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Wall of piled ice on the coast of the Bay of Chaleur on the New Brunswick side. Gaspe, Quebec in the background.
The luckiest Barbie of all! Cali Girl Barbie, she had Blaine and Ken fighting over her for a time, Blaine won! and then she went back to her old love...Ken!
“Well, good for you, you look happy and healthy
Not me, if you ever cared to ask
God, I wish that I could do that
I've lost my mind, I've spent the night
Crying on the floor of my bathroom
But you're so unaffected, I really don't get it
But I guess good for you”
good 4 u is a song recorded by American singer-songwriter Olivia Rodrigo, released on May 14, 2021, through Geffen and Interscope Records, as the third single from Rodrigo's debut studio album, Sour. The song was announced on May 10 via Rodrigo's social media. It was written by Rodrigo and its producer Dan Nigro; Hayley Williams and Josh Farro are also credited as co-writers due to the inspiration from Paramore's Misery Business
Musically, good 4 u has been described as an upbeat song blending rock, pop, punk, grunge, emo, and alternative styles. It consists of a staccato bassline, energetic electric guitars, and explosive drumming, with lyrics addressing a former lover who moved on very quickly after a breakup. The song received acclaim from music critics, who praised the instrumentation reminiscent of the 1990s–2000s and Rodrigo's crisp songwriting. The accompanying music video features Rodrigo as a cheerleader exacting revenge, visually alluding to the 1990s and 2000s' cult classic films Audition, The Princess Diaries, and Jennifer's Body. At the 64th Annual Grammy Awards good 4 u received a nomination for Best Music Video.
The single reached number one in 23 different countries including Australia, Germany, Canada, Czech Republic, United Kingdom, Ireland, Latvia, and the United States; it was the second chart-topping single from Sour in many of those countries, following Rodrigo's debut single Drivers License. The single good 4 u peaked within the top 10 in more than 20 territories. en.wikipedia.org/wiki/Good_4_U
Public domain image of Olivia Rodrigo posing for a photo with President Joe Biden in the Oval Office by the White House on Wikimedia Commons w.wiki/4mXL
In Alaska, more so than elsewhere I think, we use the term “breakup” as both a noun and a verb. In the latter sense as a description of the ice going out on the rivers, which can be quite dramatic and occurs at different times depending on any number of circumstances. But we also say “Breakup” to refer to a season, in many ways its more or equally significant than “Spring.” After the calm and soft season of winter, breakup is a raucous and mad rush, as if to say there’s no time for spring, let’s get to summer straight on. Breakup is rather late this year, in fact it may be record setting late.
This is the little Chena River, a relatively small stream, the larger rivers are still mostly locked in ice. This shot was made from the Nordale Road bridge looking upstream. You will notice the ice jam up above, in populated areas near the river those things can cause some real problems.
Looking at the sunset as the sun had set on my relationship with my partner Jasmine. Goodbye my special friend. May you find happiness where you go.
The breakup of the Soviet Union left Kazakhstan with large numbers of tactical reconnaissance and strike aircraft, plus a heavy bomber regiment at Chargan Air Base near Semipalatinsk with 40 Tupolev Tu-95M5 strategic missile carrier aircraft. However, the newly-formed republic had no tactical units at all and had no use for the bombers. Wanting to keep on friendly terms with Kazakhstan so they could continue to use the Baikonur Space Centre and several military training grounds in the country, Russia exchanged the bombers for a suitable number of Su-27 and MiG-29 and Su-25 fighters from Russian Air Force stocks. By 1995, 73 combat aircraft were delivered including 38 Flankers. The Su-27s entered service with the 60th IAP in 1999 and by 2000 the Kazakhstan Air Force was reformed into the Republic of Kazakhstan Air Defence Force with aviation bases as the primary elements in its order of battle, not air regiments. The 60th IAP was transformed into the 604th AvB and stationed at Taldykorgan, with some Flankers being transferred to Qarahandy-Sary Arka International airport in order to have a more even distribution of fighters across the country.
In September 2007, the Kazakhstan Air Defence Force sent ten of its Su-27s to 558th ARZ in Baranovichi, Belarus for upgrades to the BM2 standard. The N001 radar was upgraded with the actual beam and ground mapping modes and increased its compatibility with the R-77 active radar homing AAM and the Kh-31A anti-shipping missile. The cockpit featured an EFIS with colour liquid-crystal MFDs, an enhanced navigation system, a data collection/transmission system, and data cockpit recorders. The first BM2 variant was completed in 2009. In 2015, the Kazakhstan Air Defence Force placed an order for 24 Su-30SM aircraft to replace its ageing MiG-27 Floggers.
