All posts by Coastal Care

Why the world is running out of sand

Sand miners, Maldives. Photograph: © Denis Delestrac.
As of 2011-2012, when investigative filmmaker Denis Delestrac and team, were first collecting and unveiling sand mining datas and information from the professionals involved, the Sand business was estimated to be a $70 billion industry, worldwide…!—Denis Delestrac (©-2013)
Sand is the second most consumed natural resource, after water. The construction-building industry is by far the largest consumer of this finite resource. The traditional building of one average-sized house requires 200 tons of sand; a hospital requires 3,000 tons of sand; each kilometer of highway built requires 30,000 tons of sand… A nuclear plant, a staggering 12 million tons of sand…”
All captions by: “Sand Wars” Multi Award-Winning Filmmaker Denis Delestrac (©-2013).


It may be little more than grains of weathered rock, and can be found in deserts and on beaches around the world, but sand is also the world’s second most consumed natural resource…

Read Full Article; BBC (11-17-2019)

Why Sand Is Disappearing, By John R. Gillis, Professor Emeritus of History, Rutgers University; The New York Times, November 4th, 2014.

The world is running out of sand; The New Yorker (05-29-2017)

The world is running out of sand; MNN (11-02-2017)

Concrete, or Beaches? World’s Sand Running Out As Global Construction Booms; The Ecologist (05-09-2017)

The Economist explains: Why there is a shortage of sand; The Economist (04-24-2017)
It may be plentiful, but so is the demand for it…

A microscopic look at why the world is running out of sand; Video; The Verge (09-04-2018)

Sand, Rarer Than One Thinks: A UNEP report (GEA-March 2014)
Despite the colossal quantities of sand and gravel being used, our increasing dependence on them and the significant impact that their extraction has on the environment, this issue has been mostly ignored by policy makers and remains largely unknown by the general public.
In March 2014 The United Nations released its first Report about sand mining. “Sand Wars” investigative film by Denis Delestrac – first broadcasted on the european Arte Channel, May 28th, 2013, where it became the highest rated documentary for 2013 – expressly inspired the United Nations Environment Programme (UNEP) to publish this 2014-Global Environmental Alert.

Sand Is in Such High Demand, People Are Stealing Tons of It, By Dave Roos; HowStuffWorks (03-06-2017)
As strange as it may sound, sand is one of the world’s hottest commodities. The global construction boom has created an insatiable appetite for sand, the chief ingredient for making concrete. The problem is that sand isn’t as abundant as it used to be. And when high demand and high value meets scarcity, you open the doors to smuggling…

The Conservation Crisis No One Is Talking About, TakePart (09-21-2016)
Beaches around the world are disappearing. No, the cause isn’t sea-level rise, at least not this time. It’s a little-known but enormous industry called sand mining, which every year sucks up billions of tons of sand from beaches, ocean floors, and rivers to make everything from concrete to microchips to toothpaste…

A looming tragedy of the sand commons; Science (09-08-2017)
Because of the difficulty in regulating their consumption, common-pool resources are prone to tragedies of the commons as people may selfishly extract them without considering long-term consequences, eventually leading to overexploitation or degradation. Even when sand mining is regulated, it is often subject to rampant illegal extraction and trade…

Sand Wars, An Investigation Documentary, By Multi Award-Winning Filmmaker Denis Delestrac (©-2013)
Is sand an infinite resource? Can the existing supply satisfy a gigantic demand fueled by construction booms? What are the consequences of intensive beach sand mining for the environment and the neighboring populations…? This investigative documentary takes us around the globe to unveil a new gold rush and a disturbing fact: the “Sand Wars” have begun…

Global Sand Mining: Learn More, Coastal Care


PETITION: Take Action To End Global Beach Sand Mining, Coastal Care

Illegal beach and dune sand mining operations, near Tangier, Morocco. Photograph: © SAF — Coastal Care

World War II Hazards Emerge on Massively Eroded Australian Beach

Australia. Photo source: © SAF — Coastal Care


Unprecedented coastal erosion on an Australian beach has uncovered thousands of potentially hazardous spiky World War II tank traps…

Read Full Article; Weather News (12-03-2019)

D-Day’s Legacy Sands, Omaha Beach; By Earle F. McBride & M. Dane Picard; Coastal Care’s Beach of the Month June 2012
Before dawn on June 6, 1944, more than 160,000 Allied troops began storming the shores of Normandy, France, in what would be the turning point of World War II. Troops poured out of planes and off ships along an 80-kilometer stretch of coastline. Omaha Beach sand retains evidence of the Invasion…

Great Barrier Reef study shows how reef copes with rapid sea-level rise

Great barrier of reef, Australia. Photo source: ©© Secruza


A survey of coral reef cores on the Great Barrier Reef has revealed how it has responded to recent periods of rapid sea-level rise. The study, covering the past 9000 years, has revealed a system in delicate balance.

