Paul Newman Passed Away

The world lost a formidable talent yesterday. Iconic actor Paul Newman passed away at his home in Westport, Conn from cancer. He was 83.

When you used the words "movie star", Newman is the guy you meant. He had a career that spanned several decades, from Cat on a Hot Tin Roof in 1958 all the way up to Road to Perdition in 2002.

Newman also owned a food company, Newman's Own, in which all the money has gone to charity. The company has donated over $200 million so far.

He's survived by his actress wife Joanne Woodward, and five children. About Woodward, Newman was once asked if he would ever cheat on her.

"Why would I go out for a hamburger when [I] have steak at home?" he asked. Dude was a man's man, and a class act.

And I must say, I recently saw Cat on a Hot Tin Roof, and Mr. Newman was a sexy mf back in the day. Hey, I'm being tributey!

Click on any image in the gallery for ten more photos of Paul Newman and his illustrious career.



Photo Credit: WENN
Website: www.photo.wenn.com

4 Comments

What a terrible loss! It's really sad that he is gone!
I will always remeber all of his perfermences!
"Raindrops keeps falling on my head..."
Goodbye Mr Newman!

September 27, 2008 10:23 AM

Sorry to see such a wonderful human being pass on. Paul Newman was "hot" just by the virtue of his character...the facade was just a bonus. Blessing to his family -- he will live on in our hearts.

September 27, 2008 3:16 PM

Mr. Newman ruled in Road to Perdition.

Vanity Fair had a great article about Paul and his wife Joanne in the last issue. Well worth the read. It was intimate without being exploitative.

*Sigh* A great loss, Socialites.

Talented, classy, extremely charitable. There won't be another like him.

