![]() ![]() The configuration options vary depending on the monitor type that you select.įor documentation or more information, click the Help icon next to the list. Monitor type other than All - You must configure the monitor type. All - All the monitor types will have default values. ![]() Name of the monitor type that you want to configure. You cannot add or remove them from a profile. The monitor types that belong to a profile are pre-determined. To view all the monitor types that belong to a selected profile, click the Click to view Monitor Types option. If the profile has no monitor types that require input, all the monitor types are enabled by default and the Monitor Type list is disabled. If a profile has monitor types that require you to enter information, they are listed in the Monitor type list, and you can configure them. Each monitoring profile is associated with a group of monitor types. Name of the monitor profile to which the monitor types that you want to enable are associated.Įach solution contains multiple monitoring profiles that help to reduce unnecessary monitoring. Version of the selected monitoring solution A solution can have many Knowledge Modules (KMs) under it. During humid intervals, sheet-floods and high-sinuosity rivers transported a more mud-rich sediment load into the basin, where eolian activity was minimal.Name of the monitoring solution. During arid intervals, ephemeral braided streams transported sandy bed-load into the erg-margin area, where eolian reworking took place. These climatic fluctuations apparently controlled both sediment yield to the basin and the depositional conditions in the erg-margin region. The stacked drying-upward or drying-wetting-upward sequences suggest that this long-term climatic change was characterized by a number of fluctuations between relatively arid and humid conditions. The general time trend is interpreted as a gradual change toward a more humid climate. Individual sequences show much lateral variation but characteristically contain lower, muddy, ephemeral-stream deposits and upper, sandy, ephemeral-stream deposits sand-sheet deposits or incipientdune deposits. Sediments of the overlying association contain up to six drying-upward or drying-wetting-upward sequences but are apparently only fully preserved in the outer erg-margin zone. The basal association thins markedly toward the west-northwest. Sequences of the inner erg-margin zone contain dune facies in their upper parts, sequences in the intermediate erg-margin zone contain sand-sheet facies, and those in the outer erg-margin zone contain sabkha facies. The sediments of the basal association are composed of three drying-upward or locally drying-wetting-upward sequences that can be traced from the erg margin 100 km slightly upwind (that is, toward the west-northwest) into the outer erg-margin zone. The succession is divided into a basal erg-margin association (8-27 m) dominated by eolian facies and an overlying erg-margin association (as much as 90 m thick) composed mainly of fluvial and lacustrine facies. The erg-margin deposits, which extend across a 50- to 100-km-wide region, are composed of dune, eolian sand-sheet, mud-flanked eolian, sabkha, ephemeral-stream and lacustrine facies. ![]() The Moenave Formation (Dinosaur Canyon Member) and the closely associated Wingate Sandstone in southern Utah represent the southwestern erg margin of the Lower Jurassic Wingate erg.
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