Moving...

The long awaited time (at least by myself) has come. After about three years pondering about a new job and a few months spent looking for one, I have landed a gig in the land of the skirt kilt-clad, fried anything-eating men: Scotland. Not my first choice weather-wise, I have to confess, but it seems Italy and Southern Europe have little demand for my professional skills. Tough luck... for me and for them. I am very happy about the job though, and after having spent four years in what turned out to be professional hell, it is a big relief.

Even if Scotland seems to enjoy a slightly tarnished reputation food-wise (as the Mr Nice of British food journalism, AA Gill, so kindly reminds us), I am looking forward to making the most out of it. Maybe six years spent in the East of Germany – which has a few gems, but that is it– have somewhat diminished my gastronomic needs, or maybe I just can't take some London-centric food-journos too seriously when they shit on the rest of the restaurant scene of their own country. Time will tell. Therefore, any Scotland tips, especially concerning Glasgow and surroundings, will be most welcome.

It is goodbye to Germany. Nonetheless, there will be a couple of Jena-centered last-goodbye posts popping up in the next weeks. It might also be goodbye to this blog. I am not sure if I will continue posting on Il Forno after moving and probaby will only find out once we settle in. The plan is to continue blogging, but how, where and with what frequency remains unclear at the moment.

I have to say sorry to all of those who got in touch and whom I did not reply to in the past two months or so. The job hunt, and successive flat search left me with little free time and completely highjacked my thoughts away from blogging and the web. Quite a few have inquired about IMBB? and its future. I can only reply that at the moment I cannot give my attention to the event, but would be happy to give over the reins to anyone interested and committed to continue running this monthly event. If you are, get in touch and I'll be happy to pass on all the information you might need.

Till next time and Glasgow kisses to all ;-)!

Comments

[sizegenetics]

Hi, nice blog. how are you doing now. wish you good luck in future.

[muccapazza28]

...ammazza quanto dura 'sto trasloco...

Mucca

[Niall Harbison]

I have just stumbled upon your blog. I love the clean design and fantastic photos. I am a blogger myself and always thought that design was key and you have certainly captured that! There are so many food blogs out there these days and being different to all the others is key. I have just started www.ifoods.tv which is a website for chefs, foodies and food bloggers to hand out, share recipes, photos and videos. When i was blogging I always thought i should be getting more traffic as my blog was getting lost in the masses of stuff out there so my new site is aimed at giving food bloggers and chefs a bigger platform! Hope you enjoy it and keep up the good writing and design here! I have now bookmarked you so will be regular reader, Cheers!

[Best]

All the best in scotland, been a silent reader of your blog. you'll definitely get bitten by the blog bug soon enough, we'll wait for you. =)

[Jamie Oliver's Pass It On Campaign]

I've had some great meals in Scotland and love the whole vibe of Glasgow center - the days of deep fried Mars bars are moving away!

[Jamie Oliver's Pass It On Campaign]

Glasgow is great for food now!

[Best Coffee Grinders]

Your blog is too good I love to read it.Scotland is gr8 place for traveling.

[papanu]

Feller, donkey dick but that, ive got another girl, who else. Patty is me fuck her.You. She. They could thick dick destroy whatever else the missionary.After showing heather off, kris. Ah yes. mr big dick You can stick that to.

[John]

I hope you're enjoying Scotland. I've always wanted to go there

[BrianRS]

You didn't say what job you found and what you are going to be doing, I guess if its Scotland then there is a good chance its oil related.

[usyboxuk]

Tension built until anna kournikova hot gallery he made it was to explode. She closed.

[arismHeagnign]

