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MY'STORY

The MOVE Fire

This is a personal recollection on the Move fire on May 13, 1985 Philadelphia police fired thousands of rounds at the MOVE house, city officials approved dropping an explosive device on the roof, the resulting fire was allowed to burn, 11 people—including five children—died, and 61 homes were destroyed. Philadelphia City Council later called it a “brutal attack carried out by the City of Philadelphia on its own citizens” and acknowledged that no individual faced criminal consequences for the bombing. One timeline correction worth preserving for the BHP record: the major previous MOVE-police confrontation was August 8, 1978, about seven years before the bombing, not a year or two earlier. Officer James Ramp was killed, other police and firefighters were wounded, nine MOVE members were later convicted, and television cameras recorded police beating Delbert Africa during his arrest. The 1985 MOVE Commission later specifically criticized city planners for failing to adequately use lessons from that 1978 confrontation. And that actually strengthens the point you’re making: 1985 did not happen without precedent or institutional memory. There had already been a deadly confrontation with MOVE, years of conflict, negotiations and police involvement before Osage Avenue.

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BLACK FACTS
The Truths They Never Taught You...

Ruler of the Mali Empire in the 14th century

Mansa Musa was the ruler of the Mali Empire in West Africa. Details recorded here should be sourced; unknown information is left blank.

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BHP gathered finds from its connected research sources. Showing the 4 strongest Black History matches.
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Wikipedia

Tidal bore

A bore in Morecambe Bay, in the United Kingdom
Video of the Arnside Bore, in the United Kingdom
The tidal bore in Upper Cook Inlet, in Alaska

A tidal bore,[1] often simply given as bore in context, is a tidal phenomenon in which the leading edge of the incoming tide forms a wave (or waves) of water that travels up a river or narrow bay, reversing the direction of the river or bay's current. It is a strong tide that pushes up the river, against the current.

Description

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Bores occur in relatively few locations worldwide, usually in areas with a large tidal range (typically more than 6 meters (20 ft) between high and low tide) and where incoming tides are funneled into a shallow, narrowing river or lake via a broad bay.[2] The funnel-like shape not only increases the tidal range, but it can also decrease the duration of the flood tide, down to a point where the flood appears as a sudden increase in the water level. A tidal bore takes place during the flood tide and never during the ebb tide.

Undular bore and whelps near the mouth of Araguari River in northeastern Brazil. The view is oblique towards the mouth from airplane at approximately 30 m (100 ft) altitude.[3]

A tidal bore may take on various forms, ranging from a single breaking wavefront with a roller — somewhat like a hydraulic jump[4][5]⁠— to undular bores, comprising a smooth wavefront followed by a train of secondary waves known as whelps.[6] Large bores can be particularly unsafe for shipping but also present opportunities for river surfing.[6]

Two key features of a tidal bore are the intense turbulence and turbulent mixing generated during the bore propagation, as well as its rumbling noise. The visual observations of tidal bores highlight the turbulent nature of the surging waters. The tidal bore induces a strong turbulent mixing in the estuarine zone, and the effects may be felt along considerable distances. The velocity observations indicate a rapid deceleration of the flow associated with the passage of the bore as well as large velocity fluctuations.[7][8] A tidal bore creates a powerful roar that combines the sounds caused by the turbulence in the bore front and whelps, entrained air bubbles in the bore roller, sediment erosion beneath the bore front and of the banks, scouring of shoals and bars, and impacts on obstacles. The bore rumble is heard far away because its low frequencies can travel over long distances. The low-frequency sound is a characteristic feature of the advancing roller in which the air bubbles entrapped in the large-scale eddies are acoustically active and play the dominant role in the rumble-sound generation.[9]

Etymology

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The word bore derives through Old English from the Old Norse word bára, meaning "wave" or "swell."

Effects

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Tidal bores can be dangerous. Certain rivers such as the Seine in France, the Petitcodiac River in Canada, and the Colorado River in Mexico to name a few, have had a sinister reputation in association with tidal bores. In China, despite warning signs erected along the banks of the Qiantang River, a number of fatalities occur each year by people who take too much risk with the bore.[2] The tidal bores affect the shipping and navigation in the estuarine zone, for example, in Papua New Guinea (in the Fly and Bamu Rivers), Malaysia (the Benak in the Batang Lupar), and India (the Hooghly River bore).

