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The Case for Democracy
An international report released on July 2 reiterated the key role democracy plays in improving the quality of life for people trapped in poverty in the Middle East.
The document stated that "the wave of democracy that transformed governance in most of Latin America and East Asia in the 1980s and early 1990s has barely reached the Arab states. This freedom deficit undermines human development."
It noted the lack of opportunity for Arab women, the lack of a voice for intellectuals who might disagree with the government, the failure to institute a free press, and a dearth of political rights for Arab citizens. The report also made a direct connection between the lack of liberty in the Arab world and the fact that Arab countries fall far behind many other nations in education, income level, and other measures of achievement.
The most interesting thing about this document is not its impressive conclusions, however, but its authors. It was co-written by the Arab Fund for Economic and Social Development, which the New York Times identified as "a group of distinguished Arab intellectuals."
This is an encouraging sign - and an opportunity that should be seized upon by the United States.
For more than two centuries, America has been the world's loading democracy - and its leading supporter around the world. By and large, democratic nations have demonstrated that they are the most peaceful, boast the healthiest economies, lead the world in a trove of scientific and medical achievements, and have the most stable system of government.
In a world where an increasing number of people are encouraged by radicals to hate the West, it is no longer enough for America to serve as democracy's role model. We must also be its champion. As Woodrow Wilson once characterized America's involvement in the First World War as an effort "to make the world safe for democracy," today, in our war against terror, President Bush must take the opportunity to demonstrate that democracy is the key to remaking a safer world.
The President understands this. And his policy toward Afghanistan -- where the oppressive
Taliban tyranny was replaced with a fledgling democracy under Hamid Karzai - is one example of that. Bush's latest enunciation of administration policy regarding the Israeli-Palestinian conflict is another. By rightfully tying U.S. support for a Palestinian state to free and fair leadership elections by the Palestinian people, the President hopes to build a democracy in place of the discredited and corrupt Arafat regime.
As the President said in June, "If liberty can blossom in the rocky soil of the West Bank and Gaza, it will inspire millions of men and women around the globe who are equally weary of poverty and oppression, equally entitled to the benefits of democratic government."
This call for democracy must also accompany our determination to oust the brutal dictatorship in Iraq. Saddam Hussein masterminded the invasion of a peaceful neighbor, plotted the attempted assassination of a U.S. President, and ordered that chemical weapons be used against his own people. There is no question that he must go.
But the administration understands that it is not enough for the United States to simply dispatch one brutal dictatorship and replace it with another. What comes after Saddam Hussein must be better. Remaking Iraq into a peaceful democracy would be an ambitious task, particularly in a culture where democracy has no long-standing tradition. But the benefits of such an undertaking would be equally enormous: Iraq would serve as a model for the rest of the Arab world, and stand as a testament to the West's commitment to a better life for the Arab people.
This is how we should see the new push for democracy: not simply as a strategic interest, but also a moral imperative to improve the lives of people across the globe.
President Bush sums this view up best: "Prosperity and freedom and dignity are not just American hopes, or Western hopes. They are universal, human hopes. America believes those hopes have the power to transform lives and nations."
That is a fitting mission for a great nation at the start of a new millennium.
- Arizona National Guard assists Navajo Nation
- Curfew takes effect for Navajo Nation as COVID-19 cases reaches 128
- Businesses in Winslow shut down as COVID-19 fears empty shelves
- $2 trillion stimulus package provides COVID-19 funds for tribes
- Navajo student comes home to Navajo Nation after school at Duke and DC
- Authorities investigating deaths of 2 Ohio men in Arizona
- Member of the Navajo Nation tests positive for COVID-19 coronavirus
- SRP suspends NGS Decommissioning in response to COVID-19
- Arizona governor issues stay-at-home order effective Tuesday
- Navajo Nation reports 69 positive COVD-19 cases, 20 more than previous day
- Member of the Navajo Nation tests positive for COVID-19 coronavirus
- Navajo County Public Health Officials Announce Presumptive COVID-19 Case in Navajo County
- Bashas' reservation stores change hours to support elders
- Arizona National Guard assists Navajo Nation
- Winslow closures as of March 20
- Tribes make preparations for COVID-19, no reported cases on Hopi and Navajo land
- Businesses in Winslow shut down as COVID-19 fears empty shelves
- 27-year-old woman's body identified after being found by camper near Sunset Crater National Monument
- Navajo student comes home to Navajo Nation after school at Duke and DC
- Navajo Nation declares Public Health State of Emergency for COVID-19 coronavirus
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Justin Bieber
Justin Bieber
Canadian singer-songwriter
Justin Drew Bieber is a Canadian singer, songwriter and actor. Discovered at 13 years old by talent manager Scooter Braun after he had watched his YouTube cover song videos, Bieber was signed to RBMG Records in 2008. Wikipedia
Born: March 1, 1994 (age 26 years), St. Joseph's Hospital, London, Canada
Full name: Justin Drew Bieber
Spouse: Hailey Rhode Bieber (m. 2018)
Parents: Pattie Mallette and Jeremy Bieber
Yummy · 2020
Intentions · 2020
I Don't Care
I Don't Care · 2019
Sorry (Latino Remix) · 2015
All I Want For Christmas Is You
Merry Christmas · 1994
10,000 Hours
10,000 Hours (Piano) · 2019
Love Yourself
Love Yourself · 2015
What Do You Mean?
