Foredune

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A foredune is a dune ridge that runs parallel to the shore of an ocean, lake, bay, or estuary. Foredunes consist of sand deposited by wind on a vegetated part of the shore. Foredunes can be classified generally as incipient or established. [1]

Contents

Formation

Foredunes may begin as shadow dunes that form in the wind shadows of clumps of vegetation. [2] Several shadow dunes may eventually join to form an incipient foredune. [3] When an incipient foredune reaches a height of about 1.5 feet (0.5 m), it has a significant wind shadow of its own. Wind-blown sand will tend to fall on this incipient dune rather than traveling further inland. When a foredune becomes 3 to 5 feet (0.9 to 1.5 m) high, it may trap all of the wind-blown sand from the beach. [4]

In active dune systems, the foredunes appear closest to the sea or other body of water. However, some dune systems, such as those on eroding coasts, do not have foredunes. In those systems, other kinds of dunes may be closest to the water. [1]

Landscape of Northern California parabolic dunes. DuneSystem.jpg
Landscape of Northern California parabolic dunes.

A foredune ecosystem begins with the first dune ridge directly behind an active beach. The ridge of a foredune can range in height from a few meters to tens of meters tall. Foredunes are formed when sand accumulates and wind actively transforms the landscape. This results in sand sheets can consuming in-land ecosystems. United States Fish and Wildlife Service actively manages Humboldt Bay's Lanphere Dunes. Active sand sheets at Lanphere Dunes have been measured to be in excess of six hundred meters.

Parabolic dunes in Northern California

Parabolic dunes are identified by vegetated dune ridges and vegetated deflated plains. Due to variable wind gusts, parabolic dunes are commonly unvegetated in troughs or dune swells where wind tunnels transport currents. Ripple alignment in association with the main dunes can also identify parabolic dunes. Ripples minuet accumulations of sand against the main dune swale. The heights of ripples are normally measured on a millimeter to centimeter scale. In Humboldt Bay, the wind is predominately blowing in from the northwest. As a result, the dune ridges are formed parallel to the wind currents while ripples are formed perpendicular to the wind.

Wind

Northern California coastal dune environments are subject to high velocity winds at all times throughout the year. This strong variable causes the morphology of the dune ecosystem to constantly change. Dunes can range in height from a meter to tens of meters tall creating elevation changes and habitat complexities. Invasive species can further armor dune ridges, creating linear dunes, and preventing naturalistic parabolic dunes from being created.

Sediment transport

Sand granules are transported in three ways: suspension, saltation, and creep. Suspended grains are fine granules that can easily be picked up by wind and carried for variable distances. Most visitors to coastal beach environments can attest to having sand blown in their face or leaving with a gritty feeling on their skin. This is due to fine sediment suspended in the moisture rich air. When suspended sediment is returned to the ground, granules physically impact the grounded grains. Due to physics principles, the grounded grains are receiving energy from the once suspended sediment. This impact leads to the dislodgement of grounded grains or creep of coarser grains. [6] Saltation is the movement of grains being picked up by the wind and dropped in a cycling repetitive motion.

Sources of sediment

Coastal environments act as drainage outlets for freshwater river systems. As a result, sediment from tributaries and headwaters are deposited at the mouth of the river. Long shore transport is a linear current off the coastline that moves sediment. For Northern California, this current moves sediment in a northern direction. Therefore, sand and sediment constructing Humboldt Bay's thirty-four mile dune ecosystem, is a result of sediment deposition at a southern location. [7]

Sediment accumulation can also be a result of wave action. Wave currents occur in a swash and backwash motion. This continual wave action allows for the movement of sediment. The angles at which the swash and backwash occur, are associated with the off shore transport current as well as the change in winter and summer ocean currents.