In this image, a recently upgraded Su-27BM2 (“05 Yellow”) from the 604th AvB at Taldykorgan flies over the Kazakhstan countryside. 05 Yellow was the first Su-27 to receive the BM2 upgrades in Belarus. The new paint scheme also does away with the old Soviet-era camouflage with a dazzling dark blue, light blue, and grey pattern. Note the two B-13L rocket launchers mounted on the number 3 and 4 pylons.
Here lays my heart
All broken and torn
There are no feelings left in it
For me to mourn
Here lays my mind
Which has repressed
All the memories we have shared
That have left me a mess
Here lays my soul
Which you took away
Along with my faith and trust in you
That you broke in a day
Here lays my body
All mangled and left to die
I hope that I can get through this
And find another guy.
"Breakup" by Julie Scricco
夜的寧靜是時候好好反省
月的陰晴圓缺就像我的心
夜下著雨 天在哭泣
不知道何時才放晴
我忽然非常想念你
你的背影讓我失去了理性
你的放棄讓我迷失了自己
你的離去就像刺青
永遠烙印在我的心
是如此痛 而如此的美麗
我努力的想哭泣
卻哭不出淚滴
一次又一次的灰心
才發現早已麻痺
終於發現自己
已經不在乎你
原來分手也能如此安寧
安寧／詞：林倛玉
****************************************************************************************
To one of my fiends,
whose heart is broken.
送給一位心碎卻哭不出來的朋友。
加油，我們都在你身邊。
Horned Puffins mirror one another against a deeply shadowed cliff face. Little Tanaga Strait, Aleutian Islands, Alaska, USA.
Canon 5DM3 | Canon 400mm f/5.6 | Handheld from boat
Original Caption: View East Across Spring Flood Channels of the Lowe River These Gravel Bars, Dry During the Summer Months, Become Filled with Silty Gray Water During the Spring Melt, Or Breakup as It Is Called in Alaska. The Pipeline Will Run West Along the Lower Slopes of the Hillside Seen in the Upper Right Portion of the Picture. Mile 770-773, Alaska Pipeline Route 08/1974
U.S. National Archives’ Local Identifier: 412-DA-13230
Photographer: Cowals, Dennis, 1945-
Subjects:
Alaska (United States) state
Environmental Protection Agency
Project DOCUMERICA
strong>Persistent URL: catalog.archives.gov/id/555682
Repository: Still Picture Records Section, Special Media Archives Services Division (NWCS-S), National Archives at College Park, 8601 Adelphi Road, College Park, MD, 20740-6001.
For information about ordering reproductions of photographs held by the Still Picture Unit, visit: www.archives.gov/research/order/still-pictures.html
Reproductions may be ordered via an independent vendor. NARA maintains a list of vendors at www.archives.gov/research/order/vendors-photos-maps-dc.html
Access Restrictions: Unrestricted
Use Restrictions: Unrestricted
poster art for the february installment of an open mic series here in berkeley. art direction by joe christiano of pegasus books.
This logo for the Banana Breakup comedy improv team was on a window during the North Carolina Comedy Arts Festival in February.
Polygon Breakup explores unfamiliar techniques for achieving visual effects. In place of a standard fadeout, a recursive polygon splitting function slowly shreds the shapes.
Prints are available at www.tylerlhobbs.com/works/item/polygon-breakup.
Broken skateboard poster/sketch/messin around...
everytime you break a skateboard, you break a heart.
-These photographs were taken September 12th 2009. Funny how I reuse oldies.
-My boyfriend and I are no more.
-I haven't felt able to say it out loud/or write it down...
-It ended the last week of May... (however it wasn't clear till July...)
-I've done badly in both of the exams I took three days after we split... I'm very unhappy.
-Its taking me a long time to "get over." I'm sorry but thats just me.
-One thing that made me happy, who made me happy.... turned upside down and became a source of upset.... :'(
-It was one inspiration for "Torn."
www.youtube.com/watch?v=e0AFsMrxwJ8
-Its hard when both people feel differently.
-I didn't want to let go.... still don't want to let go. I hurt more than I let on.
-I miss everything about him... I feel so lonely now... I want him/it back...
-I'm a single girl... There. I said it. After three months... its about time.
- :'(
Mid-Atlantic Ridge South Coast Iceland
The ridge was central in the breakup of the hypothetical Pangaea that began some 180 million years ago.