Read Full Article; Science Daily (12-03-2019)

Great Barrier Reef health outlook downgraded to “very poor” due to ocean warming; CBS News (08-30-2019)

Why the Great Barrier Reef is in danger; MNN (09-07-2018) (09-12-2018)

Video Captures the Violent Act of Coral Bleaching, LiveScience (08-17-2016)

Global warming is transforming the Great Barrier Reef; Science Daily (04-18-2018)
A new study shows that corals on the northern Great Barrier Reef experienced a catastrophic die-off following the extended marine heatwave of 2016…

Great Barrier Reef coral bleaching has started early, biologist says; Guardian UK (01-19-2018)
Warm water has already begun bleaching coral on the Great Barrier Reef, weeks ahead of the period with highest forecast risk. Satellite data suggest widespread bleaching is possible by March…

A Close-Up Look at the Catastrophic Bleaching of the Great Barrier Reef; Yale E360 (04-10-2017)
Scientists are reporting the second mass bleaching in the Great Barrier Reef in the last year. In a Yale Environment 360 interview, researcher Terry Hughes says these events have damaged two-thirds of the world’s largest coral reef and are directly caused by global warming…

Coral bleaching hits 93% of Great Barrier Reef, Video, Science Daily (04-21-2016)
Australia’s Great Barrier Reef is suffering its worst coral bleaching in recorded history with 93 percent of the World Heritage site affected, scientists say as they reveal the phenomenon is also hitting the other side of the country…

Great Barrier Reef: the scale of bleaching has the most sober scientists worried, Guardian UK (04-16-2016)
I have dived hundreds of times, with different teams of scientists, along the reef. Yet the scale of this bleaching event has even the most sober and senior coral reef scientists worried. If the rhetoric from marine biologists is to be believed, then the Great Barrier Reef is now in the grip of a “bommie apocalypse”…

Great Barrier Reef’s Unprecedented Threat From Dredging, Dumping; Guardian UK (05-07-2014)
The impact of dredging and dumping sediment on the Great Barrier Reef has been far greater than the mining industry has claimed, with nearly 150m tonnes of new dredging set to take place in the reef’s waters, a study shows…

Bacterial communities ‘hitchhiking’ on marine plastic trash

“The unprecedented plastic waste tide plaguing our oceans and shores, can become as limited as our chosen relationship with plastics, which involves a dramatic behavioral change on our part…”
Captions and Photo: © SAF — Coastal Care


Millions of tons of plastic trash are fouling the world’s ocean, most of it tiny pieces of microplastic less than a quarter-inch in size. Even the smallest marine animals can ingest these microplastics, potentially threatening their survival.

Marine microplastics aren’t floating solo, either — they quickly pick up a thin coating of bacteria and other microbes, a biofilm known as “The Plastisphere.”

Using an innovative microscopy method, scientists have revealed the structure of the microbial communities coating microplastic trash collected from a variety of ocean sites…

Read Full Article; Science Daily (12-02-2019)

New UN report finds marine debris harming more than 800 species, costing countries millions; United Nations (12-05-2016)
Marine debris is negatively affecting more than 800 animal species and causing serious losses to many countries’ economies, according to a United Nations report launched December 5th, 2016…

Plastic pollution: When The Mermaids Cry: The Great Plastic Tide, Coastal Care
Washed out on our coasts in obvious and clearly visible form, the plastic pollution spectacle blatantly unveiling on our beaches is only the prelude of the greater story that unfolded further away in the world’s oceans, yet mostly originating from where we stand: the land…

Antarctic ice sheets could be at greater risk of melting than previously thought

Antarctica. Photo courtesy of © Denis Delestrac for Coastal Care’s Photo of the Month, July and August 2018.