Purpose · 2015
R&B In The Mix 2010 · 2010
As Long as You Love Me
As Long As You Love Me (Remixes) · 2012
Purpose · 2015
Never Say Never
My Worlds (Japan "Special Edition") · 2009
Beauty and a Beat
Believe Acoustic · 2013
Changes · 2020
Eenie Meenie
My Worlds (Japan "Special Edition") · 2009
One Time
My Worlds (Japan "Special Edition") · 2009
Boyfriend · 2012
One Less Lonely Girl
My Worlds (Japan "Special Edition") · 2009
Love Me
My Worlds (Japan "Special Edition") · 2009
Journals · 2013
Come Around Me
Changes · 2020
I'll Show You
Purpose · 2015
Under the Mistletoe · 2011
That Should Be Me
My Worlds (Japan "Special Edition") · 2009
Somebody To Love
My Worlds (Japan "Special Edition") · 2009
Get Me
Get Me · 2020
All That Matters
Journals · 2013
Running Over
Changes · 2020
Never Let You Go
My Worlds (Japan "Special Edition") · 2009
Friends (Remix) · 2017
U Smile
My Worlds (Japan "Special Edition") · 2009
Second Emotion
Changes · 2020
Seattle, WA
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Greensboro Coliseum Complex
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PPG Paints Arena
Bryce Jordan Center
Columbus, OH
Ohio Stadium
Louisville, KY
KFC Yum! Center
People also search for
People also ask
How many siblings does Justin have?
How old are Justin Bieber's siblings?
Does Justin Bieber have any full siblings?
Who is Justin Bieber's brother?
Meet Justin Bieber's Siblings: Allie, Jazmyne, Jaxon, and Bay
https://www.distractify.com › Entertainment
Sep 27, 2019 · Justin Bieber has four siblings — Allie, Jazmyn, Jaxon, and Bay. Justin's parents were never married. In fact, his dad, Jeremy Bieber, and mom, Pattie Mallette, separated just a few months after he was born. Jeremy went on to date his ex-girlfriend, Erin Wagner, in 2007, and the couple was together for seven years.
Jan 27, 2020 · It is through his father's subsequent relationships that Justin does have some half -siblings and a stepsibling. Jeremy and Erin were together from ...
Justin Drew Bieber is a Canadian singer, songwriter and actor. Discovered at 13 years old by ... Through his father Jeremy, Bieber has three younger half-siblings. Jeremy and his ex-girlfriend Erin Wagner, who broke up in 2014 after seven ... Early life · Career · Artistry Labels: Island; Teen Island; RBMG; School Boy; Def Jam Years active: 2007–present Instruments: : Vocals; drums; guitar; Home town: Stratford, Ontario, Canada
Justin Bieber Introduces New Baby Sister Bay Bieber - Justin New ...
https://www.elle.com › culture › celebrities › justin-bieber-baby-sister-bay-...
Aug 16, 2018 · In a testament to how much can change in a very short amount of time, Bieber took Selena Gomez as his date then. Bieber has two other half- ...