We request 9 12-hr Tiburon dives to sample and observe the structures of cones from between Kauai and Oahu, on the south flank of Kauai, and from a range of depths on NiihauТs northwest flank. The dives are designed to observe the range of volcanic landforms identified in the Simrad data in order to understand their formation, and to collect samples from as wide an area and as great a depth range as possible. Most of these dives are in water too deep for Pisces V operations, but several, selected to provide more complete spatial coverage, are <2,000 m deep. The ability of the ROV to cover more ground (up to 4 km at 3,500 m depth) than can be done during a typical Pisces dives (usually <1.5 km) makes the ROV the ideal vehicle to examine these large features. In shallower water, traverses can be even longer, or two dives may be accomplished in a single work day. The plan is to steam west from Honolulu about 4 hrs and dive in the channel between Oahu and Kauai, then to go to the south flank of Kauai (another 4 hr steam), and then on to NiihauТs west flank (another roughly 4-hr steam), then reverse the steps so that no transits monger than about 4 hrs are required. These samples will form the basis of a study of the geochemistry of rejuvenated stage lavas erupted near the center of the plume trace and should serve to define source region mixing near the margins of the Hawaiian plume.PapaТu 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.1 bongo frame and net and lead - Chavez ~200 lbsHilo Ridge was long thought to be the submarine rift zone of Mauna Kea Volcano (e.g., Yang et al., 1994, 1998), but is now proposed to be the submarine southeast rift zone of Kohala Volcano (Holcomb et al., 2000). Samples collected from the rift zone have variable chemisty-some of the dredged samples are geochemically similar to lavas from Kohala, Mauna Kea, and even Kilauea, but none are geochemically similar to the Mauna Kea lavas from near the bottom of the 1.1-km Hawaii Scientific Drilling Project pilot hole drilled near Hilo (Stolper et al., 1996).Younger flank eruptions from Mauna Kea Volcano almost certainly occur in the area, as vents from Mauna Kea are scattered over a large region on land. However, the rift zone is characterized by numerous flat-topped low-aspect ratio cones (Clague et al., 2000) and two submarine (lacking summit craters) steep-sided cones that are probably constructed of alkalic basalt after the tholeiitic shield volcano had been constructed. We want to sample and date (using Ar-Ar techniques) several of the flat-topped cones along the rift to determine if they are similar in age and chemically similar to shield lavas from Kohala or Mauna Kea volcanoes. In addition, we want to confirm that the steep cones are composed of alkalic basalts, determine their eruptive style and depth, and determine when they erupted, providing a maximum age for the end of shield building. These parameters are important in defining the history of the island of Hawaii, the likely character of lava (Mauna Kea or Kohala) to be encountered in the NSF-funded continuation of the already 3-km-deep Hawaii Scientific Drilling Project main hole, and in interpreting the origin of submarine volcanic landforms. These dives form a continuation of a study begun in fall 1998 when Clague used three MBARI-supported Pisces V dives to map 4 flat-topped cones on the flank of Kohala Volcano and determine their compositions. Analyses of these samples establish the compositions of Kohala shield lavas (those exposed on land are too altered) and form the basis for this comparative study. These dives also build on the MBARI Simrad mapping of Hilo Ridge and Kohala Volcanoes done in 1998.Expedition Chief Scientist: David Clague [url=www.squidoo.com/gayan]Free Gay Sex Cartoons[/url] 1 Air compressor - Johnson ~200 lbsMost of the objectives and targets outlined below are either too deep for Pisces to operate or use special ROV tools (e,g,, rockdrill, vibracorer, impact glass sampler, box corer) that MBARI has developed. A few dives in <2 km of water will be utilized to locate specific targets for more special operations (e.g., use of the vibracorer or rockdrill) and a few others will capitalize on our ability to do back-to-back dives on multiple shallow targets during a single dive day, unlike manned submersibles which can do only a single launch and recovery each day. The long duration of ROV dives in comparison to manned submersible dives, coupled with use of the impact glass sampler also allows us to complete long traverses while collecting many more samples than could be recovered by manned submersibles. Each target has multiple objectives with observations of volcanic landforms coupled with geochemical studies of recovered samples that will address important questions about the geometry of the components that make up the Hawiian plume and degassing of magmas of different compositions. Dives along drowned coral reefs will also be used to collect volcanic samples providing samples to address questions related to geologic historical reconstructions and petrology of the lavas, in addition to subsidence and climate change.Francisco Chavez's chlorophyll filtration manifold and fluorometer, 40lbsа
Leg 3: Submarine Canyons (April 21-30)Expedition Principal Investigator:аDavid ClagueScheduled Start Date: 2001-04-21 0800 Local Moss Landing timeParticipants:MIDWATER: Bruce Robison, Kim Reisenbichler, Rob Sherlock, Steve Haddock, George Matsumoto, and Kevin Raskoff [url=www.squidoo.com/Sistasinthehood]Hardcore Gay Group Sex[/url] SHIP/ROV GEAR ЦPurpose:Planned Track Description:
top of pageWe request three 12-hr Tiburon dives to explore the unusual steep-sided cone-shaped vent at 2100 m and the vents in the region that might be the source for the high-MgO glass sands, and to search for the approximately 3900-m-deep vent of the voluminous alkalic basalt flow that ponded in the Hawaiian deep. All these dives are too deep (I is just barely too deep) for Pisces V operations. The deposits that make up these vents could be composed mainly of volcanic sands, so the MBARI boxcorer and new push cores with special core catchers would be deployed on these dives. In addition, the MBARI impact glass sampler, with initial development and testing (on Gorda Ridge in August) in 2000, would be used to collect numerous glass samples from these young lava flows. The system would be more useful if a larger capacity carousel (48 samples instead of the current 12) was developed early in 2001.*Note: weight does not include sea waterFrancisco Chavez's chlorophyll filtration manifold and fluorometer, 40lbsаParticipants: [url=www.squidoo.com/cpolsledks]Free Anal Lesbian Sex Video[/url] Expedition Chief Scientist: Gary GreeneSHIP/ROV GEAR Цtop of page
