Artificial intelligent assistant

overbank

answer Answers

ProphetesAI is thinking...

MindMap

Sources

1
overbank
▪ I. ˈoverbank, a. Artillery. [f. over prep. + bank n.] Applied to a kind of gun-carriage for muzzle-loading guns, so constructed as to allow of the gun's being fired over the parapet.1879 Man. Artillery Exerc. 8 The adoption of overbank carriages, jointed rammers, &c., for our siege guns. 1884 Mil.... Oxford English Dictionary
prophetes.ai 0.0 3.0 0.0
2
Overbank
Paleosols can serve as bounds for overbank depositional sequences or alternate with overbank deposits where flooding is episodic. Overbank deposits are climate-dependent. Of course, the frequency of floods has a major impact on overbank deposits. wikipedia.org
en.wikipedia.org 0.0 1.5 0.0
3
Dockum Group
The Santa Rosa is overlain by the Tecovas Formation (and its New Mexican equivalent, the Garita Creek Formation), which is dominated by overbank (distal The Trujillo Sandstone, channel-deposits, and Cooper Canyon Formation (also known as the Bull Canyon Formation), overbank deposits with minor channel and wikipedia.org
en.wikipedia.org 0.0 0.90000004 0.0
4
Hoback Formation
A prominent sandstone facies (with crossbedding, overbank deposits, and large pebbly deposits), thought to represent a large stream, is also present through wikipedia.org
en.wikipedia.org 0.0 0.6 0.0
5
RML 40-pounder gun
In some cases special overbank carriages were issued for this use. wikipedia.org
en.wikipedia.org 0.0 0.6 0.0
6
Megafan
Generally the three-dimensional architecture of megafan deposits consists of multi-storied sandsheets, gravel in upper reaches, interbedded with overbank wikipedia.org
en.wikipedia.org 0.0 0.3 0.0
7
Mendozasaurus
"Fossil preservation of large titanosaur sauropods in overbank fluvial facies: a case study in the Cretaceous of Argentina". wikipedia.org
en.wikipedia.org 0.0 0.3 0.0
8
Fedexia
The earliest portions of the Casselman Formation, consisting of sandstones and siltstones, are overbank levee deposits that were formed at the shoreline Above the sandstone lies the Birmingham Shale, which includes fine-grained siltstone and shale overbank deposits. wikipedia.org
en.wikipedia.org 0.0 0.3 0.0
9
Meander cutoff
Formation A chute cutoff channel can form during a flood resulting in an overbank flow where water goes over the banks of the river, creating erosion Neck cutoff channels are commonly formed the same way when an overbank flow occurs during a flood and the narrow piece of land between a bend in a meander wikipedia.org
en.wikipedia.org 0.0 0.3 0.0
10
SpongeBob SquarePants Rock Bottom Plunge
Guests then "plunge" down the past-vertical drop at 97 degrees, and ride through: a vertical loop at 40 miles per hour, speed hill, cutback overbank turn , heartline roll, mid-course break run, overbank helix, an additional break run, then finally return to the boarding station. wikipedia.org
en.wikipedia.org 0.0 0.3 0.0
11
Galula Formation
typified by coarser sandstone, a higher frequency of conglomerates, higher proportions of extraformational clasts, thicker and a greater frequency of overbank Namba member is between 340–360 m in the type section, and is less variable in facies, predominated by very fine-to medium-grained sandstones with less overbank wikipedia.org
en.wikipedia.org 0.0 0.0 0.0
12
Litothallus
Litothallus is a genus of non-marine thalloid organism found in overbank deposits from the Triassic of Antarctica. wikipedia.org
en.wikipedia.org 0.0 0.0 0.0
13
门多萨龙属
"Fossil preservation of large titanosaur sauropods in overbank fluvial facies: a case study in the Cretaceous of Argentina". wikipedia.org
zh.wikipedia.org 0.0 0.0 0.0
14
Floodplain
Formation Most floodplains are formed by deposition on the inside of river meanders and by overbank flow. Natural levees are ridges along river banks that form from rapid deposition from the overbank flow. wikipedia.org
en.wikipedia.org 0.0 0.0 0.0
15
Ferris Formation
It contains a variety of trace and body fossils, preserved in sandy fluvial channel deposits and overbank units. wikipedia.org
en.wikipedia.org 0.0 0.0 0.0