Foredune ecology

The vegetation analyzed at the Mad River County Beach showed an evolutionary change in the ecosystem as a result of several thriving invasive species. Upon arrival to the beach, it became visually apparent just how abundant the Ammophila arenaria (European beach grass) species is. According to Pickart and Sawyer (1998), Ammophila arenaria is described as being foredune engineers. As Ammophila arenaria attaches and begins to grow on a relatively flat dune system, wind currents that push sand inland it allows the plant to accumulate and mound massive amounts of sand creating large foredune ridges. [8]

This shift is supporting the invasion of but not limited to, Ammophila arenaria, Tanacetum vulgare (tansy) and Bromus diandrus (ripgut brome). Since introduction of these invasive plants, scientists have recorded a severe displacement in native grasses and dune mat vegetation throughout California. A characteristic of Ammophila arenaria and Bromus diandrus entering an ecosystem, are elevated levels of nitrogen within the soil [8] . Unfortunately, the implementation of nitrogen into the soil, limits the growth and livelihood of other species such as Layia carnosa and Erysimum menziesii .

Since the early 1900s, Ammophila arenaria has been introduced into the California landscape to perform as a natural re-engineering feature to transform the beach landscape. [8] In areas without Ammophila arenaria, dune mat vegetation was relatively abundant and thriving. This data shows that with active restoration efforts to combat invasive species, land managers could sustain a healthy native vegetation population and thus transform the landscape back to its native habitat. Understanding how invasive species change and manipulate landscapes and the characteristics of specific invasive species, is the best way to reduce impacts and restore ecosystems for native species.

Ammophila arenaria is an ecosystem engineer that has the ability to displace native dune mat vegetation by transforming historical dune ecology. [5] Removal of Ammophila arenaria presents a daunting task for land managers and restoration teams. Ammophila arenaria has evolved to grow in“vigorous root and rhizome systems”. [8] Research shows that these root systems can be in excess of ten feet. [9]

Characteristically, Ammophila arenaria invades the historically flat Californian foredunes transforming the ecology of the dune system. As wind currents push sand inland, the Ammophila arenaria begins to accumulate massive amounts of sand creating large foredune ridges. [5] The alteration of dune morphology affects native plants and animal species that rely heavily on the dunes for nourishment and habitat. [8]

Related Research Articles

<span class="mw-page-title-main">Dune</span> Hill of loose sand built by aeolian processes or the flow of water

A dune is a landform composed of wind- or water-driven sand. It typically takes the form of a mound, ridge, or hill. An area with dunes is called a dune system or a dune complex. A large dune complex is called a dune field, while broad, flat regions covered with wind-swept sand or dunes with little or no vegetation are called ergs or sand seas. Dunes occur in different shapes and sizes, but most kinds of dunes are longer on the stoss (upflow) side, where the sand is pushed up the dune, and have a shorter slip face in the lee side. The valley or trough between dunes is called a dune slack.

<span class="mw-page-title-main">Beach</span> Area of loose particles at the edge of the sea or other body of water

A beach is a landform alongside a body of water which consists of loose particles. The particles composing a beach are typically made from rock, such as sand, gravel, shingle, pebbles, etc., or biological sources, such as mollusc shells or coralline algae. Sediments settle in different densities and structures, depending on the local wave action and weather, creating different textures, colors and gradients or layers of material.

<i>Ammophila</i> (plant) Genus of flowering plants in the grass family Poaceae

Ammophila is a genus of flowering plants consisting of two or three very similar species of grasses. The common names for these grasses include marram grass, bent grass, and beachgrass. These grasses are found almost exclusively on the first line of coastal sand dunes. Their extensive systems of creeping underground stems or rhizomes allow them to thrive under conditions of shifting sands and high winds, and to help stabilize and prevent coastal erosion. Ammophila species are native to the coasts of the North Atlantic Ocean where they are usually the dominant species on sand dunes. Their native range includes few inland regions, with the Great Lakes of North America being the main exception. The genus name Ammophila originates from the Greek words ἄμμος (ámmos), meaning "sand", and φίλος (philos), meaning "friend".

<span class="mw-page-title-main">Aeolian processes</span> Processes due to wind activity

Aeolian processes, also spelled eolian, pertain to wind activity in the study of geology and weather and specifically to the wind's ability to shape the surface of the Earth. Winds may erode, transport, and deposit materials and are effective agents in regions with sparse vegetation, a lack of soil moisture and a large supply of unconsolidated sediments. Although water is a much more powerful eroding force than wind, aeolian processes are important in arid environments such as deserts.