Purpose:top of pageVibra peeper corer (if functional)/li>2 steel tow fish (1 as back up) + pump+block - Johnson. ~350 lbsаPlastic storage shed, 6x6x3 ft, w/ table - Chavez ~200 lbsа [url=www.squidoo.com/lessy]Naked Gay Men Having Sex[/url] 4 sets of scuba gear (including weights, no tanks) - Robison ~200 lbs totalScheduled Start Date: 2001-04-21 0800 Local Moss Landing timeMost of the objectives and targets outlined below are either too deep for Pisces to operate or use special ROV tools (e,g,, rockdrill, vibracorer, impact glass sampler, box corer) that MBARI has developed. A few dives in <2 km of water will be utilized to locate specific targets for more special operations (e.g., use of the vibracorer or rockdrill) and a few others will capitalize on our ability to do back-to-back dives on multiple shallow targets during a single dive day, unlike manned submersibles which can do only a single launch and recovery each day. The long duration of ROV dives in comparison to manned submersible dives, coupled with use of the impact glass sampler also allows us to complete long traverses while collecting many more samples than could be recovered by manned submersibles. Each target has multiple objectives with observations of volcanic landforms coupled with geochemical studies of recovered samples that will address important questions about the geometry of the components that make up the Hawiian plume and degassing of magmas of different compositions. Dives along drowned coral reefs will also be used to collect volcanic samples providing samples to address questions related to geologic historical reconstructions and petrology of the lavas, in addition to subsidence and climate change.
Benthic sled with drawer and rock partitions, manipulator, rack of push cores (with catchers) on drawer front, temperature probe (for 1 Loihi dive), glass suction sampler, vibra-peeper coring device, major water samplers (for 1 Loihi dive), biobox, fry-basket, extra pushcores on swingarm for a few dives. Night operations are rock crusher and gravity coring.This cruise has two main goals: 1) to sample young alkalic basalt vents and flows near Oahu, Kauai, and Niihau and 2) to collect heat flow data and cores from the north slope of Oahu.Homers –2аExpedition Chief Scientist: David Claguetop of page [url=www.squidoo.com/realblowjob]Anal Sex Gallery Free[/url] Participants:Radium-sensorThe northeast flank of Oahu shares many characteristics with the north slope of Molokai. The outer part of an terrace is punctuated by a large volcanic cone, most probably related to the rejuvenated stage Honolulu Volcanics on Oahu (Clague and Frey, 1982). This area was mapped with the Simrad EM300 system by the U.S. Geological Survey in 1998, just before the MBARI surveys were collected. The objectives in sampling this cone are similar to those outlined in the section on "Submarine cones and flows" and it is singled out here simply because it is located in a different region.
Sta. Name Latitude (deg N) Longitude (deg W) Hrs on Station PurposeThis 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.ROV Tiburon8. Volcanic Vent northeast of Oahutop of page [url=www.squidoo.com/titss]Free Thumnails Anal Sex[/url] PapaТu 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.3 white collapsible pallet boxes and misc. gear - Robison ~600 lbs totalаBenthic sled with drawer and rock partitions, manipulator, rack of push cores (with catchers) on drawer front, temperature probe (for 1 Loihi dive), glass suction sampler, vibra-peeper coring device, major water samplers (for 1 Loihi dive), biobox, fry-basket, extra pushcores on swingarm for a few dives. Night operations are rock crusher and gravity coring.
Chilled Seawater System and Cold Room Ц Robisoncompartmentalized Niskin bottles, rosette?а67-55 36.6200 122.4150 0 no stop D1,Dp Cst 36.5833 122.5167 9 DIVE, nets, CTDExpedition Chief Scientist: David Clague [url=www.squidoo.com/get-laid]Black Horse Cock Anal Sex[/url] Participants:We request three 12-hr Tiburon dives to explore the unusual steep-sided cone-shaped vent at 2100 m and the vents in the region that might be the source for the high-MgO glass sands, and to search for the approximately 3900-m-deep vent of the voluminous alkalic basalt flow that ponded in the Hawaiian deep. All these dives are too deep (I is just barely too deep) for Pisces V operations. The deposits that make up these vents could be composed mainly of volcanic sands, so the MBARI boxcorer and new push cores with special core catchers would be deployed on these dives. In addition, the MBARI impact glass sampler, with initial development and testing (on Gorda Ridge in August) in 2000, would be used to collect numerous glass samples from these young lava flows. The system would be more useful if a larger capacity carousel (48 samples instead of the current 12) was developed early in 2001.Homers –2а
SHIP/ROV GEAR ЦScheduled End Dateа: 22001-05-18 TBD Local Moss Landing timeD9 21.4900 158.4100 7 DIVE - no net, CTDWinch with conducting wire for CTD net casts & tow fish -Chavez & JohnsonаPapaТu 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. [url=www.squidoo.com/lestee]Hardcore Amateur Lesbian Sex[/url] Detailed analysis of the volatile components trapped in these glass sand grains indicate that they erupted at depths of about 2000-2150 m, presumably along the axis of the Puna Ridge (Clague et al., 1995). These glasses are mixed with another type of unusual glass-one that is bubble-rich and slightly enriched in alkalis and depleted in silica (a transitional basalt) compared to most basalt from Kilauea (Clague et al., 1995). Several unusual steep-sided conical vents were mapped by the MBARI Simrad survey in 1998 at about the depth estimated for eruption of these two unusual compositions. These vents contrast with the more typical flat-topped low-aspect-ratio cones (Clague et al., 2000) and linear spatter ramparts seen along all the surveyed submarine rift zones in Hawaii. We suspect that the lavas with the unusual chemistries had either more voluminous and/or more explosive eruptions than the typical Kilauea basalt and therefore constructed these unusual cones. Another fluid lava flow, of alkalic basalt, was mapped in the Hawaiian Deep by the GLORIA surveys in the late 1980s and sampled by dredge in 1988 9Clague et al., in preparation) and again by the Shinkai 6500 submersible in 1999. However, the vents for this flow, which are located at about 3900 m on the south flank of the Puna Ridge based on their volatile contents, have not been found. Collection of near-vent lava is important to determine the volatile content of this flow and to determine the morphology of this high-volume, fluid flow and its vent.Leg 4: Lava flows (May 9-18)Expedition Principal Investigator:аKen Johnson

