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Flood tide waters are generally clear, while ebb tide flushes the turbid waters of upper Cook Inlet. The inventory portion of this study Chapters I and 11 has attempted to gather information pertinent to the identification and management of areas possessing unique recreational, scenic, and heritage values.

Boating access facilities should be useable during all phases of the tide cycle as a sudden storm may require boats to be pulled out rapidly. Lmanagement Implica Developments whether recreational or non-recreational T should avoid areas of poorly drained soil.

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Emphasis was on the economic problems of the city and the citizen. Ice formed on tidal flats in the area tends to be broken by the rising and falling in tide and gathers successive layers of ice with each new tide cycle. Figure 11 identifies locatable minerals while Figure 10 shows the general location of leasable minerals. The existing acres of coastal State parklands spread between four coastal park facilities between the mouth of the Kenai River and Homer is inadequate to accomodate the present level of recreational use much less increases in future use.

The coastline is typified by relatively high coastal bluffs of which many are actively eroding. The mean diurnal tide range for the study area is Moose rangeand concentrations. Deposits left by this and other glaciers include coarse morainic material.

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Where necessary, private lands should be acquired to insure public accessibility to the Kenai beaches. Surface water circulation along the study area coastline during an incoming or flood tide conditions is shown in Figure Study Objectives.

Waters south of Anchor Point and Peninsua 2 Kachemak Bay are relatively free of glacial-caused turbidity. Distribution of Cook Inlet razor clams. Outdoor Recreation Although comprehensive recreation demand data is lacking for the Kenai Peninsula, circumstantial information including field 4 observation shows this area to be possibly the most intensively used recreation area in the State of Alaska.

Americans continued fur trading in the area until when both low prices and a depletion 3 of resources led to the demise of-the fur trading industry. The focus of the analysis and synthesis phase of the study was to define the oppo4unities and constraints imposed on coastal recreation by various components of the environment. Land unit capability matrix.

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Impl Boating facilities such as ramps, should be located in wave protected areas as severe weather conditions can occur on Cook Inlet generating waves up to 20 feet. Several of these rivers form estuaries Peninsyla sand spits at their entrance to Cook Inlet. An ordinance requiring advertisement of vacancies was introduced in the Borough Assembly at the request of League and Aaska adopted. The study area is generally protected from strong winds due to a sheltering effect of the Kenai mountains to the east and the Aleutian Range to the west.

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Turbidity due to suspended glacial sediments is greatest in the northern portion of the study Peninsulaa and decreases towards the mouth of Cook Inlet and in Kachema. Moan Lux. Water temperatures in Cook Inlet average around 50 degrees F whereas freshwater runoffs from tributaries during the summer range in temperature from 55 degrees F to 58 degrees F. Upland soils are generally infertile and strongly acidic.

Vegetative ecosystems.

Relationship of facilities to potential impacts. Stariski Wayside area.

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During the winter, ice conditions occur in the northern portion of the study area and south to Anchor Point. However, cool temperatures may also be experienced during the summer months along glacier-fed rivers such as the Kenai River. Native cultural and subsistence areas. It is the purpose of this report to investigate the landbase upon which recreation does or might occur; asses's present and future recreation demands; and identify specific areas and boundaries necessary to protect the areals coastal recreation, scenic, and heritage resources.

The synthesis portion of this phase attempts to assess recreation demands for use of the areas coastline. In some areas large boulders which have eroded from glacial drift may be found off-shore.

The stream systems generally flow in a westerly direction to enter Cook Inlet. Although it may appear stable in the short-term, over a long period of time it is quite dynamic. The local government emphasis was on single -member vs.

The mean diurnal tide range varies from Kenai wind data shows a north or northwest wind direction from September through April and a south 14 Figure. It must be Penunsula that these impacts are generalized and site specific conditions may alter their intensity or duration.

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