Justin Bieber: Inside The 'Yummy' Singer's Family Relationships ...
https://www.capitalfm.com › 2020-tour-yummy-wife-hailey-baldwin-sister
Feb 13, 2020 · Justin Bieber: Inside The 'Yummy' Singer's Family Relationships, From His Wife Hailey Baldwin To His Parents & Siblings. 13 February 2020 ...
Turns Out Justin Bieber Has A Secret Sister You Never Knew About ...
https://www.capitalfm.com › justin-bieber › secret-sister-sibling-photoshop
Apr 19, 2018 · We know Justin Bieber has two siblings, Jaxon and Jazmyn and one on the way, but did you know he has a secret sister that looks just like him ...
Justin Bieber's lookalike half-brother Jaxon, nine, poses with their ...
https://www.dailymail.co.uk › tvshowbiz › article-7521647 › Justin-Biebers...
Sep 30, 2019 · Jaxon posed with his younger half-sibling Bay, one years old, in a snap he captioned: 'Love my sister.' Jaxon is the third child of Jeremy Bieber.
Justin Bieber has a new baby half-sister; see pictures of Bay Bieber
https://www.usatoday.com › story › life › music › 2018/08/16 › justin-bieb...
Aug 16, 2018 · Justin Bieber has a new sibling, half-sister Bay Bieber, born Thursday to Jeremy Bieber and his wife Chelsey. Papa Bieber took to social media ...
Jan 3, 2019 - Justin Bieber's Brother & Sister | Jaxon Bieber & Jazmyn Bieber || 2019 - YouTube.


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Tibetan Cranial Public Clinic
Saturday, February 29, 2020, 7:00 PM - 12:15 AM
"Tibetan Cranial® is holding a Public Clinic in Denver, Colorado on Saturday, February 29 & Sunday, March 1, 2020 at the Co-Op at 1st. This is a great opportunity to get an experience of the Tibetan Cranial work and see what it is all about. Our Apprentices will begin the session and receive instruction from Shar Lee, Teacher Interns, and other Practitioners during the session. Shar or a Practitioner will personally finish each session. You will meet our Apprentices and have an opportunity to set future appointments. To schedule your 45 minute Tibetan Cranial® session for only $35, you can sign-up and prepay online or pay $40 at the door. More details about this event. Learn more about Tibetan Cranial®. Contact us at firstname.lastname@example.com with any questions.
Tibetan Cranial® (TC) is an ancient healing art designed to promote our innate capacity for self-healing. It uses subtle touch to the head, face, palate, jaw, and neck, based on a sophisticated assessment of pulses. Many people have reported pain reduction as well as relief from a wide variety of symptoms, including headaches, migraines, back and neck discomfort, whiplash, anxiety, head injury, concussion, stress-related conditions, TMJ pain, depression, nervous-system related issues, and many other health problems."
Please use the following website to schedule your 45 min session:
Cost: Use the following website to schedule your clinic time: https://www.signupgenius.com/go/20f0a44afab22a3f85-denver Cost is $35 (by 2/26) and $40 at the door.
5045 West 1st Avenue
Denver, CO 80219


text:
Sheikh Mohamed Bin Zayed honours Dr Adnan Pachachi in Abu Dhabi. File
His Highness Sheikh Mohamed Bin Zayed Al Nahyan, Crown Prince of Abu Dhabi and Deputy Supreme Commander of the UAE Armed Forces, expressed his deepest regret with loss of Dr Adnan Pachachi, who passed away on Sunday.
Sheikh Mohamed Bin Zayed condoles martyrs families
Mohamed Bin Zayed spends quality time with grandchildren
Sheikh Mohamed took to Twitter and said, "We have lost a dear man and a true friend… He has worked with Sheikh Zayed sincerely since the beginning of the Union, and contributed his experience to the noble attitudes in the delivery of the voice of the UAE to the world… May God have mercy on Dr Adnan Pachachi and grant him place in paradise, and provide patience and solace to his family."
The Ministry of Presidential Affairs has mourned the death of Pachachi.
In a statement issued today, the Ministry expressed sincere condolences, asking Allah Almighty to rest his soul in Paradise and grant his family the patience and solace to bear this loss.
The extraordinary response by the participants showed the humility exhibited by the visionary leaders of the UAE.
His Highness Sheikh Mohamed bin Zayed Al Nahyan, Crown Prince of Abu Dhabi and Deputy Supreme Commander of the UAE Armed Forces, yesterday received at Qasr Al Bahr the participants in the meetings of the International Council on Archives and Forum of National Archivists.