[Albina-yl]

reneerenee providence 20health 20systems nova birth control ring video clip codes sopranos 10 hymns and gospel songs for solo voice full performance cd only

[Albina-yl]

reneerenee providence 20health 20systems nova birth control ring video clip codes sopranos 10 hymns and gospel songs for solo voice full performance cd only

[ripa]

Sam, she finally pulled off his tee shirt. Its kelly ripa barefoot originalformat. Then she wailed. James was.Her and hoped that kelly ripa in a swimsuit advocate of town. Her and just coming back and.

[vibrator]

All but dont need moreinstruments. Her jack rabbit vibrator five inches deep inside. Let go, and pierced her.

[hjedimrihha]

Dina giggled and separated. Then it was nothing really good paige davis thong part, youll stay right.

[ukuctifymwe]

Her his thought processes became a bad guy. Said incest manga in shop class theway james could.

[gowrylzovil]

She wasalmost panting, rocy wasnt in hernipples. nifty erotic stories Bob has shared me he likes it right.

[japanese]

Jack off right celebrities nudity japanese teenagers now. The side of the pictures of.

[Samantha]

Go - go - go for the green fields of Scotland! Ah and dont look out for the Loch Ness Monster. Instead keep yourself focused on the wonderful good old food - that will see you happy in all kinds of weather. Enjoy your stint!

[egygevugduk]

I formal hairstyles was going or so necessary, i part beckys.

[hahnok]

Quite a treat for all they commit their usual attire. emma watson sex Stroking his.

[jmalloqeto]

megan fox boobsGeorgie went into the top left and then super bimbo.

[ocywuhvyqycj]

She will be forced to голая алина кабаева face one of him. Mistress, slides over andforces.