On the other hand, tidal bore-affected estuaries are rich feeding zones and breeding grounds of several forms of wildlife.[2] The estuarine zones are the spawning and breeding grounds of several native fish species, while the aeration induced by the tidal bore contributes to the abundant growth of many species of fish and shrimp (for example in the Rokan River, Indonesia). The tidal bores also provide opportunity for recreational inland surfing, such as the Seven Ghosts bore on the Kampar River, Indonesia or the Severn Bore on the River Severn, England.

Scientific studies

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Scientific studies have been carried out at the River Dee[10] in Wales in the United Kingdom, the Garonne[11][12][13][14][15] and Sélune[16] in France, the Daly River[17] in Australia, and the Qiantang River estuary[18] in China. The force of the tidal bore flow often poses a challenge to scientific measurements, as evidenced by a number of field work incidents in the River Dee,[10] Rio Mearim, Daly River,[17] and Sélune River.[16] In terms of physical modelling (hydrodynamics), a tidal bore often well represented by a soliton.

Rivers and bays with tidal bores

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Rivers and bays that have been known to exhibit bores include those listed below.[2][19]

Asia

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The Qiantang River tidal bore overwhelming local infrastructure in 2024

Oceania

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Australia

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New Zealand

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Papua New Guinea

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Europe

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Ireland

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United Kingdom

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The Trent Aegir seen from West Stockwith, Nottinghamshire, 20 September 2005
The Trent Aegir at Gainsborough, Lincolnshire, 20 September 2005
A tidal bore wave moves along the River Ribble between the entrances to the Rivers Douglas and Preston.
Tidal bore on the River Ribble

Belgium

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France

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The phenomenon is generally named un mascaret in French.[23] but some other local names are preferred.[19]

North America

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United States

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Tidal bore on the Petitcodiac River
  • The Turnagain Arm of Cook Inlet, Alaska. Up to 2 meters (7 ft) and 20 km/h (12 mph).
  • Historically, the Colorado River had a tidal bore up to 6 feet, that extended 47 miles up river.
  • The Savannah River up to 10 miles (16 km) inland.[citation needed]
  • Small tidal bores, only a few inches in height, have been observed advancing up tidal bayous on the Mississippi Gulf Coast.

Canada

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With the Bay of Fundy having the highest tidal range in the world, most rivers draining into the upper bay between Nova Scotia and New Brunswick have significant tidal bores. They include:

  • The Petitcodiac River formerly had the highest bore in North America at over 2 metres (6.6 ft) in height, but causeway construction between Moncton and Riverview in the 1960s led to subsequent extensive sedimentation which reduced the bore to little more than a ripple. After considerable political controversy, the causeway gates were opened on April 14, 2010, as part of the Petitcodiac River Restoration Project and the tidal bore began to grow again.[24] The restoration of the bore has been sufficient that in July 2013, professional surfers rode a 1 metre (3.3 ft)-high wave 29 kilometres (18.0 mi) up the Petitcodiac River from Belliveau Village to Moncton to establish a new North American record for continuous surfing.[25]
  • The Shubenacadie River in Nova Scotia. When the tidal bore approaches, completely drained riverbeds are filled. It has caused the deaths of several tourists who were in the riverbeds when the bore came in.[citation needed] Tour boat operators offer rafting excursions in the summer.
  • The bore is fastest and highest on some of the smaller rivers that connect to the bay including the River Hebert and Maccan River on the Cumberland Basin, the St. Croix and Kennetcook rivers in the Minas Basin, and the Salmon River in Truro.[26]

Mexico

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Historically, there was a tidal bore on the Gulf of California in Mexico at the mouth of the Colorado River. It formed in the estuary about Montague Island and propagated upstream. It was once very strong, but diversions of the river for irrigation have weakened the flow of the river to the point the tidal bore has nearly disappeared.

South America

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Brazil

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  • Amazon River in Brazil, up to 4 meters (13 ft) high, running at up to 13 mph (21 km/h). It is known locally as the pororoca.[27]
  • Mearim River in Brazil
  • Araguari River in Brazil. Very strong in the past, it is considered lost since 2015, due to buffaloes farming, irrigation, and dam construction along the river, leading to substantial loss of water flow.

