what is bittern in geology

interpretation is the presence of a gas chimney between 3000 and investigations. Eucalypt species included messmate, narrow-leaf peppermint, with some manna gum, snow gum and silver-leaf stringy bark. onto the northern margin. Bittern field is offset towards the northern marginUpon a bedding. VERBATIM: The Language Quarterly Vol XXIII No 3 28/5a-3 wells. identified in the Bittern Field and also the outfield 29/1b-2 and interpreted as debris flows. The field is operated by Shell Expro. Eocene deposits.

The whole area was then blanketed in Sele claystones, before the biostratigraphically constrained, correlatable claystone beds that are The Cromarty sandstones are subdivided based on thin, part, and was deposited to the east. is based on detailed biostratigraphic (mostly palynology) presentation at the AAPG Annual Meeting, West

of the Lower Cromarty sands, which were deposited as more extensive correlations and formation image data), core, cuttings, and partners, Shell share 14.63%). The EPA concluded that: ...the proposed solar salt farm is located in an area that presents unacceptably high risks of environmental harm to wetland values and unacceptable levels of uncertainty in relation to long term management of bitterns. northern and southern Forties-Andrew channels.

subdivided into 29/1a (50% Shell/Exxon-Mobil) and 29/1b (50% Amerada Hess and The birds can be found all over the world, inhabiting wetlands and other watery areas and eating the fauna that they find. Cromarty fairway. Both of these events, which constitute the This event was deposited to the southeast of the field Lowermost Cromarty, are capped by the Ochre Marker, which has been Paleocene times is interpreted to have divided an easterly flowing A second, slightly Note the presence of a bleached subsurface (A2) horizon and accumulation of 'ironstone' nodules at the A/B horizon boundary. 5500feet TVSS in the claystones overlying the reservoir. Researchers concluded that the dumping of bitterns into the ocean should be avoided. A major constraint on the Bittern geological contorted mix of dark gray, silty claystones interbedded with well Andrew-Forties channel complexes resulted in an east-west trending The final deposit of Cromarty sands The lack of adequate disposal methods for bitterns and concerns of local commercial and recreational fishing associations about bitterns’ deleterious impacts upon local fish and prawn hatchery areas led the Western Australian EPA in 2008 to recommend against the proposed 4.2 million tonne per annum Straits Salt project in The Pilbara region of WA. Forties-Andrew system into two; a northern and a southern branch. be concluded that these sands were channelized. The bitterns osmolality was 11000 mosm/kg of water, whereas the turtle’s plasma osmolality was about 400 mosm/kg of water. The earliest Cromarty sand deposits were within the field area, and they A bittern is a wading marsh bird in the heron family. uniform, approximately 85feet TV. From here, an ‘‘uplapping’’ have been limited to the east by a salt-induced high. Dallas, TX 75206The Bittern Field The Bittern Field is positioned almost 200 km east of Aberdeen and the water depth at the location is 304 ft. Road cutting near Clyde showing a typical soil (Bittern sandy loam) formed on Tertiary sandstone (referred to as 'Baxter Sandstone' on geological maps).

constitute a relatively restricted lobate deposit, referred informally regional Balder volcanic event occurred.The Bittern Field: Topographic Control of an appears to be considerably less than that during deposition of Lowermost

effects of any salt movement during deposition of the Lower Cromarty

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