Antarctica is the largest reservoir of ice on Earth — but new research by the University of South Australia suggests it could be at greater risk of melting than previously thought…

Read Full Article; Science Daily (12-02-2019)

315 billion-tonne iceberg breaks off Antarctica; BBC News (09-30-2019)
The Amery Ice Shelf in Antarctica has just produced its biggest iceberg in more than 50 years…

Pipe Dream – II; By Sean Davey

By © Sean Davey
Image originally published on February 1st, 2014
In celebration of Coastal Care’s 10 years Anniversary, we are republishing an acclaimed selection of the most popular Photo Of the Month contributions.

“Sean Davey first picked up a Kodak 126 Instamatic camera after school one afternoon in late October of 1977, to photograph a tiny perfect wave at his home beach. Little did he know at the time that it would develop into a lifelong obsession that would take Sean many, many places, in pursuit of his chosen craft of photography.

Fast forward some 30 years and Sean is now a veteran of the surf scene. Widely published in several countries, a career that has spawned more than a 140 magazine covers along the way. When not in Hawaii, shooting the north shore, Sean often leads exploratory photo expeditions to many of the worlds more “out of the way” surf zones…” —About Sean Davey Photography

Sean Davey Photography

Sean Davey, Facebook

“Our Deepest Gratitude And Thanks To Our Talented And Inspiring Photo Of The Month Photographers Contributors.”
—Santa Aguila Foundation – Coastal Care

Skara Brae Beach, Scotland: Thoughts on the Short and Long of Sea-Level Rise; By William J. Neal

By William J. Neal Department of Geology, Grand Valley State University, Allendale, Michigan

“The sea gives and takes. The sea Devoured four houses one winter.”
— Excerpt from “Skara Brae” by George Mackay Brown (1921 – 1996)

Perceptions based on the present – what we see, hear, feel at the moment – bias our perception of the past and future. A static view of our environment is misleading. The human association with water, particularly shorelines, is a case in point. We do not perceive the history of place, and globally we occupy sites as if they are unchanging, not realizing that in fact they are of high risk. The following are the author’s impressions and personal discoveries from a couple of hours’ visit to Skara Brae, Scotland, site of a Neolithic village with origins going back 5000 years. This UNESCO World Heritage Site abounds in mystery, secrets yet to be discovered, and lessons to be derived. The poet, George Mackay Brown’s words, that the “sea gives and takes” reflects the history of Skara Brae’s discovery, partial loss, and is visionary in that the latter continues. Skara Brae, along with several other important archaeological sites in the Orkney Islands, are now in the “sea takes” category.

Skara Brae is now on the shore of Skaill Bay, Mainland, Orkney Islands, just off the northern coast of Scotland (Figure 1). The crescent-shaped beach at the head of the bay is subject to a high tidal range, and during Atlantic storms the shore is battered by very high wave energy (Figure 2). At spring low-tide there is a wide beach, but during the high tides the beach can be completely inundated. In 1850 a storm erosion at the back of the beach exposed some of the houses of the old Neolithic village, roofless but otherwise intact (Figures 3 and 4). The land owner initiated an excavation that continued until 1868, after which the site remained undisturbed, except for being raided for artifacts in 1913. The sea again took a bite out of the site during a 1924 or 1925 storm that destroyed one of the houses. The first-generation protective seawall was then built in the late 1920s, and has since been reinforced several times (Figure 5).

“The environmental setting of the village when first constructed has been determined to be well away from the ocean shore, behind protective dunes… ”
— William J. Neal

In viewing the village, one’s first impression is “why would they build their houses in such a hazardous place?” (Figures 4 and 5). But we must flash back from 5000 years ago to present in order to understand how the site came to be at the mercy of the waves. The environmental setting of the village when first constructed has been determined to be well away from the ocean shore, behind protective dunes, and near a freshwater lake. By that time, the rapid post-ice-age sea-level rise had slowed, but sea level was still rising. And the climate was changing. Very likely, the ocean shoreline was moving up the valley that is now the bay, and some archaeologists suggest that over time, the village was abandoned, perhaps because of storms moving sand dunes over the structures, as well as changes in the culture. In the sense of “the sea gives,” the dune burial preserved the village. Some millennia later, as the bay extended landward, the sea gave again when the 1850 storm revealed some of the village, before beginning the processes of “taking” by eroding the site.