October 26, 2008 8:21 PM


D6 28.8200 141.6200 9 DIVE, nets, CTDThe rift is also surmounted by a series of three extensive coral terraces at 1150, 400 and 150-m depths. These coral terraces correlate with dated terraces at similar depths on the west side of the island that are 15, 125, and 425 thousand years old (summary in Moore and Clague, 1992). Several additional terraces between the 125 and 425 ka terraces present on the west side of the island are missing here. The terraces drowned during sea level fluctuations when sea level rose faster than the reefs could grow at the onset of interglacial periods during the Pleistocene. Confirming that the reefs are indeed correlated correctly with those from the west side of the island is critical to determining the subsidence of the island and whether Hawaii has tipped significantly. In addition, a small reef terrace at about 380-m depth is evident in the bathymetry, but is never modelled, suggesting that the sea level variation curves for the Pleistocene-the best record of long-term climatic change-have smoothed out some real sea level fluctuations. Collection and dating of samples from this reef would allow us to determine when this sea level fluctuation took place.Vibra peeper corer (if functional)/li>D2, 67-75 35.9530 123.8420 9 DIVE, nets, CTDEK-500 water column profiling system Ц Robison (continuous use during transit)а Live Lesbian Sex Webcams Equipment Description (include weight if available):67-90 35.4530 124.9030 9 DIVE, nets, CTD2 steel tow fish + block + pump, 350lbs
D8 24.7800 152.3800 9 DIVE, nets, CTDCruise History and BackgroundFrench-fry basket scoopExpedition Chief Scientist: David ClaguePurpose: Gay Mexican Men Having Sex D6 28.8200 141.6200 9 DIVE, nets, CTD4 sets of scuba gear (including weights, no tanks) - Robison ~200 lbs total1 incubator - Chavez. ~200 lbsа
Equipment Description (include weight if available):67-85 35.6200 124.5500 2 CTD, nets D3,Benthic sled with manipulatorThis Hawaii expedition is multidisciplinary in nature and the various legs reflect the diversity of interests and objectives. In addition to the geological objectives listed below, MBARI is also utilizing the transit times both to Hawaii (Leg 1) and back to Monterey (Leg 5).D8 24.7800 152.3800 9 DIVE, nets, CTD Free Lesbian Toy Sex Leg 4: Lava flows (May 9-18)Planned Track Description:We request four 12-hr Tiburon dives to observe and collect lava and coral samples from the cones and terraces outlined above. The 400-m terrace is partly overrun by subsequent lavas from Mauna Kea Volcano, whereas the 1150-m terrace has some small cones from an unknown volcano built on top. One dive will collect both the corals and the lavas draping the 400 and the 380-m terraces and another will attempt to sample the 1150-m terrace, where prior dredging (two attempts) failed to recover coralline material. Two dives will explore several of the flat-topped and pointed cones along the deeper (>2000-m) part of the rift. The impact glass sampler will be used here since the lavas have only thin (1 mm) Mn-oxide crusts (as seen in the few dredged samples from the rift) and the box corer should also be useful.
This proposal requests 28 Tiburon dive days, admittedly a large number of dive days. Most of these dives will include benthic biology observations and some biological sampling with Jim Barry and George Matsumoto as successfully done on Pioneer, Guide, Gumdrop, Taney, and Davidson Seamounts in 2000. Hawaii is the primary study area for Clague, as it has been for nearly 30 years. The Western Flyer will return to Hawaii no sooner than 2004, so this expedition will provide the data for several years of lab analysis and writing. All but two of the dives proposed are within areas surveyed with the Simrad EM300 system in 1998, so excellent basemaps are in hand.This cruise will address topics as diverse as formation of karst topography in drowned reefs to dynamics of submarine basaltic eruptions and formation of volcanic landforms to hydrothermal circulation and geochemistry. Dives are planned to address the interplay of volcanism and reef formation on Mahukona and Kohala (Hilo Ridge) Volcanoes, formation of pointed volcanic cones, flat-topped volcanic cones, and lava ponds on Haleakala, Kilauea, and Koolau Volcanoes, the structure of folded volcanicalstic rocks along the margin of the Hilina slump at Papa'u Seamount, eruption dynamics of fire fountains and explosive eruptions at Loihi Seamount, long-term changes in the hydrothermal system at Loihi Seamount, and formation of karst topography i drowned coral reefs on Mahukona Volcano.2 steel tow fish + block + pump, 350lbsScheduled End Dateа: 2001-03-28 1830 Local Moss Landing timeBox corer Gay Men Sex with Animals Winch with conducting wire for CTD net casts & tow fish -Chavez & Johnsonаtop of pagePlastic storage shed, 6x6x3 ft, w/ table - Chavez ~200 lbsа
2 steel tow fish + block + pump, 350lbstop of pagePlanned Track Description:top of pageMidwater Acoustic Current Meter (ACM) - Robisonа Hot International Lesbian Sex David Clague, Marcia McNutt, Kelsey Jordahl, Jennifer Reynolds (U. of Alaska), Jackie Dixon (U. of Miami), Jenny Paduan, Alice Davis, Brian Cousens (Carlton U., Canada), Ed Seidel (MBA), Ken Hon (U. of Hawaii, Hilo), Nancy Jacobsen-Stoutgravity corer and rock crusher for night operationsаD2, 67-75 35.9530 123.8420 9 DIVE, nets, CTD
D8 24.7800 152.3800 9 DIVE, nets, CTDC1 36.7960 121.8500 0.25 Surface sample only1 Air compressor - Johnson ~200 lbsPurpose:Planned Track Description: Preteen Lesbian Sex Stories Benthic sled with manipulatorExpedition Principal Investigator:аKen JohnsonDavid Clague, Marcia McNutt, Kelsey Jordahl, Jennifer Reynolds (U. of Alaska), Jackie Dixon (U. of Miami), Jenny Paduan, Alice Davis, Brian Cousens (Carlton U., Canada), Ed Seidel (MBA), Ken Hon (U. of Hawaii, Hilo), Nancy Jacobsen-Stout
