PEI Sandhills EarthCache

This cache has been archived.

El Nimrod: Archiving at the request of Parks Canada because some IDIOT cacher was found climbing on the dunes "looking for a geocache" -- stupidity has no boundries (it's an EC)!

Thanks to all who visited and followed the cache directions.

More
Hidden : 6/23/2016
Difficulty:
1.5 out of 5
Terrain:
1.5 out of 5

Size: Size: other (other)

Join now to view geocache location details. It's free!

Watch

How Geocaching Works
Looking for a different adventure?

Please note Use of geocaching.com services is subject to the terms and conditions in our disclaimer.

Geocache Description:


Sand dunes are accumulations of wind blown sand found at the rear of a beach, above the usual maximum reach of the waves. They range in size from ridges less than a meter in height and width, to massive dune fields that extend inland for many kilometers. The word “dune” derives from a medieval Germanic or Norse word – “dun”, a hill.

The PEI Sandhills are located on the North Shore of the Island. They are nearly 5 km in length, with a maximum width of 250 m; the Atlantic Ocean is along their north shoreline and the New London Bay along their south shoreline. There is no salt marsh or brackish back-water associated with them on their landward side. In short, they are a long spit of dynamic, ever-changing sandhills and dunes exposed and vulnerable to the wind and sea. The round trip walk to GZ is a flat beach walk approximately 8 km in length, taking about 2 hours. Weather can change quickly along the North Shore, so be vigilant.

Uses of Coastal Sand Dunes

Coastal sand dunes serve many functions.

1. Act as an essential store of sediment, protecting the land behind them from storm erosion and potential sea level rise.
2. With vegetation, trap wind blown sand and prevent sand being blown further inland.
3. Act as a filter for rainwater and groundwater and in some situations provide aquatic habitats (e.g. dune lakes)
4. Provide habitats for specially adapted plants, birds, and animals – several of which are now rare or endangered.

Sand Dune Formation and Life Cycle

Shaped by wind into curving ridges, coastal sand dunes are among the most dynamic and fragile natural formations. Their contours shift over time until hardy dune pioneer plants take hold in drifting sand and create a stable landform. Even then, dunes can change form rapidly under the stress of storm waves and wind, or the traffic of human activity.

Offshore sand bars and sediment deposited at the mouths of rivers are the most important sources of material for dune building. Sediment is carried by long shore currents until a projection landform traps the particles and they are deposited on the beach by wave action. Dune formation begins when wind blows dry sand particles landward from the beach. All it takes is a bit of a breeze (16 km/hr) to put fine sand in motion (Figure 1).

Figure 1


The finest grains may be suspended in the air and carried along (suspension). Heavier grains tend to bounce along as they are lifted into the air, fall back to the ground, then bounce back up again (saltation). The heaviest grains the wind can move are usually nudged along by impact from bouncing, saltating grains (impact creep).


Dunes develop at the back of beaches where there is sufficient sand supply and wind energy to transport it landwards. Drifts accumulate around physical barriers (vegetation, driftwood, rocks) that interrupt the wind flow. With steady winds, the sand drift acts as a barrier to moving sand, and the drift gradually grows into a sizeable mound, forming rows at right angles to the prevailing wind direction (transverse ridges). The wind affects the mound of sand by eroding sand particles from the windward side and depositing them on the leeward side (Figures 2 & 3). Gradually this action causes the dune to “migrate” inland; as it does so it accumulates more and more sand.

Figure 2


Figure 3


All dune fields consist of 2 or 3 sets of parallel dunes, with the most recently formed foredunes nearest the beach, and the older, usually vegetated and stabilized dunes farthest inland. The inland dunes may be thousands of years old.

Young dunes are called yellow dunes while older dunes which have a higher humus content are called grey dunes. Leaching occurs on the dunes, washing humus into the slacks (“valley” or trough between dunes), and the slacks may be much more developed than the exposed tops of the dunes. (Figure 4)

Figure 4


Sand dunes have an ever-changing life cycle, forever moving landward. Beaches and foredunes (those closest to the beach) are in a constant state of change in response to wind conditions, sea levels, and sediment supply. Erosion and accretion (rebuilding) are the results of this readjustment. For example, a beach may take on a very different form after a storm (Figure 5).

Figure 5


During a storm the beach may be eroded and the face of the foredune severely cut back (scarped) as a response to the greater waves imposed upon it. These changes can be rapid – a matter of hours, but the recovery of the beach may be much more gradual – days or weeks, as sand is again returned to the beach and blown up against the eroded dune face. In some cases erosion or accretion is permanent; but more often it is just temporary changes and part of a natural cycle of dune erosion, rebuilding and stabilization. However, until the dune is completely veiled and stabilized by plant cover, sand may be borne away by the wind.

Foredune Flora and Fauna

Sand dunes can be important ecosystems supporting unique plant life (Figures 6 & 7) and a healthy population of small animals, birds and insects.

Figure 6


Figure 7


As a dune forms, plant succession occurs. Critical to the formation, stabilization and post-storm recovery process is the presence of specialized dune plants, in particular, Marram grass (Ammophilia breviligulata). This grass covers much of the surface of the dunes. It is a coarse, pale green grass, and even a single shoot can trap wind borne sand. It thrives on being buried in the sand, an action that stimulates the growth of rhizomes (horizontal runners just below the surface of the sand) and the growth of the shoots and roots. The fine mat of roots further traps sand grains (the roots have a small fungus growing inside them which puts out sticky threads that help to glue the sand grains in place). The grasses also add nitrogen to the soil, meaning other less hardy plants can then colonize the dunes. Closer to the beach you will find purple beach pea (Lathyrus japonicus) while beach heather or woolly hudsonia (Hudsonia tomentosa) forms grey woolly mats on the leeside of dunes and bayberry bushes (Myrica pensylvanica) populate the sheltered hollows.

Threats to Sand Dunes

Coastal sand dunes are one of Prince Edward Island’s most endangered habitats. These dunes are very vulnerable to erosion by natural processes (storm waves, wind), and by human activity (beach vehicles, foot traffic, ‘dune surfing’, construction of seawalls and other structures that interfere with natural coastal processes, and dams that trap river sediments, depleting the sand supply). Other threats include pests (e.g. rabbits), grazing farm animals, which eat native dune grasses, and the introduction of exotic plants and weeds, which invade and displace native dune plants.

Remember -- Stay Off the Dunes. Walking on dunes eliminates the protective plant cover. Studies have shown that it can take as few as 10 footsteps through the same area to destroy a marram grass colony. Once the grass is gone, the wind blows away the exposed sand and carves small depressions into giant holes called blowouts. Blowouts turn stable dunes into constantly shifting hills, unable to support vegetation or wildlife.

To claim this Earthcache:

1. Take and post a picture of you and your GPSr at the base of the dune (optional) and e-mail me the answers to the following:

2. Estimate the height of the sand dune at the posted coordinates (do NOT climb the dune).

3. At GZ, in terms of dune development, are the dunes primarily "yellow" or "grey", and what do you base your answer on?

4. At GZ, what general direction are the two large dunes aligned, and why would this be?

5. What is the general colour of the sand dunes at GZ and why might that be?

6. Looking at the topography of the Sandhills, why do you think there is minimal salt water marshes associated with the dunes?

Do NOT post your answers on your log, encrypted or otherwise.

Failure to answer required questions through e-mail will result in a log deletion without notice. Exceptions will be considered if you contact me first.

Additional Hints (No hints available.)



Advertising with Us

Inventory

There are no Trackables in this cache.

View past Trackables

What are Trackable Items?

Bookmark Lists

View all bookmark lists...