Intertidal and Subtidal Zones
With tidal fluctuations as large as 25 vertical feet, Glacier Bay exhibits some of the largest tidal extremes in the world. Visitors to the park will notice dramatic difference between high and low tides. One minute you can be gazing out over 100 yards of mud flats and six hours later the waves can be lapping at your toes.
That area between high and low tides – known as the intertidal zone – is an extremely complex and important biological community and a fun place to explore. Lower portions of the intertidal zone are dominated by marine organisms such as algae and kelp, invertebrates and fishes. Grazers like sea urchins, predators like sea stars and dogwinkles, and space dominators like rockweed, barnacles, and mussels are some of the dominant members that strongly influence this community's structure.
The Intertidal Life of Bartlett Cove
Organisms that live in this area need to be able to move or they need to be able to survive long periods of time out of the water when the tide is low. During such times they are exposed to heat from the sun and risk being eaten hungry animals.
Grasses and sedges colonize the area immediately above the intertidal zone in areas where they find enough stable soil to grow. Because they contain highly nutritious plants, flowers, and berries, these meadows are important food sources for animals. In fact, sedge meadows are perhaps THE most important single habitat type in the park for bears. The absence of large trees and tangled underbrush makes beach meadows ideal for travel, and they serve as important thoroughfares for everything from mink to bears to people.
Where the water is relatively free of suspended particles, sunlight can penetrate the water surface to a depth of over 100 feet. Shallow subtidal communities in this photosynthetic zone may be dominated by dense aggregations of kelp in some areas. These "kelp forests" provide critical nursery areas for numerous invertebrates and marine fishes. They are also key foraging areas for sea otters, seals, many diving birds, and schools of adult salmon. The productivity of these communities – that is, their growth rate and food content – may be the greatest of any in the park. Kelp forests are not found in the glacially influenced areas near the glaciers because the bottom is often too silty for the kelp to find purchase, and the amount of sediments in the water makes it difficult for photosynthesis to take place.
On rocky fjord walls, submarine moraine crests, and current-scoured areas, the fauna is dominated by a variety of attached filter-feeding organisms that include corals, hydroids, sea pens, sponges, sea anemones, barnacles, scallops and mussels. These animals take water into their bodies and filter out water-borne detritus and dissolved organic matter, and in turn provides the base of a food web that includes species such as sculpins, shrimps, flatfish and (in the southern part of Glacier Bay and Icy Strait) rockfish and greenlings. Current-scoured areas in the mid-bay area are considered prime real estate, as kelp and algae can grip the bottom and grow. It is here you will find the greatest diversity of kelps and algae and these areas are especially known for being rich and productive feeding areas for marine life.
Did You Know?
In 1899, an earthquake measuring 8.4 on the Richter Scale so shook the glaciers in Glacier Bay, the budding tourism industry nearly died. There was so much ice in the water from the shattered glaciers, visitors to Glacier Bay did not return to for over ten years.