A Playa Lake Usually Contains Laminated Mudstone

Playa lake laminated mudstone siltstone evaporites rock salt rock gypsum and others glacial environments outwash much like braided streams horizon bedded conglom and cross bedded sandstone mudrocks not there.

A playa lake usually contains laminated mudstone.

Tuff beds selected for 40ar 39ar analysis occur within laminated mudstone are matrix supported and lack evidence of reworking. It form sin very salty lagoons and desert playa lakes detrital rocks mudstone sandstone breccia and conglomerate. In figure 2 the maximum expansion strain ɛ max is plotted against the strength reduction index i s which is defined as i s 1 s cw s cd 100 where s cd and s cw. Laminated to thick bedded.

Mudstone and shale are highly susceptible to slaking and undergo considerable expansion on wetting. Burrowed massive 11111ds1011e dominated by sediment filled tubes having constant diameters and commonly containing soft sediment deformation features deep narrow mud cracks and lacustrine fossils is interpreted as intermiuently exposed shallow lake or swampy flood plain deposits. At lake hill the lower unit contains the cephalopod armenoceras and several species of the. The base of an ideal perennial lake parasequence consists of laminated black shale overlain by laminated or massive gray mudstone both interpreted as perennial lake facies.

Pink and red orthoquartzite. This resulted in the large scale deposition of sandy debris flow in the deep lake region. An aggregate of dolomite mineral crystals that are usually microcrystalline. Playa lakes are characterized by laminated muds evaporites and mudcracks rock description of an outwash plane environment an outwash plane is characterized by sands silts clays and braided stream deposits.

The deposits of eocene lake gosiute that constitute the green river formation of wyoming contain numerous tuff beds that represent isochronous correlatable strati graphic markers. Is interpreted as subaerial playa mud flat deposits. From 1 8 billion year old metamorphic rocks exposed in the black mountains to recent playa sediments deposited in the valley basins death valley possesses a superb geologic record. Chang 7 2 contains mainly mudstone and fine sandstone facies with less shale facies suggesting that the deep lake facies began to shrink and large deltas developed in the northeast and southwest parts and extended lakeward.