The approval of this instalment for Emirati citizens in Abu Dhabi stems from the leadership's commitment to ensure social stability, enhance living standards and provide the citizens with all their needs to enable them to be active contributors to the development of their community.
Human beings hate 'not knowing', yet no innovation ever begins with 'knowing', Dr Beau Lotto told a lecture hosted at the Majlis Mohamed bin Zayed on Monday, in the presence of His Highness Sheikh Mohamed bin Zayed Al Nahyan, Crown Prince of Abu Dhabi and Deputy Supreme Commander of the UAE Armed Forces.
Two specially equipped high-speed trains carried 36 patients from Mulhouse and Nancy to hospitals along France's western coast, where the outbreak has been limited so far.
Brought forward by Trump at the outdoor briefing, Fauci said his projection of a potential 100,000 to 200,000 deaths is "entirely conceivable" if not enough is done to mitigate the crisis.
Over the next 10 days, test centres will open in Dubai, Sharjah (which will also serve Ajman and Umm al Qaiwain), Ras Al Khaimah, Fujairah, Al Ain and Al Dhafra.


text:
Want some magic done on your writing?
Request writing or editing by emailing me.
Every business is different, so I cannot sell the same "packages" to you as what I might be selling to other businesses.
You have a unique brand, voice, and style (not to mention, product or service) that requires 100% customization of your strategy and content.
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text:
"Excellent hotel. Close to parking areas. Great rooms and fantastic service. Great pool."
"Accessible parking. Friendly service. Spacious rooms. Clean rooms."
Great location
Good location.
Hotel description
The hotel comprises a total of 26 rooms. Services and facilities at the hotel include a baggage storage service, a restaurant, a bar, room service, a laundry service and a conference room. Wireless internet access is available to travellers in the public areas. Those arriving in their own vehicles can leave them in the car park of the establishment. , Each of the rooms is appointed with a bathroom. Cots are available for younger guests. All rooms offer a fridge, a mini fridge and a safe. Amenities in the bathrooms include a shower. Special family rooms are available for families with children. , The accommodation offers attractions including sport and entertainment opportunities. The hotel features a pool and an outdoor pool. The establishment offers a sauna (for a fee) to travellers. Copyright GIATA 2004 - 2019. Multilingual, powered by www. Giata. Com for client no. 125642
Information about the type of meals included in the price is indicated in the rate details.
Children and information about extra beds
Fee for an extra bed: 20.00 EUR per night. The number of extra beds depends on the room category. You must take a look at the information about the size of the selected room.
Extra info
A cleaning tax is not included in the reservation price and is payable separately at the hotel.
Food & Drink
Health & Fitness


text:
Year 9 Science
Activities to support your learning
Year 9 science planner
Use this planner to help you organise the work that you should be completing over the coming weeks.
You need to log on to Educake using your log in. Complete the tasks that have been set up for you even if the tasks aren't assigned by your teacher. To create your own quizzes select "set yourself a test" select the topic that you want to revise and set the number of questions you want to complete.
Sign up to the website using your own email address. Click "I'm a student" and search for "Carr Manor" and select our school. This should take you to a page saying welcome to either Year 7 revision or Year 8 revision, then click on start assignment. Read through the information the website is giving you and answer the questions.
BBC Bitesize
Use this website (exam board OCR Gateway - combined Science) for revision and quizzes.
CPG worksheets
Use the CPG worksheets, which are separated into Biology, Chemistry and Physics, to aid with your revision.
Use the following revision broadsheets and complete as much as you can:
Sending your work to your teacher
You can send either a file (eg. a Word file or PowerPoint file) or a photograph of your handwritten work to your teacher.
You can send your message from any email account - it doesn't have to me your school account.
Make sure you include your name and your teacher's name in the subject of the email.
Send your email to:
Your teacher will then reply to you on the email address you emailed them from, so please make sure you are checking your emails.
If you need help with this, please click here.


text:
Welcome to the award winning Clapham Restaurant, located in the historic Kingston Theatre Hotel.
Set the in the heart of Hull's historic old town, the hotel overlooks the Kingston Square Gardens and is opposite the Hull New Theatre.