Visiting the site during a low-spring tide reveals a beautiful beach; one in which the sediment distribution reflects the energy gradient of storm waves (Figure 6 and 7). The steep slope of the beach is apparent from atop the bluff, with cobble to boulder sized, flat flagstones at the uppermost back beach, a zone of more rounded cobbles to boulders at the base of the back beach, and the wide sandy inter-tidal beach on which ridges and runnels have developed (Figures 7 and 8). The flat flagstones are derived in part from the bedded sandstone outcrops that cross the beach (Figures 9 and 10). This island’s west coast is made up primarily of Devonian age sedimentary rocks, the “Old Red Sandstone”, which consists of these bedded sandstones and siltstones that have been referred to as ‘flagstones’ since the early days of quarrying, and are still used in construction. The flat stones in the walls of the Skara Brae houses were of the same origin, 5000 years ago.

The low-tide beach is a wonderful canvas on which a variety of bed forms have developed from waves and currents. Ripple marks can be seen in the runnels (troughs) as they drain, and the water-saturated sand from high tide drains during low tide, giving the beach mirror-like watery patches (Figure 8), and forming tiny rill marks from seeps (Figure 11). In places, one can see stripes of light and dark on the beach from truncated antidunes that formed during the falling tide (Figure 12), and beach cusps on a grander scale. The beach sand is generally fine to very fine, and poorly sorted with very small pebbles of dark gray siltstone. The light gray color of the beach reflects the varied sand composition (Figures 13 and 14), which includes a surprising amount of calcareous material from microscopic shells and skeletal fragments (e.g., clams, snails, forams, echinoid spines, and a lot of unidentifiable material). The darker shade is derived from black sand-sized rock fragments and mineral grains including biotite mica. Quartz grains are also common.

Not far from Skara Brae are other ancient sites (e.g., Maeshowe, Stones of Stenness, the Ring of Brodgar), but for this geologist the nearby Yesnaby coast was the highlighted contrast to Skara Brae beach. Yesnaby is a sheer rock coast – beachless with sea cliffs, stacks and arches. All cut in the “Old Red Sandstone” sequence including the Stromness Flagstones (Figure 15) in which one can find ancient ripple marks (Figure 16) and mudcracks on the bedding planes of these ancient lake deposits. And local beds contain fish fossils of the kind first described by Hugh Miller and his contemporaries in the 19th Century, in the days of the development of the science of geology in the British Isles.

For this author, Skara Brae was a place of discovery, that former civilizations did retreat in the face of climate change and associated hazards, that a poet understood better than most that the “sea gives and takes”, that there are a few places like Skara Brae where a seawall is justified (even there the wall contributes to nearby erosion), and, along with its Orkney sister sites, this Neolithic village is an example that a shoreline can be a reservoir to be ‘mined’ for knowledge rather than sand.