The Mid-Atlantic Ridge in Iceland
The Mid-Atlantic Ridge (MAR) is a mid-ocean ridge, a divergent tectonic plate boundary located along the floor of the Atlantic Ocean, and part of the longest mountain range in the world. It separates the Eurasian Plate and North American Plate in the North Atlantic, and the African Plate from the South American Plate in the South Atlantic. The Ridge extends from a junction with the Gakkel Ridge (Mid-Arctic Ridge) northeast of Greenland southward to the Bouvet Triple Junction in the South Atlantic. Although the Mid-Atlantic Ridge is mostly an underwater feature, portions of it have enough elevation to extend above sea level. The section of the ridge which includes the island of Iceland is also known as the Reykjanes Ridge. The average spreading rate for the ridge is about 2.5 cm per year.
Plate tectonics
The tectonic plates of the world were mapped in the second half of the 20th century.
Remnants of the Farallon Plate, deep in Earth's mantle. It is thought that much of the plate initially went under North America (particularly the western United States and southwest Canada) at a very shallow angle, creating much of the mountainous terrain in the area (particularly the southern Rocky Mountains).
Plate tectonics is a scientific theory that describes the large-scale motions of Earth's lithosphere. The model builds on the concepts of continental drift, developed during the first decades of the 20th century. It was accepted by the geoscientific community after the concepts of seafloor spreading were developed in the late 1950s and early 1960s.
The lithosphere is broken up into tectonic plates. On Earth, there are seven or eight major plates (depending on how they are defined) and many minor plates. Where plates meet, their relative motion determines the type of boundary: convergent, divergent, or transform. Earthquakes, volcanic activity, mountain-building, and oceanic trench formation occur along these plate boundaries. The lateral relative movement of the plates typically varies from zero to 100 mm annually.
Tectonic plates are composed of oceanic lithosphere and thicker continental lithosphere, each topped by its own kind of crust. Along convergent boundaries, subduction carries plates into the mantle; the material lost is roughly balanced by the formation of new (oceanic) crust along divergent margins by seafloor spreading. In this way, the total surface of the globe remains the same. This prediction of plate tectonics is also referred to as the conveyor belt principle. Earlier theories (that still have some supporters) proposed gradual shrinking (contraction) or gradual expansion of the globe.
Tectonic plates are able to move because the Earth's lithosphere has a higher strength and lower density than the underlying asthenosphere. Lateral density variations in the mantle result in convection. Plate movement is thought to be driven by a combination of the motion of the seafloor away from the spreading ridge (due to variations in topography and density of the crust, which result in differences in gravitational forces) and drag, downward suction, at the subduction zones. Another explanation lies in the different forces generated by the rotation of the globe and the tidal forces of the Sun and the Moon. The relative importance of each of these factors is unclear, and is still subject to debate.
Continental Drift.
Continental drift is the movement of the Earth's continents relative to each other by appearing to drift across the ocean bed. The speculation that continents might have 'drifted' was first put forward by Abraham Ortelius in 1596. The concept was independently (and more fully) developed by Alfred Wegener in 1912. The theory of continental drift was superseded by the theory of plate tectonics, which builds upon and better explains why the continents move.
North Amercan Plate
The North American Plate is a tectonic plate covering most of North America, Greenland, Cuba, Bahamas, and parts of Siberia, Iceland and the Azores. It extends eastward to the Mid-Atlantic Ridge and westward to the Chersky Range in eastern Siberia. The plate includes both continental and oceanic crust. The interior of the main continental landmass includes an extensive granitic core called a craton. Along most of the edges of this craton are fragments of crustal material called terranes, accreted to the craton by tectonic actions over the long span of geologic time. It is believed that much of North America west of the Rockies is composed of such terranes.
Geographic extent
The easterly side of the North American Plate is a divergent boundary with the Eurasian Plate to the north and the African Plate to the south forming the northern part of the Mid-Atlantic Ridge.
The southerly boundary with the Cocos Plate to the west and the Caribbean Plate to the east is a transform fault, represented by the Cayman Trench under the Caribbean Sea and the Motagua Fault through Guatemala. The parallel Septentrional and Enriquillo-Plantain Garden faults, which run through the island of Hispaniola and bound the Gonâve Microplate, are also a part of the boundary. The rest of the southerly margin which extends east to the Mid Atlantic Ridge and marks the boundary between the North American Plate and the South American Plate remains poorly understood and undefined.