67-65 36.2870 123.1300 2 nets, CTD67-90 35.4530 124.9030 9 DIVE, nets, CTD1. Loihi SeamountTo investigate submarine canyons and associated features located along the flanks of the Hawaiian Islands. We will examine mid-canyon plunge pools, walls and canyon heads to ascertain processes that are actively shaping these canyons. In addition, we will investigate submerged coral reefs and carbonate platforms to determine age and origin. Rocks samples, rock cores, sediment push cores and scoop samples will be collected. We are also interested in establishing whether waters are actively flowing through the submerged flanks of the islands. Fresh waters associated with the islands may be discharging do to the hydraulic head on the adjacent island. In addition, geothermal heating may stimulate seawater flow cells within the flanks of the island. We will obtain in situ data consisting of radium and conductivity measurements, pore waters from cores, and samples to establish diagenetic signatures associated with paleo-flow. We anticipate a 14-hour dive days. Some dives will be in shallow waters (100-300 m deep) where a dive day may have two or more dives. Nighttime operations will consist of taking CTD casts not to extend past 0100 the following dive day. Transit to the next days dive site will be done during the nighttime, non-scientific operational hours.SHIP/ROV GEAR Ц Free Gay Sex Movie Trailers Chilled Seawater System and Cold Room Ц RobisonThe cruise will depart Honolulu at 8 am an May 9 and transit 56 nm to dive 5/9 site, arriving about 1:30-2 pm. A short dive will be done on a small volcanic cone at about 700 m depth that had an anomaly in the water column above the cone when mapped in Dec. 2000. The anomaly is most likely either magmatic gas bubbles or a hydrothermal plume and suggests that the cone may be recently or currently active. This dive should be completed by 8-9 pm. Following a 25 nm transit to the first of McNutt's 2 dive targets on the north slope of Oahu, several gravity cores would be collected during the night. Dive 5/10 would use the heat flow probe and collect 60-cm cores using the vibra-peeper device. This dive will be at about 3400-3460 m depth. Night operations will consist of gravity coring and a short (4 nm) transit to dive 5/11, a second dive to collect heat flow data and 60-cm cores for conductivity measurements. Night operations will consist of gravity coring and a 45 nm transit to dive site 5/12. Dive 5/12 is the deepest dive on the entire Hawaii expedition, starting at 3925 m and ending at 3560 m, all on a group of young volcanic cones and flows in the channel between Oahu and Kauai. Night operations will consist of gravity coring and a 27 nm transit to the south flank of Kauai, where dive 5/13 will sample a series of volcanic vents related to the rejuvenated-stage lavas on Kauai, the Koloa Volcanics. Night operations will consist of gravity coring and a 46 nm transit to dive 5/14, located on the northwest flank of Niihau. This dive will start at 3220 m depth and end at about 1630 m and survey and sample a series of flat-topped volcanic cones. Night operations will consist of gravity coring and a 15 nm transit to dive 5/15. Dive 5/15, also on the northwest flank of Niihau, will survey and sample several additional flat-topped cones and a pointed volcanic cone near the northwest rift zone on Niihau between 2720 and 1910 m depth. Night operations will consist of gravity coring and a 12 nm transit to the third and final dive on Niihau. Dive 5/16 will survey and sample more of the flat-topped cones including one with a perched lava pond at its summit. The dive will start at 1680m and work up to 1260 m depth. Night operations will consist of gravity coring followed by a 47 nm transit back to the south flank of Kauai and dive 5/17. This dive will sample a series of volcanic cones near those of dive 5/13. Night operations will consist of gravity coring followed by a 27 nm transit to the final dive site in the channel between Oahu and Kauai. Dive 5/18 will probably need to start earlier than normal in order to complete the dive in time to transit the 78 nm to Honolulu to arrive by 5 pm. The dive is at about 2960 m depth, but is relatively short.WF Rosette/CTD (+ our mini rosette, 150lbs.)
Participants:Expedition Chief Scientist: Bruce Robison7. Hilo RidgePapaТu Seamount is a large mound located along the southwest transverse margin of the active Hilina Slump on Kiluaea (Moore et al., 1989). It was originally though to be a sandy debris flow derived from collapse of a shoreline lava delta. Interpretation of recently collected seismic data and MBARIТs Simrad bathymetry indicate that it is a coherent west-vergent fold developed along an east-dipping fault that defines the southwestern boundary of the mobile south flank of Kilauea Volcano (Morgan et al., submitted). Our analysis of the structures in this region suggests that the main thrust fault is exposed along the western flank of PapaТu Seamount and that we should be able to map the fault zone and determine the lithologies of the rocks both above and below the thrust. The formation of PapaТu Seamount is a key to understanding the formation and structure of the entire Hilina Slump and in understanding the formation of giant landslides in Hawaii. Results from some of the Kaiko and Shinkai dives elsewhere in the Hilina slump have found submarine-erupted alkalic and transitional basalts indicative of the earliest (Loihi) stage of volcano growth (Naka et al., 2000). The locations of the proposed PapaТu dives are stratigraphically between these early (deep) lavas and lavas more typical of present-day Kilauea. The chemistry of samples from these dives will help constrain the volume of this early alkalic-tranistional stage in the development of Hawaiian volcanoes.Equipment Description (include weight if available): Painful and first anal sex porn TRACE METAL: Ginger Elrod (female), and Steve FitzwaterScheduled End Dateа: 2001-03-28 1830 Local Moss Landing timePlanned Track Description:

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