Figure Captions

  • Figure 1. Outline map of the Orkney Islands at the northern tip of Scotland (circled area of UK inset map at lower right). The islands are at the boundary of the Atlantic Ocean (left) and the North Sea (right). The star marks the approximate location of Skaill Bay and Skara Brae on the western shore of ‘Mainland’, the largest of the islands.
  • Figure 2. Google Earth image of crescent-shaped Skara Brae Beach at the head of Skaill Bay during low tide. Rocky headlands yoke the beach, and are probably a partial source for the beach sand which is mostly derived from reworking of earlier beaches and sand dunes that formed when the shoreline was seaward of its present position. Even in the satellite image the strong cuspate pattern along the beach is apparent, and one can discern a ridge and runnel pattern. The remnants of Skara Brae village lie atop a cliff/bluff of bedrock, capped by old sand dunes (lower left).
  • Figure 3. Skara Brae’s Neolithic structures were preserved by being buried by sand dunes after their abandonment around 2200 B.C. The stone walls were constructed without cement, but the design and construction created below-ground dwellings that were water-proof. The furniture also was stone. Note people on beach (upper left) which gives perspective that village site is at top of bluff.
  • Figure 4. Skara Brae structures. Note the beach in background (top), and the far bluff of dune sand that is retreating under the influence of storm wave erosion, exacerbated by the rising sea level. Brown wrack line on beach is from high spring tide. Note offset in shore line is past the position of the old village structures, now protected by a seawall (Figure 5)
  • Figure 5. The seawall protecting the archaeologic site was constructed in the late 1920s after a storm had destroyed one of the houses in 1924 or 1925. The natural shoreline position has retreated past the line of the seawall. The erosion rate at the ends of the seawall has probably accelerated due to refracted wave energy.
  • Figure 6. Skara Brae beach at low tide shows the ridge (outer bar) and runnel (trough) system. The water drainage is back flow from runnels that breaches the outer bar, as well as ground water draining from the beach. The brown wrack line in the foreground marks the level of the last high tide. Note the steep upper beach on which cobble to boulder sized material has been concentrated by storm waves, with flatter flagstones at top, and more rounded stones lower on the beach.
  • Figure 7. View looking down the steep beach face from the sand dune cover to the flagstone zone, then rounded cobbles and small boulders, to the intertidal sandy beach. This sediment size/shape distribution reflects the energy gradient of storm waves. The largest storm waves toss the flat flagstones and slabs (cobbles to boulders) to the base of the eroding dune face, with a zone of more rounded stones in the same size range just seaward of the flagstone zone.
  • Figure 8. This view of the low-tide beach also shows the size-sorting pattern as well as the character of the sandy beach. Standing water in the runnels and water seeps along the mid-beach face produce mirror-like surfaces.
  • Figure 9. Close-up of the flagstones. The similarity of these beach rocks and the construction materials of the Neolithic structures are obvious. Given that a similar beach would have been farther from the village site at the time it was occupied, the convenience of the shape of the stones would have made their transport worthwhile.
  • Figure 10. The beach outcrop of a rock unit producing flagstones explains in part the source of these rocks on the upper beach. But some of the beach materials probably have come from the erosion of the nearby headlands.
  • Figure 11. In addition to the larger drainage patterns on the beach (Figure 8), the micro drainage produces smaller bedforms as water seeps from the beach. Rill marks are like micro-canyons cut by the running water. Small 20p coin for scale.
  • Figure 12. Note the striped pattern (dark and light) at the back of the sandy beach (mid-photo). This pattern of truncated anti-dunes forms by wave swash/backwash on the falling tide, and is a fairly common bed pattern on high-energy beaches.
  • Figure 13. The light gray color of the beach sand is due to a fairly high content of dark-colored sand grains. The sand is poorly sorted, but generally fine to very fine in grain size, with some coarser granule to small pebble-sized rock fragments of dark gray siltstone. Dime for scale.
  • Figure 14. A microscopic view of the beach sand shows a surprising amount of calcareous material derived from shelly organisms; the white chalky grains, as well as very fine fragments of thin shells. Whole microscopic snails, clams, and possibly forams were noted. The darker grains include sand-sized rock fragments and mineral grains including black biotite mica. Scale divisions equal mm.
  • Figure 15. The sea cliffs at Yesnaby include the beautiful Stromness Flagstones formation which consists of moderately thin beds (flags) of sandstones and siltstones, part of the “Old Red Sandstone” sequence (Devonian). Not far from this location is a unit containing fish fossils for which the “Old Red” became famous for all over the British Isles in the mid-19th Century.
  • Figure 16. Ripple marks on the bedding planes of these sandstones and siltstones formed around 400 million years ago when these sediments were deposited in an ancient lake basin. These bedforms are not unlike the ripple marks you might find today on the beach at Skara Brae.


This Florida Keys neighborhood has been flooded for nearly 3 months

Photo source: ©© Bryan Elkus


The flooding here and elsewhere is happening during so-called “king tides.” Those are times, mostly in the fall, when the moon’s gravitational pull means tides are higher than usual.

Read Full Article; NPR (11-28-2019)

Rising tides force Miami Beach residents to seek higher ground; CBS News (09-25-2019)

Column: High-rises spell the end for Florida beaches; By Orrin H. Pilkey and J. Andrew G. Cooper; Tampa Bay (07-25-2017)
Floridians are becoming more attuned to sea level rise and more familiar with nuisance flooding related to the rising sea. However, we believe there is less recognition that by century’s end it is likely that most of Florida’s major beaches will be permanently gone…

California King Tides Project: January 10-12 and February 8-9, 2020; California Coastal Commission (10-31-2019)

Worst floods for 50 years bring Venice to ‘its knees’; CNN (11-13-2019)
The worst flooding to hit Venice in more than 50 years has brought the historic city to its knees. Local authorities in the Italian lagoon city called for a state of emergency to be imposed…

