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THE JOURNEY THROUGH TIME

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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...

Shirley Chisholm — Unbought and Unbossed

In 1968 Shirley Chisholm became the first Black woman elected to the United States Congress. In 1972 she launched a campaign for the Democratic presidential nomination, breaking another political barrier.

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Wikipedia

Tasman Front

The Tasman Front is a relatively warm water east-flowing surface current and thermal boundary that separates the Coral Sea to the north and the Tasman Sea to the south.

Naming

[edit]

The name was proposed by Denham and Crook in 1976,[1] to describe a thermal front that extends from Australia and New Zealand between the Coral Sea and Tasman Sea.[2][3]

Geography

[edit]

Originating in the edge of the East Australian Current (EAC), the Tasman Front meanders eastward between longitudes 152° E and 164° E and latitudes 31° S and 37° S,[4][5] then reattaches to the coastline at New Zealand, forming the East Auckland Current.[6]

Topography plays a dominant role in establishing the Tasman Front.[2] Data on the Tasman Front shows that the path of the front is influenced in part by the forcing of the flow over the major ridge systems.[7] Meanders observed in the Tasman Front can be driven by meridional flows along ridges such as those observed at the New Caledonia Trough (166° E) and the Norfolk Ridge (167° E). Abyssal currents also drive meanders associated with the Lord Howe Rise (161° E) and Dampier Ridge (159° E).[8]

Oceanography

[edit]

There have been a number of observational[5][7] and modeling[8][9] studies on this front in addition to a number of paleo-oceanographic studies of marine sediments.[10] Contrarily, there have been few biological observational studies, but those have been conducted resulted in relating the physical features of the front to properties of fish communities.[11] Likewise, there are even fewer studies relating biogeochemical properties to physical processes of the Tasman Front.[3]

See also

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References

[edit]
  1. ^ Denham, R. N.; Crook, F. G. (March 1976). "The Tasman front". New Zealand Journal of Marine and Freshwater Research. 10 (1): 15–30. Bibcode:1976NZJMF..10...15D. doi:10.1080/00288330.1976.9515596. ISSN 0028-8330.
  2. ^ a b Andrews, John C.; Lawrence, Martin W.; Nilsson, Carl S. (November 1980). "Observations of the Tasman Front". Journal of Physical Oceanography. 10 (11): 1854–1869. Bibcode:1980JPO....10.1854A. doi:10.1175/1520-0485(1980)010<1854:oottf>2.0.co;2. ISSN 0022-3670.
  3. ^ a b Baird, Mark E.; Timko, Patrick G.; Middleton, Jason H.; Mullaney, Thomas J.; Cox, Deborah R.; Suthers, Iain M. (November 2008). "Biological properties across the Tasman Front off southeast Australia". Deep-Sea Research Part I: Oceanographic Research Papers. 55 (11): 1438–1455. Bibcode:2008DSRI...55.1438B. doi:10.1016/j.dsr.2008.06.011.
  4. ^ Stanton, B. R. (September 1981). "An oceanographic survey of the Tasman Front". New Zealand Journal of Marine and Freshwater Research. 15 (3): 289–297. Bibcode:1981NZJMF..15..289S. doi:10.1080/00288330.1981.9515924. ISSN 0028-8330.
  5. ^ a b Mulhearn, P. J. (August 1987). "The Tasman Front: A Study Using Satellite Infrared Imagery". Journal of Physical Oceanography. 17 (8): 1148–1155. Bibcode:1987JPO....17.1148M. doi:10.1175/1520-0485(1987)017<1148:ttfasu>2.0.co;2. ISSN 0022-3670.
  6. ^ Roemmich, Dean; Sutton, Philip (1998-06-15). "The mean and variability of ocean circulation past northern New Zealand: Determining the representativeness of hydrographic climatologies". Journal of Geophysical Research: Oceans. 103 (C6): 13041–13054. Bibcode:1998JGR...10313041R. doi:10.1029/98JC00583. ISSN 2156-2202.
  7. ^ a b Stanton, B. R. (June 1979). "The tasman front". New Zealand Journal of Marine and Freshwater Research. 13 (2): 201–214. Bibcode:1979NZJMF..13..201S. doi:10.1080/00288330.1979.9515795. ISSN 0028-8330.
  8. ^ a b Tilburg, Charles E.; Hurlburt, Harley E.; O'Brien, James J.; Shriver, Jay F. (October 2001). "The Dynamics of the East Australian Current System: The Tasman Front, the East Auckland Current, and the East Cape Current". Journal of Physical Oceanography. 31 (10): 2917–2943. Bibcode:2001JPO....31.2917T. doi:10.1175/1520-0485(2001)031<2917:tdotea>2.0.co;2. ISSN 0022-3670.
  9. ^ Oke, Peter R.; Middleton, Jason H. (April 2001). "Nutrient enrichment off Port Stephens: the role of the East Australian Current". Continental Shelf Research. 21 (6–7): 587–606. Bibcode:2001CSR....21..587O. doi:10.1016/S0278-4343(00)00127-8.
  10. ^ Grant, Katharine M.; Dickens, Gerald R. (November 2002). "Coupled productivity and carbon isotope records in the southwest Pacific Ocean during the late Miocene–early Pliocene biogenic bloom" (PDF). Palaeogeography, Palaeoclimatology, Palaeoecology. 187 (1–2): 61–82. Bibcode:2002PPP...187...61G. doi:10.1016/S0031-0182(02)00508-4. S2CID 128569245.
  11. ^ Griffiths, F. B.; Wadley, V. A. (November 1986). "A synoptic comparison of fishes and crustaceans from a warm-core eddy, the East Australian Current, the Coral Sea and the Tasman Sea". Deep-Sea Research Part A: Oceanographic Research Papers. 33 (11): 1907–1922. Bibcode:1986DSRA...33.1907G. doi:10.1016/0198-0149(86)90085-3.