<span class="mw-page-title-main">Grey dune</span>

Grey dunes are fixed, stable sand dunes that are covered by a continuous layer of herbaceous vegetation. These dunes are typically located 50–100 meters from the ocean shore and are found on the landward side of foredunes. Grey dunes are named for their characteristic grey color which is a result of the ground cover of lichen combined with a top soil layer of humus.

This article gives an overview of the shingle, strandline and sand-dune communities in the British National Vegetation Classification system.

<span class="mw-page-title-main">Blowout (geomorphology)</span> Depressions in a sand dune ecosystem caused by the removal of sediments by wind

Blowouts are sandy depressions in a sand dune ecosystem (psammosere) caused by the removal of sediments by wind.

<span class="mw-page-title-main">Guadalupe-Nipomo Dunes</span> Dune system in California

Guadalupe-Nipomo Dunes is the largest remaining dune system south of San Francisco and the second largest in the U.S. state of California. It encompasses an 18-mile (29 km) stretch of coastline on the Central Coast of California and extends from southern San Luis Obispo County to northern Santa Barbara County.

<i>Ammophila arenaria</i> Species of flowering plant in the grass family Poaceae

Ammophila arenaria is a species of grass in the family Poaceae. It is known by the common names marram grass and European beachgrass. It is one of two species of the genus Ammophila. It is native to the coastlines of Europe and North Africa where it grows in the sands of beach dunes. It is a perennial grass forming stiff, hardy clumps of erect stems up to 1.2 metres (3.9 ft) in height. It grows from a network of thick rhizomes which give it a sturdy anchor in its sand substrate and allow it to spread upward as sand accumulates. These rhizomes can grow laterally by 2 metres in six months. One clump can produce 100 new shoots annually.

Sand dune ecology describes the biological and physico-chemical interactions that are a characteristic of sand dunes.

<i>Ammophila breviligulata</i> Species of flowering plant in the grass family Poaceae

Ammophila breviligulata is a species of grass native to eastern North America, where it grows on sand dunes along the Atlantic Ocean and Great Lakes coasts. Beachgrass thrives under conditions of shifting sand, sand burial, and high winds; it is a dune-building grass that builds the first line of sand dunes along the coast. Beachgrass is less vigorous in stabilized sand, and is only infrequently found further inland than the coastal foredunes. On the Atlantic coastline of North America, Ammophila breviligulata has been observed as far south as North Carolina, and is often planted in dune restoration projects. Ammophila breviligulata was introduced to the Pacific coast of North America in the 1930s. It is proving to be invasive, and is increasingly important to coastal ecology and development in Oregon, Washington, and British Columbia.

<span class="mw-page-title-main">Lanphere Dunes</span>

The Lanphere Dunes National Natural Landmark a unit of the Humboldt Bay National Wildlife Refuge Complex, is located in Humboldt County, California. The dune complex consists of the wave slope, fore dune, herbaceous and woody swales, coniferous and riparian forest, freshwater swamp, freshwater marsh, brackish marsh, salt marsh, and intertidal mudflats. The site exemplifies dunes succession.

NVC community SD19 is one of the 16 sand-dune communities in the British National Vegetation Classification system. It is one of six communities associated with foredunes and mobile dunes.

<span class="mw-page-title-main">Sand dune stabilization</span> Coastal management practice

Sand dune stabilization is a coastal management practice designed to prevent erosion of sand dunes. Sand dunes are common features of shoreline and desert environments. Dunes provide habitat for highly specialized plants and animals, including rare and endangered species. They can protect beaches from erosion and recruit sand to eroded beaches. Dunes are threatened by human activity, both intentional and unintentional. Countries such as the United States, Australia, Canada, New Zealand, the United Kingdom, and Netherlands, operate significant dune protection programs.

<span class="mw-page-title-main">Schaabe</span>

The Schaabe is a bar, almost twelve kilometres long, on the German Baltic Sea island of Rügen. It joins the peninsulas of Jasmund and Wittow.

