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High water mark

A high water mark is a point that represents the maximum rise of a body of water over land. Such a mark is often the result of a flood, but high water marks may reflect an all-time high, an annual high (highest level to which water rose that year) or the high point for some other division of time. Knowledge of the high water mark for an area is useful in managing the development of that area, particularly in making preparations for flood surges.[1] High water marks from floods have been measured for planning purposes since at least as far back as the civilizations of ancient Egypt.[2] It is a common practice to create a physical marker indicating one or more of the highest water marks for an area, usually with a line at the level to which the water rose, and a notation of the date on which this high water mark was set. This may be a free-standing flood level sign or other marker, or it may be affixed to a building or other structure that was standing at the time of the flood that set the mark.[3]

Sign indicating high water marks of different floods in Missouri, United States
High water mark memorial at Lake Missoula, Montana, United States
High water mark sign in Bisset Park, Virginia, United States
High water marks of Arno river (Florence) floods on August 13, 1547 (left) and November 3, 1844 (metal plate on the right). Photographed in Via delle Casine.

A high water mark is not necessarily an actual physical mark,[4] but it is possible for water rising to a high point to leave a lasting physical impression such as floodwater staining. A landscape marking left by the high water mark of ordinary tidal action may be called a strandline and is typically composed of debris left by high tide. The area at the top of a beach where debris is deposited is an example of this phenomenon. Where there are tides, this line is formed by the highest position of the tide, and moves up and down the beach on a fortnightly cycle.[5] The debris is chiefly composed of rotting seaweed, but can also include a large amount of litter, either from ships at sea or from sewage outflows.[6]

Ecological significance

The strandline is an important habitat for a variety of animals. In parts of the United Kingdom, sandhoppers such as Talitrus saltator and the seaweed fly Coelopa frigida are abundant in the rotting seaweed, and these invertebrates provide food for shore birds such as the rock pipit, turnstone[6] and pied wagtail,[7] and mammals such as brown hares, foxes, voles and mice.[5]

Legal significance

One kind of high water mark is the ordinary high water mark or average high water mark, the high water mark that can be expected to be produced by a body of water in non-flood conditions. The ordinary high water mark may have legal significance and is often being used to demarcate property boundaries.[8] The ordinary high water mark has also been used for other legal demarcations. For example, a 1651 analysis of laws passed by the English Parliament notes that for persons granted the title Admiral of the English Seas, "the Admirals power extended even to the high water mark, and into the main streams".[9]

In the United States, the high water mark is also significant because the United States Constitution gives Congress the authority to legislate for waterways, and the high water mark is used to determine the geographic extent of that authority. Federal regulations (33 CFR 328.3(e)) define the "ordinary high water mark" (OHWM) as "that line on the shore established by the fluctuations of water and indicated by physical characteristics such as a clear, natural line impressed on the bank, shelving, changes in the character of soil, destruction of terrestrial vegetation, the presence of litter and debris, or other appropriate means that consider the characteristics of the surrounding areas.[10] For the purposes of Section 404 of the Clean Water Act, the OHWM defines the lateral limits of federal jurisdiction over non-tidal water bodies in the absence of adjacent wetlands. For the purposes of Sections 9 and 10 of the Rivers and Harbors Act of 1899, the OHWM defines the lateral limits of federal jurisdiction over traditional navigable waters of the US.[11] The OHWM is used by the United States Army Corps of Engineers, the United States Environmental Protection Agency, and other federal agencies to determine the geographical extent of their regulatory programs. Likewise, many states use similar definitions of the OHWM for the purposes of their own regulatory programs.