On the northerly boundary is a continuation of the Mid-Atlantic ridge called the Gakkel Ridge. The rest of the boundary in the far northwestern part of the plate extends into Siberia. This boundary continues from the end of the Gakkel Ridge as the Laptev Sea Rift, on to a transitional deformation zone in the Chersky Range, then the Ulakhan Fault between it and the Okhotsk Plate, and finally the Aleutian Trench to the end of the Queen Charlotte Fault system.
The westerly boundary is the Queen Charlotte Fault running offshore along the coast of Alaska and the Cascadia subduction zone to the north, the San Andreas Fault through California, the East Pacific Rise in the Gulf of California, and the Middle America Trench to the south.
On its western edge the Farallon Plate has been subducting under the North American Plate since the Jurassic Period. The Farallon Plate has almost completely subducted beneath the western portion of the North American Plate leaving that part of the North American Plate in contact with the Pacific Plate as the San Andreas Fault. The Juan de Fuca, Explorer, Gorda, Cocos and Nazca Plates are remnants of the Farallon Plate.
The boundary along the Gulf of California is complex. The Gulf is underlain by the Gulf of California Rift Zone, a series of rift basins and transform fault segments between the northern end of the East Pacific Rise in the mouth of the gulf to the San Andreas Fault system in the vicinity of the Salton Trough rift/Brawley seismic zone.
It is generally accepted that a piece of the North American Plate was broken off and transported north as the East Pacific Rise propagated northward, creating the Gulf of California. However, it is as yet unclear whether the oceanic crust east of the Rise and west of the mainland coast of Mexico is actually a new plate beginning to converge with the North American Plate, consistent with the standard model of rift zone spreading centers generally.[citation needed]
Hotspots
A few hotspots are thought to exist below the North American Plate. The most notable hotspots are the Yellowstone (Wyoming), Raton (New Mexico), and Anahim (British Columbia) hotspots. These are thought to be caused by a narrow stream of hot mantle convecting up the Earth's core-mantle boundary called a mantle plume, although some geologists prefer upper-mantle convection as a cause. The Yellowstone and Anahim hotspots are thought to have first arrived during the Miocene period and are still geologically active, creating earthquakes and volcanoes. The Yellowstone hotspot is most notable for the Yellowstone Caldera and the many calderas that lie in the Snake River Plain while the Anahim hotspot is most notable for the Anahim Volcanic Belt, currently found in the Nazko Cone area.
Plate motion
For the most part, the North American Plate moves in roughly a southwest direction away from the Mid-Atlantic Ridge.
The motion of the plate cannot be driven by subduction as no part of the North American Plate is being subducted, except for a small section comprising part of the Puerto Rico Trench; thus other mechanisms continue to be investigated.
One recent study suggests that a mantle convective current is propelling the plate.
** FILE ** In this Oct. 18, 2007 file photo, Mexico's band RBD presents the award for Best Pop Artist during the 2007 MTV Latin Video Music Awards at the Palacio de los Deportes in Mexico City. RBD announced on Friday, Aug. 15, 2008 that they are breaking up after fours years. (AP Photo/Gregory Bull,File)
Edited Landsat 8 image of the breakup of the large iceberg that just split away from the Larsen C ice shelf. Processing variant.
Image source: earthobservatory.nasa.gov/IOTD/view.php?id=90627
Original caption: When a massive iceberg first broke away from Antarctica’s Larsen C ice shelf sometime between July 10-12, 2017, scientists knew it would eventually start breaking apart. That’s the normal life cycle of a drifting iceberg, which is at the mercy of the ocean’s battering currents, tides, and winds. Already those forces have turned A-68 into two named bergs, A-68A and A-68B, as well as a handful of pieces too small to be named by the U.S. National Ice Center.
In the two weeks following the initial break, satellite imagery has documented the iceberg’s motion. The southern end appears to have slammed into a mix of floating ice above Gipps Ice Rise—the bump of snow- and ice-covered bedrock visible in the lower right of the image. Then the berg rebounded and its northern end swung back toward the just opened rift. The resulting impact caused both the berg’s north end and the ice shelf to fracture.
“The back-and-forth movement of A-68 looks akin to maneuvering a parallel-parked car out of a tight parking space—like an Austin Powers three-point turn,” said Christopher Shuman, a cryospheric scientist at NASA’s Goddard Space Flight Center and the University of Maryland, Baltimore County.
The fractured berg and shelf are visible in these images, acquired on July 21, 2017, by the Thermal Infrared Sensor (TIRS) on the Landsat 8 satellite. The false-color view shows the relative warmth or coolness across the region. White indicates where the ice or water surface is warmest, most notably in the widening strip of mélange between the main iceberg and the remaining ice shelf. Dark grays and blacks are the coldest areas of ice.