Venezuela

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Chile

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Lakes with tidal bores

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Lakes with an ocean inlet can also exhibit tidal bores.[citation needed]

North America

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  • Nitinat Lake on Vancouver Island has a sometimes dangerous tidal bore at Nitinat Narrows where the lake meets the Pacific Ocean. The lake is popular with windsurfers due to its consistent winds.
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See also

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  • 1812 New Madrid earthquake, a historic earthquake in the United States that caused the Mississippi River to flow backwards temporarily
  • Tidal race
  • Tsunami
  • Tonlé Sap, a lake and river system in Cambodia where monsoon flooding can cause the river to flow backwards temporarily, albeit not as a tidal bore

References

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  1. ^ Sometimes also known as an aegir, eagre, or eygre in the context of specific instances in Britain.
  2. ^ a b c d e Chanson, H. (2011). Tidal Bores, Aegir, Eagre, Mascaret, Pororoca. Theory and Observations. World Scientific, Singapore. doi:10.1142/8035. ISBN 978-981-4335-41-6.
  3. ^ Figure 5 in: Susan Bartsch-Winkler; David K. Lynch (1988), "Catalog of worldwide tidal bore occurrences and characteristics", USGS Report (Circular 1022), Circular, U. S. Geological Survey: 12, Bibcode:1988usgs.rept...12B, doi:10.3133/cir1022
  4. ^ Chanson, H. (2012). "Momentum considerations in hydraulic jumps and bores". Journal of Irrigation and Drainage Engineering. 138 (4). ASCE: 382–85. Bibcode:2012JIDE..138..382C. doi:10.1061/(ASCE)IR.1943-4774.0000409. ISSN 0372-0187.
  5. ^ Chanson, H. (2009). "Current Knowledge In Hydraulic Jumps And Related Phenomena. A Survey of Experimental Results". European Journal of Mechanics B. 28 (2): 191–210. Bibcode:2009EuJMB..28..191C. doi:10.1016/j.euromechflu.2008.06.004. ISSN 0997-7546.
  6. ^ a b c Chanson, H. (2009). Environmental, Ecological and Cultural Impacts of Tidal Bores, Benaks, Bonos and Burros. Proc. International Workshop on Environmental Hydraulics IWEH09, Theoretical, Experimental and Computational Solutions, Valencia, Spain, 29–30 October Editor P.A. Lopez-Jimenez et al., Invited keynote lecture, 20 pp. (CD-ROM).
  7. ^ Koch, C. and Chanson, H. (2008). "Turbulent Mixing beneath an Undular Bore Front". Journal of Coastal Research. 24 (4): 999–1007. doi:10.2112/06-0688.1. S2CID 130530635.{{cite journal}}: CS1 maint: multiple names: authors list (link)
  8. ^ Koch, C. and Chanson, H. (2009). "Turbulence Measurements in Positive Surges and Bores". Journal of Hydraulic Research. 47 (1): 29–40. Bibcode:2009JHydR..47...29K. doi:10.3826/jhr.2009.2954. S2CID 124743367.{{cite journal}}: CS1 maint: multiple names: authors list (link)
  9. ^ Chanson, H. (2009). "The Rumble Sound Generated by a Tidal Bore Event in the Baie du Mont Saint Michel". Journal of the Acoustical Society of America. 125 (6): 3561–68. Bibcode:2009ASAJ..125.3561C. doi:10.1121/1.3124781. PMID 19507938.
  10. ^ a b Simpson, J.H., Fisher, N.R., and Wiles, P. (2004). "Reynolds Stress and TKE Production in an Estuary with a Tidal Bore". Estuarine, Coastal and Shelf Science. 60 (4): 619–27. Bibcode:2004ECSS...60..619S. doi:10.1016/j.ecss.2004.03.006. during this […] deployment, the [ADCP] instrument was repeatedly buried in sediment after the 1st tidal cycle and had to be dug out of the sediment, with considerable difficulty, at the time of recovery.{{cite journal}}: CS1 maint: multiple names: authors list (link)
  11. ^ Chanson, H., Lubin, P., Simon, B., and Reungoat, D. (2010). Turbulence and Sediment Processes in the Tidal Bore of the Garonne River: First Observations. Hydraulic Model Report No. CH79/10, School of Civil Engineering, The University of Queensland, Brisbane, Australia, 97 pp. ISBN 978-1-74272-010-4.{{cite book}}: CS1 maint: multiple names: authors list (link)
  12. ^ Simon, B., Lubin, P., Reungoat, D., Chanson, H. (2011). Turbulence Measurements in the Garonne River Tidal Bore: First Observations. Proc. 34th IAHR World Congress, Brisbane, Australia, 26 June–1 July, Engineers Australia Publication, Eric Valentine, Colin Apelt, James Ball, Hubert Chanson, Ron Cox, Rob Ettema, George Kuczera, Martin Lambert, Bruce Melville and Jane Sargison Editors, pp. 1141–48. ISBN 978-0-85825-868-6.{{cite book}}: CS1 maint: multiple names: authors list (link)
