Outburst flood

Source: Wikipedia, the free encyclopedia.

In

Landslides, lahars, and volcanic dams can also block rivers and create lakes, which trigger such floods when the rock or earthen barrier collapses or is eroded. Lakes also form behind glacial moraines or ice dams, which can collapse and create outburst floods.[3][4]

Definition and classification

Megafloods are

sedimentary deposits and the erosional and constructional landforms that individual megafloods have created. Floods that are known to us through historical descriptions are mostly related to meteorological events, such as heavy rains, rapid melting of snowpacks, or combination of these. In the geological past of the Earth, however, geological research has shown that much larger events have occurred.[3]
In the case of outburst floods, such floods are typically linked to the collapse of a barrier which formed a lake. They fall in the following classification according to the mechanism responsible:

Examples

Examples where evidence for large ancient water flows has been documented or is under scrutiny include:

Overflow of lakes formed by landslides

An example is the lake overflow that caused one of the worst landslide-related disasters in history on June 10, 1786. A landslide dam on Sichuan's

Dadu River, created by an earthquake ten days earlier, burst and caused a flood that extended 1,400 km (870 mi) downstream and killed 100,000 people.[5]

Postglacial rebound

Lake Pielinen
in Finland is an example of this.

Tectonic basins

The Black Sea (around 7,600 years ago)

5600 BC
(dark blue) according to Ryan's and Pitman's theories

A rising sea flood, the proposed and much-discussed refilling of the freshwater glacial Black Sea with water from the Aegean, has been described as "a violent rush of salt water into a depressed fresh-water lake in a single catastrophe that has been the inspiration for the flood mythology" (Ryan and Pitman, 1998). The marine incursion, caused by the rising level of the Mediterranean, apparently occurred around 7,600 years ago. It remains an active subject of debate among geologists, with subsequent evidence discovered to both support and refute the existence of the flood, while the theory that it is the basis of later flood myths is not proven.

Persian Gulf Flood (24,000 to 14,000 years ago, or 12000 to 10000 years ago)

Flooding of this area scattered peoples to both sides of the gulf depression. It was an area fed by four rivers. Rose calls it the "Gulf Oasis" which may have been a demographic refuge fed by the Tigris, Euphrates, Karun, and Wadi Batin rivers. It was suggested to be an area of freshwater springs and rivers.[6][7]

Glacial floods in North America (15,000 to 8,000 years ago)

In North America, during glacial maximum, there were no Great Lakes as we know them, but "proglacial" (ice-frontage) lakes formed and shifted. They lay in the areas of the modern lakes, but their drainage sometimes passed south, into the Mississippi system; sometimes into the Arctic, or east into the Atlantic. The most famous of these proglacial lakes was Lake Agassiz. As ice-dam configurations failed, a series of great floods were released from Lake Agassiz, resulting in massive pulses of freshwater added to the world's oceans.

The

Missoula Floods of Oregon and Washington states were also caused by breaking ice dams, resulting in the Channeled Scablands
.

gorge. Lake Bonneville was not a glacial lake, but glacial age climate change determined the lake level and its overflow. The first scientific report of a megaflood (Gilbert, 1890) describes this event.[8]

The last of the North American proglacial lakes, north of the present Great Lakes, has been designated

Glacial Lake Ojibway by geologists. It reached its largest volume around 8,500 years ago, when joined with Lake Agassiz. But its outlet was blocked by the great wall of the glaciers and it drained by tributaries, into the Ottawa and St. Lawrence Rivers far to the south. About 8,300 to 7,700 years ago, the melting ice dam over Hudson Bay
's southernmost extension narrowed to the point where pressure and its buoyancy lifted it free, and the ice-dam failed catastrophically. Lake Ojibway's beach terraces show that it was 250 metres (820 ft) above sea level. The volume of Lake Ojibway is commonly estimated to have been about 163,000 km3 (39,000 cu mi), more than enough water to cover a flattened-out Antarctica with a sheet of water 10 metres (33 ft) deep. That volume was added to the world's oceans in a matter of months.

The detailed timing and rates of change after the onset of melting of the great ice-sheets are subjects of continuing study.

The Caspian and Black Seas (around 16,000 years ago)

A theory proposed by Andrey Tchepalyga of the

Deluge.[9]

Red Sea floods

The barrier across

Flandrian transgression (and in earlier interglacial periods) suggest that this area may have been subject to outburst flooding.[10]

English Channel floods

Originally there was an isthmus across the Strait of Dover. During an earlier glacial maximum, the exit from the North Sea was blocked to the north by an ice dam, and the water flowing out of rivers backed up into a vast lake with freshwater glacial melt on the bed of what is now the North Sea. A gently upfolding chalk ridge linking the Weald of Kent and Artois, perhaps some 30 metres (100 feet) higher than the current sea level, contained the glacial lake at the Strait of Dover. At some time, probably around 425,000 years ago and again around 225,000 years later the barrier failed[11] or was overtopped, loosing a catastrophic flood that permanently diverted the Rhine into the English Channel and replacing the "Isthmus of Dover" watershed by a much lower watershed running from East Anglia east then southeast to the Hook of Holland and (as at modern sea level) separated Britain from the continent of Europe; a sonar study of the sea bed of the English Channel published in Nature, July 2007,[12] revealed the discovery of unmistakable marks of a megaflood on the English Channel seabed: deeply eroded channels and braided features have left the remnants of streamlined islands among deeply gouged channels where the collapse occurred.[13][11]

The refilling of the Mediterranean Sea (5.3 million years ago)

A catastrophic flood refilled the Mediterranean Sea 5.3 million years ago, at the beginning of the

Mediterranean basin, following the Messinian salinity crisis during which it repeatedly became dry and re-flooded, dated by consensus to before the emergence of modern humans.[15]

The Mediterranean did not dry out during the most recent glacial maximum. Sea level during glacial periods within the Pleistocene is estimated to have dropped only about 110 to 120 metres (361 to 394 ft).[16][17] In contrast, the depth of the Strait of Gibraltar where the Atlantic Ocean enters ranges between 300 and 900 metres (980 and 2,950 ft).[18]

See also

References

External links