At the Clapham restaurant, were passionate about delivering delicious food made ingredients of the highest quality. Our restaurant combines contemporary and classic dining, which with our extensive fine wine menu makes every meal feel like a special occasion. We have Lunch, Dinner and Sunday Lunch menus available to choose from.
Why not try our traditional afternoon tea for two? With white glove service and a delicious range of finger sandwiches, cakes and drinks its the perfect way to spend an afternoon or celebrate a special occasion!
For larger parties, weddings and corporate events, our function room is available and ready to make your next special occasion a memorable one!


text:
Cruise EW9903 of the Maurice Ewing sailed from Panama to San Diego in March and April 1999, with goals of determining the structure of oceanic crust formed at superfast spreading rates and conducting site survey work in support of Joint Oceanographic Institutions for Deep Earth Sampling (JOIDES) proposal 522. Three survey grids were collected in the Guatemala Basin at sites formed at spreading rates >200 mm/yr (Wilson, 1996), and one grid was collected in the Alijos Rocks area west of Baja California (Figs. F1, F2). This report presents basic data bathymetry, magnetics, and gravity data for all of the grids and migrated multichannel seismic reflection (MCS) sections for the Guatemala Basin sites. Seismic refraction results will be reported separately (Harding et al., unpubl. data).
We analyze four expanded spread profiles acquired at distances of 0, 2.1, 3.1, and 10 km (0–0.2 m.y.) from the axis of the East Pacific Rise between 9° and 10°N. Velocity-depth models for these profiles have been obtained by travel time inversion in the τ-p domain, and by x-t forward modeling using the WKBJ and the reflectivity methods. We observe refracted arrivals that allow us to determine directly the uppermost crustal velocity structure (layer 2A). At the seafloor we find very low Vp and VS/Vp values around 2.2 km/s and ≤ 0.43. In the topmost 100–200 m of the crust, Vp remains low (≤ 2.5 km/s) then rapidly increases to 5 km/s at ∼500 m below the seafloor. High attenuation values (Qp < 100) are suggested in the topmost ∼500 m of the crust. The layer 2–3 transition probably occurs within the dike unit, a few hundred meters above the dike-gabbro transition. This transition may mark the maximum depth of penetration by a cracking front and associated hydrothermal circulation in the axial region above the axial magma chamber (AMC). The on-axis profile shows arrivals that correspond to the bright AMC event seen in reflection lines within 2 km of the rise axis. The top of the AMC lies 1.6 km below the seafloor and consists of molten material where Vp ≈ 3 km/s and VS = 0. Immediately above the AMC, there is a zone of large negative velocity gradients where, on the average, Vp decreases from ∼6.3 to 3 km/s over a depth of approximately 250 m. Associated with the AMC there is a low velocity zone (LVZ) that extends to a distance no greater than 10 km away from the rise axis. At the top of the LVZ, sharp velocity contrasts are confined to within 2 km of the rise axis and are associated with molten material or material with a high percentage of melt which would be concentrated only in a thin zone at the apex of the LVZ, in the axial region where the AMC event is seen in reflection lines. Away from the axis, the transition to the LVZ is smoother, the top of the LVZ is deeper, and the LVZ is less pronounced. The bottom of the LVZ is probably located near the bottom of the crust and above the Moho. Moho arrivals are observed in the profiles at zero and at 10 km from the rise axis. Rather than a single discontinuity, these arrivals indicate an approximately 1-km-thick Moho transition zone.
From the marine refraction data recorded on five instruments during the Clipperton Area Seismic Survey to investigate Compensation (CLASSIC) experiment in 1994 we construct a compressional velocity model for a 108 km long profile across the Clipperton transform. We apply a new seismic tomography code that alternates between ray tracing and linearized inversions to find a smooth seismic velocity model that fits the observed refraction travel times. The solution to the forward ray-tracing problem is a hybrid of the graph (or shortest path) method and a ray-bending method. The inversion is performed with least squares penalties on the data misfit and first derivatives of the seismic structure. Starting with a one-dimensional compressional velocity model for oceanic crust, the misfit in the normalized travel time residuals is reduced by 96%, decreasing the median travel time residual from 110 to 25 ms. The compressional velocity structure of the Clipperton transform is characterized by anomalously low velocities, about 1.0 km/s lower than average, beneath the median ridge and parallel troughs of the transform domain. The low compressional velocities can be explained by an increased porosity due to fracturing of the oceanic crust. We found crustal thicknesses of 5.6-5.9 km under the transform fault to produce the best fit of the PmP phase arrivals and Pg/Pn crossovers. Since the crust is not thin beneath the transform parallel troughs and the velocity anomaly is not confined to the median ridge, we find uplift by serpentinite diapirs unlikely as an explanation for the relief of the median ridge. A median ridge that is the result of brittle deformation due to compression across the transform domain is, however, compatible with our results. The upper crust is thicker to the north of the transform than to the south, which is likely a consequence of the contrast in temperature structure of these two spreading segments.