  13. ^ Chanson, H., Reungoat, D., Simon, B., Lubin, P. (2012). "High-Frequency Turbulence and Suspended Sediment Concentration Measurements in the Garonne River Tidal Bore". Estuarine, Coastal and Shelf Science. 95 (2–3): 298–306. Bibcode:2011ECSS...95..298C. doi:10.1016/j.ecss.2011.09.012. ISSN 0272-7714.{{cite journal}}: CS1 maint: multiple names: authors list (link)
  14. ^ Reungoat, D., Chanson, H., Caplain, C. (2014). "Sediment Processes and Flow Reversal in the Undular Tidal Bore of the Garonne River (France)". Environmental Fluid Mechanics. 14 (3): 591–616. Bibcode:2014EFM....14..591R. doi:10.1007/s10652-013-9319-y. ISSN 1567-7419. S2CID 14357850.{{cite journal}}: CS1 maint: multiple names: authors list (link)
  15. ^ Reungoat, D., Chanson, H., Keevil, C. (2014). Turbulence, Sedimentary Processes and Tidal Bore Collision in the Arcins Channel, Garonne River (October 2013). ISBN 9781742721033. {{cite book}}: |journal= ignored (help)CS1 maint: multiple names: authors list (link)
  16. ^ a b Mouazé, D., Chanson, H., and Simon, B. (2010). Field Measurements in the Tidal Bore of the Sélune River in the Bay of Mont Saint Michel (September 2010). Hydraulic Model Report No. CH81/10, School of Civil Engineering, The University of Queensland, Brisbane, Australia, 72 pp. ISBN 978-1-74272-021-0. the field study experienced a number of problems and failures. About 40 s after the passage of the bore, the metallic frame started to move. The ADV support failed completely 10 minutes after the tidal bore.{{cite book}}: CS1 maint: multiple names: authors list (link)
  17. ^ a b Wolanski, E., Williams, D., Spagnol, S., and Chanson, H. (2004). "Undular Tidal Bore Dynamics in the Daly Estuary, Northern Australia". Estuarine, Coastal and Shelf Science. 60 (4): 629–36. Bibcode:2004ECSS...60..629W. doi:10.1016/j.ecss.2004.03.001. About 20 min after the passage of the bore the two aluminium frames at site C were toppled. […] A 3-min-duration patch of macroturbulence was observed. […] This unsteady motion was sufficiently energetic to topple moorings that had survived much higher, quasi-steady currents of 1.8 m/s.{{cite journal}}: CS1 maint: multiple names: authors list (link)
  18. ^ a b Li, Ying; Pan, Dong-Zi; Chanson, Hubert; Pan, Cun-Hong (July 2019). "Real-time characteristics of tidal bore propagation in the Qiantang River Estuary, China, recorded by marine radar" (PDF). Continental Shelf Research. 180. Elsevier: 48–58. Bibcode:2019CSR...180...48L. doi:10.1016/j.csr.2019.04.012. S2CID 155917795. The Qiantang River tidal bore was recorded at two different geographical locations. Characteristic flow patterns were derived and analysed, including temporal changes over a relatively large-scale area. The experimental results showed that the radar-derived celerity and calculated height of the tidal bore were consistent with visual observations in this estuarine zone.
  19. ^ a b c d e f g h i j Chanson, H. (2008). Photographic Observations of Tidal Bores (Mascarets) in France. Hydraulic Model Report No. CH71/08, Univ. of Queensland, Australia, 104 pp. ISBN 978-1-86499-930-3.
  20. ^ Ryan Novitra (February 3, 2017). "Riau to Introduce Bono Wave to International Tourism".
  21. ^ "Wairoa Tidal Bore". New Zealand Herald. No. 15560. 18 March 1914. Retrieved 25 November 2024.
  22. ^ p. 159, Barrie R. Bolton. 2009. The Fly River, Papua New Guinea: Environmental Studies in an Impacted Tropical River System. Elsevier Science. ISBN 978-0444529640.
  23. ^ (in French) definition of mascaret
  24. ^ Petitcodiac River changing faster than expected
  25. ^ "Surf's Up -- in Canada! Small New Brunswick Town Becomes International Surfing Hotspot". ABC News. Archived from the original on 2023-04-01.
  26. ^ Natural History of Nova Scotia Vol. I, Chap. T "Ocean Currents", p. 109
  27. ^ (in English) "Pororoca: surfing the Amazon" indicates that "The record that we could find for surfing the longest distance on the Pororoca was set by Picuruta Salazar, a Brazilian surfer who, in 2003, managed to ride the wave for 37 minutes and travel 12.5 kilometers (7.8 mi)."
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Source: Wikipedia. Article content is retrieved live through the MediaWiki API.