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Wikipedia

Tasman Front

The Tasman Front is a relatively warm water east-flowing surface current and thermal boundary that separates the Coral Sea to the north and the Tasman Sea to the south.

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Wikipedia

1968 Tasman Series

The 1968 Tasman Championship for Drivers was a motor racing series contested over eight races during January, February and March 1968, with four races held in New Zealand and four in Australia. The championship was open to Racing Cars fitted with non-supercharged engines with a capacity equal or inferior to 2500cc. It was the fifth annual Tasman Championship. The championship won by Jim Clark, driving a Lotus 49T. It was the third and final Tasman Championship win for Clark who was killed in a Formula 2 crash on the ultra fast Hockenheim circuit in West Germany just over a month after the series concluded. Clark won the last of his fifteen career Tasman Series wins when he won the 1968 Australian Grand Prix at the Sandown Raceway in Melbourne, only 0.1 seconds in front of the Dino 246 Tasmania of Chris Amon after a famous duel between the pair. Reigning 1967 Formula One World Champion Denny Hulme finished equal seventh in the series in his Formula 2 Brabham with a best finish of third in Round 3 for the Lady Wigram Trophy, his first race of the series.

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Wikipedia

Austin Kimberley

The Austin Kimberley and Austin Tasman (sold by Morris in New Zealand alongside the Austin models) "X6" models are a pair of Leyland Australia-designed front-wheel-drive sedans based on the Austin 1800 (ADO17) platform, that were produced from 1970 to 1972 and sold by Austin. At the time of the X6 being launched onto the Australian market it was quite an advanced design in comparison to the other competitors from Ford, Holden and Chrysler, whose rear-wheel drive, conventionally sprung underpinnings dominated the market at the time.

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Wikipedia

Tasman Sea

The Tasman Sea is a marginal sea of the South Pacific Ocean, situated between Australia and New Zealand. It measures about 2,000 km (1,200 mi) across and about 2,800 km (1,700 mi) from north to south. The sea was named after the Dutch explorer Abel Janszoon Tasman, who in 1642 was the first known European to cross it. British explorer Lieutenant James Cook later extensively navigated the Tasman Sea in the 1770s during his three voyages of exploration. The Māori people of New Zealand call this sea Te Moana-a-Rehua meaning 'the sea of Rehua' which clashes with the Pacific waters named Te Tai-o-Whitirea ('the sea of Whitirea') – after Whitirea, Rehua's lover – at Cape Reinga, the northernmost tip of North Island.

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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

Who became the first Black woman to travel into space?

Mae Jemison, aboard Space Shuttle Endeavour in 1992.