In 2016, the Court of Appeals of Indiana ruled that land below the OHWM (as defined by common law) along Lake Michigan is held by the state in trust for public use. [12]

See also

References

  1. ^ J. Curtis Weaver and Thomas J. Zembrzuski, Jr., "August 31, 1993, Storm Surge and Flood of Hurricane Emily on Hatteras Island, North Carolina", in Charles A. Perry, L. J. Combs, Summary of floods in the United States, January 1992 through September 1993 (1995), U.S. Geological Survey Water-Supply Paper 2499, p. 260, stating: Documentation of notable coastal floods provides scientists and flood-plain managers with useful data and technical information for an improved understanding of the hazard and for improved management of flood-prone areas. Of particular importance is documentation of the duration of flooding (and rates of rise and recession of floodwaters), maximum flood elevations and depths, and delineation of the extent of storm-surge flooding.
  2. ^ Daniel Kahneman, Thinking, Fast and Slow (2011), p. 137.
  3. ^ Nancy McTigue, James M. Symons, The Water Dictionary: A Comprehensive Reference of Water Terminology (2011), p. 284.
  4. ^ Bruce S. Flushman, Water Boundaries: Demystifying Land Boundaries Adjacent to Tidal Or Navigable Waters (2001), p. 73.
  5. ^ a b "Strandline" (PDF). Durham Biodiversity Partnership.
  6. ^ a b (PDF). North Cornwall District Council. Archived from the original (PDF) on 2007-10-18.
  7. ^ Gunnleyg Eldevig & Andrew Flack. "Strand Line". Ecology of Portland Harbour. The Heritage Coast.
  8. ^ Bruce S. Flushman, Water Boundaries: Demystifying Land Boundaries Adjacent to Tidal Or Navigable Waters (2001), p. 72.
  9. ^ Nathaniel Bacon, The Continuation of an Historicall Discourse, of the Government of England until the end of the Reign of Queen Elizabeth (1651), p. 44.
  10. ^ "Electronic Code of Federal Regulations (eCFR)". Electronic Code of Federal Regulations (eCFR).
  11. ^ "USACE 2005 OHWM Regulatory Guidance Letter" (PDF).
  12. ^ "Gunderson v. State of Indiana, Indiana Department of Natural Resources, Court of Appeals of Indiana, Opinion 46A03-1508-PL-1116, December 7, 2016" (PDF). 9 November 2020..