The shortest path method (SPM) is a robust ray-tracing technique that is particularly useful in 3-D tomographic studies because the method is well suited for a strongly heterogeneous seismic velocity structure. We test the accuracy of its traveltime calculations with a seismic velocity structure for which the nearly exact solution is easily found by conventional ray shooting. The errors in the 3-D SPM solution are strongly dependent on the choice of search directions in the "forward star," and these errors appear to accumulate with traveled distance. We investigate whether these traveltime errors can be removed most efficiently by an SPM calculation on a finer grid or by additional ray bending. Testing the hybrid scheme on a realistic ray-tracing example, we find that in an efficient mix ray banding and SPM account for roughly equal amounts of computation time. The hybrid method proves to be an order of magnitude more efficient than SPM without ray bending in our example. We advocate the hybrid ray-tracing technique, which offers an efficient approach to find raypaths and traveltimes for large seismic refraction studies with high accuracy.
A three-dimensional (3-D) seismic refraction study of the Clipperton transform fault, northern East Pacific Rise, reveals anomalously low compressional velocities from the seafloor to the Moho, We attribute this low-velocity anomaly to intensive brittle deformation, caused by transpression across this active strike-slip plate boundary. The seismic velocity structure south of the Clipperton transform appears unaffected by these tectonic forces, but to the north, seismic velocities are reduced over 10 km outside the zone of sheared seafloor. This contrast in seismic velocity structure corresponds well with the differences in mid-ocean ridge morphology across the Clipperton transform. We conclude that the amount of fracturing of the upper crust, which largely controls seismic velocity variations, is strongly dependent on the shallow temperature structure at the ridge axis. Intermittent supply of magma to the shallow crust north of the Clipperton transform allows seawater to penetrate deeper, and the cooler crust is brittle to a greater depth than south of the transform, where a steady state magma lens is known to exist. The crustal thickness averages 5.7 km, only slightly thinner than normal for oceanic crust, and variations in Moho depth in excess of similar to0.3 km are not required by our data. The absence of large crustal thickness variations and the general similarity in seismic structure imply that a steady state magma lens is not required to form normal East Pacific Rise type crust. Perhaps a significant portion of the lower crust is accreted in situ from a patchwork of short-lived gabbro sills or from ductile flow from a basal magma chamber as has been postulated in some recent ophiolite studies.
[ 1] Multichannel seismic reflection data collected in July 2002 at the Endeavour Segment, Juan de Fuca Ridge, show a midcrustal reflector underlying all of the known high-temperature hydrothermal vent fields in this area. On the basis of the character and geometry of this reflection, its similarity to events at other spreading centers, and its polarity, we identify this as a reflection from one or more crustal magma bodies rather than from a hydrothermal cracking front interface. The Endeavour magma chamber reflector is found under the central, topographically shallow section of the segment at two-way traveltime (TWTT) values of 0.9 - 1.4 s ( similar to 2.1 - 3.3 km) below the seafloor. It extends approximately 24 km along axis and is shallowest beneath the center of the segment and deepens toward the segment ends. On cross-axis lines the axial magma chamber (AMC) reflector is only 0.4 - 1.2 km wide and appears to dip 8 - 36 degrees to the east. While a magma chamber underlies all known Endeavour high-temperature hydrothermal vent fields, AMC depth is not a dominant factor in determining vent fluid properties. The stacked and migrated seismic lines also show a strong layer 2a event at TWTT values of 0.30 +/- 0.09 s ( 380 +/- 120 m) below the seafloor on the along-axis line and 0.38 +/- 0.09 s ( 500 +/- 110 m) on the cross-axis lines. A weak Moho reflection is observed in a few locations at TWTT values of 1.9 - 2.4 s below the seafloor. By projecting hypocenters of well-located microseismicity in this region onto the seismic sections, we find that most axial earthquakes are concentrated just above the magma chamber and distributed diffusely within this zone, indicating thermal-related cracking. The presence of a partially molten crustal magma chamber argues against prior hypotheses that hydrothermal heat extraction at this intermediate spreading ridge is primarily driven by propagation of a cracking front down into a frozen magma chamber and indicates that magmatic heat plays a significant role in the hydrothermal system. Morphological and hydrothermal differences between the intermediate spreading Endeavour and fast spreading ridges are attributable to the greater depth of the Endeavour AMC and the corresponding possibility of axial faulting.