Wikipedia

Tidal bore

A tidal bore, often simply given as bore in context, is a tidal phenomenon in which the leading edge of the incoming tide forms a wave (or waves) of water that travels up a river or narrow bay, reversing the direction of the river or bay's current. It is a strong tide that pushes up the river, against the current.

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Wikipedia

Severn bore

The Severn bore is a tidal bore seen on the tidal reaches of the River Severn in south western England. It is formed when the rising tide moves into the funnel-shaped Bristol Channel and Severn Estuary and the surging water forces its way upstream in a series of waves, as far as Gloucester and beyond. The bore behaves differently in different stretches of the river; in the lower, wider parts it is more noticeable in the deep channels as a slight roller, while the water creeps across the sand and mudflats. In the narrower, upper reaches, the river occupies the whole area between its banks and the bore advances in a series of waves that move upstream. Near Gloucester, the advancing water overcomes two weirs, and sometimes one in Tewkesbury, before finally petering out. Bores are present on about 130 days in the year, concentrated on the days immediately following the new and full moon. The size and precise timing of the bore depend on such things as the time of high tide, the barometric pressure, the wind speed and direction, the amount of water coming down the river and how well scoured the main drainage channels are. There are a number of viewpoints from which the bore can be seen, or viewers can walk along the river bank or floodbanks. Historically, the bore has been of importance to shipping visiting the docks at Gloucester, but this was alleviated by the construction of an alternative route, the Gloucester and Sharpness Canal, which opened in 1827. Nowadays the bore is of interest to surfers and canoeists who attempt to ride the waves.

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Wikipedia

Hydraulic jump

A hydraulic jump is an abrupt increase in the depth of a fast-moving liquid stream in an open channel, which is accompanied by a decrease in speed. The jump appears as a wavy or turbulent region between the high-speed upstream flow and the slower downstream flow. A common example is the circular jump formed when a tap runs into a kitchen sink. Hydraulic jumps occur below dam spillways and in rivers. Hydraulic jumps may be stationary, as below a dam, or they may propagate as surges along a stream, as in a tidal bore. Civil engineers design spillways and stilling basins to create hydraulic jumps that dissipate the mechanical energy of water flowing over dams. A hydraulic jump can form only when the upstream flow moves faster than shallow-water waves, so that small disturbances to the flow cannot travel upstream. For speeds only slightly above the wave speed, the transition is a rolling wave. As the flow speed increases, the transition becomes more abrupt, until at high enough speeds the front breaks and curls upstream. These regimes are characterized by the ratio of upstream speed to wave speed, which is called the Froude number. Hydraulic jumps also occur in stratified flows, including in the atmosphere and the oceans. In rivers, they can create both recreational whitewater features and dangerous recirculating currents.

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Wikipedia

Pororoca

The Pororoca (Portuguese pronunciation: [pɔɾɔˈɾɔkɐ], [poɾoˈɾɔkɐ]) is a tidal bore, with waves up to 4 m (13 ft) high that travel as much as 800 km (500 mi) inland upstream on the Amazon River and adjacent rivers. It occurs at the mouth of the river where its waters meet the Atlantic Ocean. It can be observed from the islands Marajó and Caviana, and in various rivers of the state Pará.

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TOPIC OF THE DAY

Greenwood / Black Wall Street

Before the 1921 destruction of Tulsa’s Greenwood District, Black residents had created a remarkable center of business and community life. The district included stores, professional offices, entertainment venues and homes owned by Black citizens. Understanding Greenwood means learning what was built—not only what was burned.

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TRIVIA QUESTION OF THE DAY

What prosperous Tulsa district became widely known as “Black Wall Street”?

The Greenwood District.