External links

high, water, mark, this, article, about, height, water, over, land, other, uses, disambiguation, high, water, mark, point, that, represents, maximum, rise, body, water, over, land, such, mark, often, result, flood, high, water, marks, reflect, time, high, annu. This article is about the height of water over land For other uses see High water mark disambiguation A high water mark is a point that represents the maximum rise of a body of water over land Such a mark is often the result of a flood but high water marks may reflect an all time high an annual high highest level to which water rose that year or the high point for some other division of time Knowledge of the high water mark for an area is useful in managing the development of that area particularly in making preparations for flood surges 1 High water marks from floods have been measured for planning purposes since at least as far back as the civilizations of ancient Egypt 2 It is a common practice to create a physical marker indicating one or more of the highest water marks for an area usually with a line at the level to which the water rose and a notation of the date on which this high water mark was set This may be a free standing flood level sign or other marker or it may be affixed to a building or other structure that was standing at the time of the flood that set the mark 3 Sign indicating high water marks of different floods in Missouri United States The strandline at Ringstead Beach Dorset United Kingdom High water mark memorial at Lake Missoula Montana United States High water mark sign in Bisset Park Virginia United States High water marks of Arno river Florence floods on August 13 1547 left and November 3 1844 metal plate on the right Photographed in Via delle Casine A high water mark is not necessarily an actual physical mark 4 but it is possible for water rising to a high point to leave a lasting physical impression such as floodwater staining A landscape marking left by the high water mark of ordinary tidal action may be called a strandline and is typically composed of debris left by high tide The area at the top of a beach where debris is deposited is an example of this phenomenon Where there are tides this line is formed by the highest position of the tide and moves up and down the beach on a fortnightly cycle 5 The debris is chiefly composed of rotting seaweed but can also include a large amount of litter either from ships at sea or from sewage outflows 6 Contents 1 Ecological significance 2 Legal significance 3 See also 4 References 5 External linksEcological significance EditThe strandline is an important habitat for a variety of animals In parts of the United Kingdom sandhoppers such as Talitrus saltator and the seaweed fly Coelopa frigida are abundant in the rotting seaweed and these invertebrates provide food for shore birds such as the rock pipit turnstone 6 and pied wagtail 7 and mammals such as brown hares foxes voles and mice 5 Legal significance EditOne kind of high water mark is the ordinary high water mark or average high water mark the high water mark that can be expected to be produced by a body of water in non flood conditions The ordinary high water mark may have legal significance and is often being used to demarcate property boundaries 8 The ordinary high water mark has also been used for other legal demarcations For example a 1651 analysis of laws passed by the English Parliament notes that for persons granted the title Admiral of the English Seas the Admirals power extended even to the high water mark and into the main streams 9 In the United States the high water mark is also significant because the United States Constitution gives Congress the authority to legislate for waterways and the high water mark is used to determine the geographic extent of that authority Federal regulations 33 CFR 328 3 e define the ordinary high water mark OHWM as that line on the shore established by the fluctuations of water and indicated by physical characteristics such as a clear natural line impressed on the bank shelving changes in the character of soil destruction of terrestrial vegetation the presence of litter and debris or other appropriate means that consider the characteristics of the surrounding areas 10 For the purposes of Section 404 of the Clean Water Act the OHWM defines the lateral limits of federal jurisdiction over non tidal water bodies in the absence of adjacent wetlands For the purposes of Sections 9 and 10 of the Rivers and Harbors Act of 1899 the OHWM defines the lateral limits of federal jurisdiction over traditional navigable waters of the US 11 The OHWM is used by the United States Army Corps of Engineers the United States Environmental Protection Agency and other federal agencies to determine the geographical extent of their regulatory programs Likewise many states use similar definitions of the OHWM for the purposes of their own regulatory programs In 2016 the Court of Appeals of Indiana ruled that land below the OHWM as defined by common law along Lake Michigan is held by the state in trust for public use 12 See also Edit Wetlands portalChart datum Mean high water Storm surge Measuring surge Terrace geology benches left by lakes Wash marginReferences Edit J Curtis Weaver and Thomas J Zembrzuski Jr August 31 1993 Storm Surge and Flood of Hurricane Emily on Hatteras Island North Carolina in Charles A Perry L J Combs Summary of floods in the United States January 1992 through September 1993 1995 U S Geological Survey Water Supply Paper 2499 p 260 stating Documentation of notable coastal floods provides scientists and flood plain managers with useful data and technical information for an improved understanding of the hazard and for improved management of flood prone areas Of particular importance is documentation of the duration of flooding and rates of rise and recession of floodwaters maximum flood elevations and depths and delineation of the extent of storm surge flooding Daniel Kahneman Thinking Fast and Slow 2011 p 137 Nancy McTigue James M Symons The Water Dictionary A Comprehensive Reference of Water Terminology 2011 p 284 Bruce S Flushman Water Boundaries Demystifying Land Boundaries Adjacent to Tidal Or Navigable Waters 2001 p 73 a b Strandline PDF Durham Biodiversity Partnership a b Strandlliines PDF North Cornwall District Council Archived from the original PDF on 2007 10 18 Gunnleyg Eldevig amp Andrew Flack Strand Line Ecology of Portland Harbour The Heritage Coast Bruce S Flushman Water Boundaries Demystifying Land Boundaries Adjacent to Tidal Or Navigable Waters 2001 p 72 Nathaniel Bacon The Continuation of an Historicall Discourse of the Government of England until the end of the Reign of Queen Elizabeth 1651 p 44 Electronic Code of Federal Regulations eCFR Electronic Code of Federal Regulations eCFR USACE 2005 OHWM Regulatory Guidance Letter PDF Gunderson v State of Indiana Indiana Department of Natural Resources Court of Appeals of Indiana Opinion 46A03 1508 PL 1116 December 7 2016 PDF 9 November 2020 External links Edit Look up high water mark in Wiktionary the free dictionary Retrieved from https en wikipedia org w index php title High water mark amp oldid 1102107436, 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