Indian Ocean Dipole spells flood danger for East Africa; The New Humanitarian (10-22-2019)
Hundreds of thousands of people in East Africa are affected by heavy rains and floods linked to record-breaking temperature changes in the Indian Ocean. As a result, higher evaporation off the African coastline is being dumped inland as rainfall: a simplified description of 2019’s positive Indian Ocean Dipole (IOD) episode…

Engineers hope high-tech sandbags will keep the beach in Waikiki from disappearing

Coastal erosion, Hawaii. “Sandbagging is pretty much an exercise in futility. The only benefit is psychological, the feeling of doing something…” Captions and Photo source: ©© Davidd


A fresh round of repairs to Hawaii’s most famous beach have been completed ― and engineers hope their latest idea will do more to help the shoreline from washing away.

Over the last three weeks, and at a cost of roughly $700,000, engineers worked to install a 95-foot sandbag groin at Waikiki Beach, along with hauling in tons of new sand to help replenish it…

Read Full Article; Hawaii News (11-29-2019)

‘Sand mattress’ technology to combat Mother Nature at Kuhio Beach; KHON News (12-17-2017)

Waikiki Beach Is Totally Man-Made And Disappearing. Can Hawaii Save It?Huffington Green (03-10-2015)

Doubling of Coastal Erosion by Mid-Century in Hawai’i, Science Daily (03-24-2015)
Chronic erosion dominates the sandy beaches of Hawai’i, causing beach loss as it damages homes, infrastructure, and critical habitat. Researchers have long understood that global sea level rise will affect the rate of coastal erosion. However, new research indicates that coastal erosion of Hawai’i’s beaches may double by mid-century…

Terminal Groins Don’t Stop Erosion; Coastal Review (05-03-2016)

The Negative Impacts Of Groins, (02-12-2009)
The negative impact of groins on downdrift shorelines is well understood. When a groin works as intended, sand moving along the beach in the so-called downdrift direction is trapped on the updrift side of the groin, causing a sand deficit and increasing erosion rates on the downdrift side. This well-documented and unquestioned impact is widely cited in the engineering and geologic literature.

Seawalls: Ecological effects of coastal armoring in soft sediment environments; Science Daily (07-24-2017)
For nearly a century, America’s coasts — particularly those with large urban populations — have been armored with human made structures such as seawalls. These structures essentially draw a line in the sand that constrains the ability of the shoreline to respond to changes in sea level and other dynamic coastal processes…

“Seawalls Kill Beaches,” Open Letters by Warner Chabot And Rob Young; (10-03-2014)

Living on the shores of Hawaii: natural hazards, the environment, and our communities, A book by Chip Fletcher; Robynne Boyd, William J. Neal and Virginia Tice.
“Living on the shores of Hawaii: natural hazards, the environment, and our communities” addresses a wide range of environmental concerns within the context of sustainability and their influence on the future of Hawaii…

Sandbagging at the Shore: North Carolina’s Coastal Sand Bags and Political Sandbaggers; By William Neal, Orrin Pilkey & Norma Longo;
The wonder of modern English is how social use of language expands and changes the meaning of words. Sand bag is a bag filled with sand used for temporary construction—quickly made, easily transported, and easily removed. Typically, sandbagging is the emplacement of sand bags to construct a temporary protective wall or barrier, such as a dike or dam to hold back flood waters, or protection on the battlefield. But the term ‘sandbagging’ has taken on an array of other meanings…

Rethinking Living Shorelines, By Orrin H. Pilkey, Rob Young, Norma Longo, and Andy Coburn;Program for the Study of Developed Shorelines / Western Carolina University, March 1, 2012, Nicholas School of the Environment, Duke University
In response to the detrimental environmental impacts caused by traditional erosion control structures, environmental groups, state and federal resource management agencies, now advocate an approach known as “Living Shorelines”that embraces the use of natural habitat elements such as indigenous vegetation, to stabilize and protect eroding shorelines.

Waikiki beach-renourishement, 2012. Photograph: © SAF — Coastal Care.
“Hawaii’s famed Waikiki Beach started to erode again, less than a year after the completion of a $2.2 million project to replenish the sand on about 1,730 feet of shoreline that had been suffering from chronic erosion.”
“Development is absolutely responsible for the majority of the beach nourishment,” Andrew Coburn, assistant director of The Program for the Study of Developed Shorelines at Western Carolina University, said. “Well over 99 percent of the shorelines that are nourished are developed so there is some economic value placed behind them.”