<i>Leymus mollis</i> Species of grass

Leymus mollis is a species of grass known by the common names American dune grass, American dune wild-rye, sea lyme-grass, strand-wheat, and strand grass. Its Japanese name is hamaninniku. It is native to Asia, where it occurs in Japan, China, Korea, and Russia, and northern parts of North America, where it occurs across Canada and the northern United States, as well as Greenland. It can also be found in Iceland.

<span class="mw-page-title-main">Ma-le'l Dunes</span>

The Ma-le’l Dunes Cooperative Management Area (CMA) is located south of Lanphere Dunes at the upper end of the North Spit of Humboldt Bay, being approximately one mile north of the unincorporated town of Manila and 3.5 miles west of the City of Arcata, in Humboldt County, California. It consists of approximately 444 acres of public land. Ma-le’l dunes are divided into northern and southern sections. The northern portion is part of Humboldt Bay National Wildlife Refuge and is administered by the U.S. Fish and Wildlife Service (FWS). The southern portion of Ma-le’l is managed by the Bureau of Land Management (BLM) and provides access to the coastal dune environment for dog-walking and equestrian use on designated trails.

<span class="mw-page-title-main">Inland dune</span>

Inland dunes are eolian sand dunes that are found inland, away from coastal regions.

<span class="mw-page-title-main">Cresmina Dune</span> Dune system on the edge of the Sintra-Cascais Natural Park, Portugal

The Cresmina Dune extends over 66 hectares and is a part of the Guincho-Oitavos dune system, located on the edge of the Sintra-Cascais Natural Park near Cascais in Portugal. This dune system is considered fairly unique because, as a result of the prevailing northwest winds, the sand from the Guincho and Cresmina beaches eventually returns to the sea 5 km further to the south near Guia, after migrating over the flat, rocky and largely uninhabited area of Cabo Raso.

<span class="mw-page-title-main">Piejūra</span> Nature park along the Gulf of Riga, Latvia

Dabas parks Piejūra is a nature park along the Gulf of Riga in Latvia founded in 1962. It is a protected nature reserve and a Natura 2000 location. The park stretches 36.6 kilometres (22.7 mi) over an 4,180 hectares area from Riga, through Carnikava Municipality, and up to Saulkrasti. It is a popular seasonal recreation location, notably for beach access. The park is notable for its protected biotopes, particularly its dunes and boreal forests. The park's conservation plan for 2020 onwards was developed under the "LIFE CoHaBit" project.

References

  1. 1 2 Hesp, Patrick (2002). "Foredunes and blowouts: initiation, geomorphology and dynamics" (PDF). Geomorphology. 48 (1–3): 245–268. Bibcode:2002Geomo..48..245H. doi:10.1016/S0169-555X(02)00184-8. Archived from the original (PDF) on 2010-06-25. Retrieved 2012-12-11.
  2. "Lake Michigan Coastal Dunes: Shadow Dunes". Calvin College. Retrieved December 10, 2012.
  3. "Lake Michigan Coastal Dunes: Foredunes". Calvin College. Retrieved December 10, 2012.
  4. "Lake Michigan Coastal Dunes: Active Foredunes". Calvin College. Retrieved December 10, 2012.
  5. 1 2 3 Pickart, A.; Sawyer, J. (1998). Invasive Plant Species. California Native Plant Society. pp. 41–55.
  6. Bierman, P.; Montgomery, D. R. (2014). Chapter 10: Wind as a Geomorphic Agent: Key Concepts in Geomorphology. W. H. Freeman and Company Publishers. pp. 329–354.
  7. Friends of the Dunes (n.d.). Coastal Naturalist Manual. Friends of the Dunes.
  8. 1 2 3 4 Pickart, A.; Sawyer, J. (1998). Ecology and Restoration of Northern California Coastal Dunes. California Native Plant Society. pp. 1–36.
  9. Humboldt County Weed Management Area (2010). Invasive Weeds of Humboldt County: A Guide for Concerned Citizens. Arcata, California.