Depth sounding

Depth sounding refers to the act of measuring depth. It is often referred to simply as sounding. Data taken from soundings are used in bathymetry to make maps of the floor of a body of water, and were traditionally shown on nautical charts in fathoms and feet. The National Oceanic and Atmospheric Administration (NOAA), the agency responsible for bathymetric data in the United States, still uses fathoms and feet on nautical charts. In other countries, the International System of Units (metres) has become the standard for measuring depth. Depth sounding refers to the act of measuring depth. It is often referred to simply as sounding. Data taken from soundings are used in bathymetry to make maps of the floor of a body of water, and were traditionally shown on nautical charts in fathoms and feet. The National Oceanic and Atmospheric Administration (NOAA), the agency responsible for bathymetric data in the United States, still uses fathoms and feet on nautical charts. In other countries, the International System of Units (metres) has become the standard for measuring depth. 'Sounding' derives from the Old English sund, meaning 'swimming, water, sea'; it is not related to the word sound in the sense of noise or tones, but to sound, a geographical term. Traditional terms for soundings are a source for common expressions in the English language, notably 'deep six' (a sounding of 6 fathoms): see John Ehrlichman. On the Mississippi River in the 1850s, the leadsmen also used old-fashioned words for some of the numbers; for example instead of 'two' they would say 'twain'. Thus when the depth was two fathoms, they would call 'by the mark twain!'. The American writer Mark Twain, a former river pilot, likely took his pen name from this cry. The term lives on in today's world in echo sounding, the technique of using sonar to measure depth. A sounding line or lead line is a length of thin rope with a plummet, generally of lead, at its end. Regardless of the actual composition of the plummet, it is still called a 'lead'. Leads were swung, or cast, by a leadsman, usually standing in the chains of a ship, up against the shrouds. Measuring the depth of water by lead and line dates back to ancient civilization. It continues in widespread use today in recreational boating and as a backup to electronic echo sounding devices which are prone to failure and inaccuracy. Greek and Roman navigators are known to have used sounding leads, some of which have been uncovered by archaeologists. Sounding by lead and line continued throughout the medieval and early modern periods and is still commonly used today. The Bible describes lead and line sounding in Acts, whilst the Bayeux Tapestry documents the use of a sounding lead during William the Conqueror's 1066 landing in England. Lead and line sounding operates alongside sounding poles, and/or echo sounding devices particularly when navigating in shallower waters and on rivers. At sea, in order to avoid repeatedly hauling in and measuring the wet line by stretching it out with one's arms, it is common practice to tie marks at intervals along the line. These marks are made of leather, calico, serge and other materials, and so shaped and attached that it is possible to 'read' them by eye during the day or by feel at night. Traditionally the marks were at every second or third fathom: at 2, 3, 5, 7, 10, 13, 15, 17, and 20 fathoms. The 'leadsman' called out the depth as he read it off the line. If the depth was at a mark he would call 'by the mark' followed by the number, while if it was between two marks, he would call 'by the deep' followed by the estimated number; thus 'by the mark five,' since there is a five-fathom mark, but 'by the deep six,' since there is no six-fathom mark. Fractions would be called out by preceding the number with the phrases 'and a half,' 'and a quarter,' or 'a quarter less'; thus 4 3/4 fathoms would be called as 'a quarter less five,' 3 1/2 as 'and a half three,' and so on. Soundings may also be taken to establish the ship's position as an aid in navigation, not merely for safety. Soundings of this type were usually taken using leads that had a wad of tallow in a concavity at the bottom of the plummet. The tallow would bring up part of the bottom sediment (sand, pebbles, clay, shells) and allow the ship's officers to better estimate their position by providing information useful for pilotage and anchoring. If the plummet came up clean, it meant the bottom was rock. Nautical charts provide information about the seabed materials at particular locations. Nautical charts also include depth contour lines. It is thus sometimes possible to navigate in poor visibility by noting which contour line one is closest to. During the nineteenth century, a number of attempts were made to mechanise depth sounding. Designs ranged from complex brass machines to relatively simple pulley systems. Navies around the world, particularly the Royal Navy in Britain, were concerned about the reliability of lead and line sounding. The introduction of new machines was understood as a way to introduce standardised practices for sounding in a period in which naval discipline was of great concern. One of the most widely adopted sounding machines was developed in 1802 by Edward Massey, a clockmaker from Staffordshire. The machine was designed to be fixed to a sounding lead and line. It featured a rotor which turned a dial as the lead sank to the sea floor. On striking the sea floor, the rotor would lock. Massey's sounding machine could then be hauled in and the depth could be read off the dials in fathoms. By 1811, the Royal Navy had purchased 1,750 of these devices: one for every ship in commission during the Napoleonic Wars. The Board of Longitude was instrumental in convincing the Royal Navy to adopt Massey's machine.