Axis. By Joseph Mead |
title_auth | An essay on currents at sea By which it appears, There is Reason to apprehend, that the Sea is not a Fluid in a State of Rest, except those Motions which are caused by the Impulse of Winds, and that known by the Name of Tides: And consequently, That this Earth is not of a uniform Density, according to the Supposition of Sir Isaac Newton; but that the Currents of the Gulph of Florida, also on the Coast of Brasil, and the Northern In-Draught on this Western Coast, are Currents of Circulation, kept up by different Densities in this Earth, and its Motion round its Axis. By Joseph Mead |
title_exact_search | An essay on currents at sea By which it appears, There is Reason to apprehend, that the Sea is not a Fluid in a State of Rest, except those Motions which are caused by the Impulse of Winds, and that known by the Name of Tides: And consequently, That this Earth is not of a uniform Density, according to the Supposition of Sir Isaac Newton; but that the Currents of the Gulph of Florida, also on the Coast of Brasil, and the Northern In-Draught on this Western Coast, are Currents of Circulation, kept up by different Densities in this Earth, and its Motion round its Axis. By Joseph Mead |
title_exact_search_txtP | An essay on currents at sea By which it appears, There is Reason to apprehend, that the Sea is not a Fluid in a State of Rest, except those Motions which are caused by the Impulse of Winds, and that known by the Name of Tides: And consequently, That this Earth is not of a uniform Density, according to the Supposition of Sir Isaac Newton; but that the Currents of the Gulph of Florida, also on the Coast of Brasil, and the Northern In-Draught on this Western Coast, are Currents of Circulation, kept up by different Densities in this Earth, and its Motion round its Axis. By Joseph Mead |
title_full | An essay on currents at sea By which it appears, There is Reason to apprehend, that the Sea is not a Fluid in a State of Rest, except those Motions which are caused by the Impulse of Winds, and that known by the Name of Tides: And consequently, That this Earth is not of a uniform Density, according to the Supposition of Sir Isaac Newton; but that the Currents of the Gulph of Florida, also on the Coast of Brasil, and the Northern In-Draught on this Western Coast, are Currents of Circulation, kept up by different Densities in this Earth, and its Motion round its Axis. By Joseph Mead |
title_fullStr | An essay on currents at sea By which it appears, There is Reason to apprehend, that the Sea is not a Fluid in a State of Rest, except those Motions which are caused by the Impulse of Winds, and that known by the Name of Tides: And consequently, That this Earth is not of a uniform Density, according to the Supposition of Sir Isaac Newton; but that the Currents of the Gulph of Florida, also on the Coast of Brasil, and the Northern In-Draught on this Western Coast, are Currents of Circulation, kept up by different Densities in this Earth, and its Motion round its Axis. By Joseph Mead |
title_full_unstemmed | An essay on currents at sea By which it appears, There is Reason to apprehend, that the Sea is not a Fluid in a State of Rest, except those Motions which are caused by the Impulse of Winds, and that known by the Name of Tides: And consequently, That this Earth is not of a uniform Density, according to the Supposition of Sir Isaac Newton; but that the Currents of the Gulph of Florida, also on the Coast of Brasil, and the Northern In-Draught on this Western Coast, are Currents of Circulation, kept up by different Densities in this Earth, and its Motion round its Axis. By Joseph Mead |
title_short | An essay on currents at sea |
title_sort | an essay on currents at sea by which it appears there is reason to apprehend that the sea is not a fluid in a state of rest except those motions which are caused by the impulse of winds and that known by the name of tides and consequently that this earth is not of a uniform density according to the supposition of sir isaac newton but that the currents of the gulph of florida also on the coast of brasil and the northern in draught on this western coast are currents of circulation kept up by different densities in this earth and its motion round its axis by joseph mead |
title_sub | By which it appears, There is Reason to apprehend, that the Sea is not a Fluid in a State of Rest, except those Motions which are caused by the Impulse of Winds, and that known by the Name of Tides: And consequently, That this Earth is not of a uniform Density, according to the Supposition of Sir Isaac Newton; but that the Currents of the Gulph of Florida, also on the Coast of Brasil, and the Northern In-Draught on this Western Coast, are Currents of Circulation, kept up by different Densities in this Earth, and its Motion round its Axis. By Joseph Mead |
topic | Ocean currents |
topic_facet | Ocean currents |
url | http://nl.sub.uni-goettingen.de/id/0646500800?origin=/collection/nlh-ecc |
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