Geology of the Dunes
The Oregon Dunes are like no other dunes in the world. Desert-like landscapes, lakes, rivers, ocean and forest blend, creating diverse ecosystems of plants and animals. Managed by the USDA Forest Service, this is the only part of the Oregon coast covered by extensive sand dunes. The sand dunes were formed by wind, water and time.
The sand in the Oregon Dunes is from the Coast Mountain Range, which is sedimentary rock that was uplifted 12 million years ago. As rock was moved downstream by rivers, it tumbled and abraded itself into sand. The present shoreline stabilized 6,000 years ago. Tides, wave action and strong coastal winds moved sand up to 2.5 miles inland for thousands of years. This area of dune development rests on a gently sloping terrace of solid marine sandstone called the Coos Bay Dune Sheet. This low rock surface stretches 56 miles from Heceta Head to Cape Arago and contrasts with steep headlands found on most of the Oregon coastline, which prevent inland movement of sand.
Winds are a major influence in dune formation. Summer winds blow steadily from the north and northwest at 12-16 miles per hour. Mountain barriers near the coast deflect wind currents, sculpting the sand info many different shapes. In winter, winds are generally lighter; however, they can exceed 100 miles per hour during intense winter storms. These winds blow from the south and southwest moving large amounts of sand. Seasonal changes in wind direction reshape dune sculptures and ridges.
Water influences dune formation. Strong ocean currents flowing north in winter and south in summer hold sediment from rivers near the shore. Currents, tides and wave action dredge sand from the ocean floor and deposit it on the beaches where the wind takes over. Sand absorbs and stores a large part of the annual rainfall. Where winds have removed sand down to the water table, plants have flourished. In the wet winter, the rising water table creates marshy areas with standing water several feet deep. With the upward pressure of water, the sand grains become more saturated and may float, resulting in quicksand. Look for quicksand in low, unvegetated areas between the dunes.
Shaping the Sand
Wind and water are the two strongest forces shaping dune formation. Summer winds blow steadily from the north and northwest at 12 to 16 miles per hour. Mountain barriers near the coast deflect wind currents, sculpting the sand into many different shapes. In winter, winds vary more; however, they can exceed 100 miles per hour during intense winter storms. These winds blow from the south and southwest, moving large amounts of sand. Seasonal changes in wind direction reshape dune sculptures and ridges. Strong ocean currents flowing north in winter and south in summer hold sediment from rivers near the shore. Currents, tides and wave action dredge sand from the ocean floor and deposit it on the beaches where the wind takes over. Sand absorbs and stores a large part of the annual rainfall. Where winds have removed sand down to the water table, freshwater plants have flourished. In the wet winter, the rising water table creates marshy areas with standing water several feet deep. With the upward pressure of water, the sand grains become saturated and may float, resulting in quicksand.
Geology Everywhere You Look
The Oregon Dunes are the largest expanse of coastal sand dunes in North America. Spend some time in the dunes; you are sure to see geology in action! Here, the desert-like landscape blends with lakes, rivers, ocean and forest, creating a diverse ecosystem filled with plants and animal. Day to day, season to season this ecosystem can change dramatically.
From the Shore to the Forests - Take A Closer Look!
Strong ocean currents, tides and wave action transport sand along the sloping ocean floor. Smaller, lighter grains of sand, mostly quartz and feldspar, are carried inland by the winds. Heavier grains of sand remain on the beach. Offshore, the sand is 80 to 170 feet deep.
The foredune is a low hill, formed parallel to the ocean edge. Consisting of sand and driftwood, the 25 to 50 foot high foredune is capped by European Beach grass, an introduced plant species.
Hummocks are immediately inland from the foredune. These knob-like mounds are created by sand accumulation around vegetation. When the water table rises in the winter, puddles may surround the hummocks and they appear to be floating islands.
The foredune separates the beach from inland areas. Winds strip away the sand east of the foredune, deflating the area down to the permanently wet sand. This creates a deflation plain where water-loving vegetation thrives. As the dunes move eastward, the plants of the deflation plain also spread eastward.
The northwesterly winds of summer create wave-like patterns called transverse dunes. The crests of these 5 to 20 foot high dunes are perpendicular to the wind direction. Changes in wind direction create the interesting and unusual rides, although strong winter winds from the southwest tend to smooth out these dunes. As the deflation plain expands eastward, so do the transverse dunes.
Floating in the sand, these islands are small isolated remnants of older coastal forests that were almost completely buried by sand. The islands are proof that moving sand is capable of burying whatever is in its way. Steep slopes make the tree islands unstable and susceptible to erosion.
Oblique dunes are the largest and most spectacular dunes. Occurring in parallel series, these dunes can rise to heights of 180 feet with lengths up to a mile. Some oblique dunes are nearly 500 feet above sea level. "Oblique" refers to the slanted angle at which both summer and winter winds hit these dunes. Oblique dunes move constantly, making it impossible for vegetation to grow on them. The west side of an oblique dune consists of a long, sloping ridge. The east side is usually higher and steeper, forming a precipitation ridge. In winter, the southwesterly winds create freestanding sculptures called yardangs. These unusual carvings can reach 15 feet high. The Umpqua Dunes trail provides access to the best example of these dunes.
Winds create "blowouts" in some unstable areas of the coastal forest. Strong winds erode the vegetation-covered surface to bare sand. Once a section has eroded, wind carries the sand further downwind, creating characteristic U-shaped ridges call parabola dunes.
The transition forest is where the ocean-based ecosystem changes to a land-based ecosystem. The interactions in this zone between plants, animals, wind, temperature, rainfall, sand, and fresh and saltwater are unique to this area.
Estuaries are where fresh river water meets salt water. As ocean tides rise, organic matter and nutrients from both areas pool together, creating one of the most fertile environments in the world. These nutrients stimulate the growth of plankton and other organisms, providing food form many plants, fish, birds and mammals.
Lakes abound in the Oregon Dunes. Some of the 32 lakes were once mountain streams that were dammed by sand. Others were ocean inlets that were cut off. Still others were formed when depressions in the sand filled with water as the water table rose. Over the years, several lakes have been buried by sand or dried up.