So far, the calving and fracturing has taken place under the dark cover of polar night during Antarctica’s austral winter. That makes thermal imagery from satellites a critical tool for “seeing” the action. Adrian Luckman of the UK-based Project MIDAS first saw the berg break away in thermal data from the Moderate Resolution Imaging Spectroradiometer (MODIS), before Sentinel radar data became available later on July 12.
The thermal view above shows a remarkable amount of detail. The bright signature of relatively warm ocean water appears around A-68B, which broke off sometime between late July 13 and early July 14. More subtle fractures north of A-68B are visible on the shelf; these pieces will eventually break free and move out to sea with the rest of the ice.
All of the ice pieces large and small are subject to the water currents of the Weddell Gyre and the strong weather systems that can whip up blinding snow and blanket the region in clouds for many days at a time. This same ocean circulation that will eventually move the bergs northward toward South Georgia Island.
In the meantime, scientists will have to wait until August—the end of polar night here—to get their first natural-color images since the long-growing Larsen C rift became a complete break.
References and Related Reading
NASA Earth Observatory, Rift and Calving at Larsen C Ice Shelf.
NASA Earth Observatory (2017, July 12) Antarctic Ice Shelf Sheds Massive Iceberg.
NASA Earth Observatory (2017, July 12) Landsat Spots Birth of Iceberg A-68.
Project MIDAS (2017, July 12) Larsen C calves trillion ton iceberg. Accessed July 12, 2017.
NASA Earth Observatory images by Jesse Allen, using Landsat data from the U.S. Geological Survey. Story by Kathryn Hansen.
Instrument(s):
Landsat 8 - TIRS
12.17 day 4
broken hearted. :[
today was going ok. other than my usual clutzy self.
than i got a phone call that changed everything. :[
the guy that i had fallen for gave me the most heart wrenching news. i never saw it coming. and ive been crying all day.
i dunno how things are going to work out :'[
</3 brenda
With all of the technology we have access to today, it can be hard to tell if our phones and computers are bringing us closer together or pulling us further apart. It turns out that they are apparently doing both! Texting and its naughtier cousin, sexting, are both popular and discreet ways to...
blog.cogxio.com/how-sexting-could-make-or-break-your-rela...
y bueno , otraves estoy asi , asi perdido , me sentia en el cielo y luego en un segundo todo se desmorona , es tan malo sentirse asi , sentir que aveces la persona que amas , aquella persona que darias todo por aserla felis , te traicione. bueno asi es todo , todos es una real y pura mentira , en este mundo lleno de odio es dificl encontrar el amor y no se como fui tan imbecil para sentir que estoy duraria para siempre , odio esta vida , odio este mundo , odio existir pero no puedo odiarte a ti . en fin aun queda algo y ojala no se acabe porque es lo que me ase seguir . nose comolo aras para recuperame pero costara y no sera facil.
tu eras todas las cosas que yo creia conocer y pensaba que podriamos ser . tu eras todo , todo lo que yo queria , lo que debiamos ser se suponia que eramos pero lo perdimos , todos nuestros recuerdos , tan cercanos a mi se desvanecen .
todo este tiempo estabas aparentando . aun falta mucho para mi final feliz .
es bonito saber que estuviste ahi , gracias por atctuar como si te importara y hacerme sentir como si fuera el unico . es bonito saber que lo tuvimos todo gracias po mirar como caigo y hacerme saber que habiamos terminado
“i’m leaving you” she said as a matter of factly…meghan was sitting beside me at the bar…she had turned slightly so we were almost facing each other…
“why ?” I was a bit surprised, ok a lot surprised at this turn of events…
“i’m bored and I need a change…this relationship is ok but it’s always the same…we never do or try anything differently…”
“i thought we were doing ok, so what is it you want to do…”
“i don’t know…like I said I’m bored…maybe if I kind of wandered for a while…maybe…”
“is it something sexual…some different position you want to try…a different technique…maybe some toys…how about a menage…maybe one of your friends would like to join us…beth? sandra?...i’d like that too !...a lot…”
“yea you would…maybe if you thought about me for once…how about one of your friends…gary or ted…I’ve noticed the way they look at me…I could do either one...or both..."
“touche…well if you’ve made up your mind, how about one for the road?...maybe I can change your mind…”
“ok…but I don’t think anything you’ve got left is going to change my mind…if you want to try and I know you do let’s go to your place…that way I can leave after we’re done…”