The southwest margin of the Gulf of California has an array of active normal faults despite this being an oblique-divergent plate boundary with spreading centers that localized deformation along the plate boundary 2-3 million years ago. The Carrizal and Centenario faults form the western border fault of the Gulf of California marginal fault system within and south of La Paz Bay, and similar to 20-30 km west of the capital city of La Paz, Baja California Sur, Mexico. Geologic and geomorphic mapping, optically stimulated luminescence (OSL) geochronology, and paleoseismic investigations onshore, compressed high-intensity radar pulse (CHIRP) profiling offshore, and analysis of uplifted marine terraces in the footwall of the offshore Carrizal fault provide some of the first numerical and geometrical constraints on late Pleistocene-Holocene faulting along the Carrizal fault. The onshore Carrizal fault has ruptured with up to similar to 1-2 m of vertical displacement per event, likely producing similar to M 6.3-6.9 earthquakes, and at least two to three surface rupturing earthquakes have occurred since 22 ka. Onshore paleoseismic excavations and uplifted marine terraces on the western side of La Paz Bay both suggest offset rates of 0.1-0.2 mm/yr, with a footwall uplift rate of 0.13 mm/yr since 128 ka, and an approximately constant rate since marine oxygen-isotope stage (MIS) 11 terraces (420 ka). A CHIRP survey identified underwater fault scarps with heights ranging from 21 to 86 m on the Carrizal fault in La Paz Bay and from 3 to 5 m along the Centenario fault. The offshore Carrizal fault lies 8-10 km east of the western edge of La Paz Bay, forming a right step from the onshore Carrizal fault. The offshore Carrizal fault is the oldest fault of the fault system, and the fault likely grew in the latest Miocene to Pliocene in a complex way to the south toward the onshore Centenario and Carrizal faults. When the Alarcon spreading center started its modern rates at 2.4 Ma, the Carrizal fault likely slowed to the 0.1-0.2 mm/yr rates of the late Quaternary determined in this study.
We analyzed 25,675 traveltime residuals from a three-dimensional seismic tomographic inversion to investigate crack-induced seismic anisotropy in the upper oceanic crust. The study covered two regions with contrasting levels of magmatic activity on the western limb of the 9 degrees N overlapping spreading center on the East Pacific Rise. The level of anisotropy gradually decreases with depth in the magmatically and hydrothermally active ridge region. In contrast, we observed a highly variable anisotropic structure in the magmatically and hydrothermally less active tip region at the end of the dying ridge segment: a weakly anisotropic layer beneath strongly anisotropic extrusive volcanic rocks is likely to be the result of relatively shallow cracks closed by hydrothermal precipitation. Strongly anisotropic dikes with inferred narrow and water-saturated cracks provide important along-axis pathways for the circulation of hydrothermal fluids beneath the shallow cracks in the less magmatically active regions. Furthermore, a significant clockwise rotation (20 degrees -30 degrees ) of fast directions occurs in both regions with increasing depth. Such a rotation provides evidence that the geometry of the underlying crack structure of the western limb is significantly different from that defined by the bathymetric ridge crest.
A new three-dimensional tomographic velocity model and depth-converted reflection images of the melt sills beneath the 9degrees03'N overlapping spreading center on the East Pacific Rise show that the upper crustal construction at this ridge discontinuity is highly asymmetric with reference to the bathymetric ridge crests of the overlapping limbs. Despite the similarly curved ridge crests, the asymmetries are markedly different under the two limbs and appear to be related to the contrasting evolutionary history of the limbs. The overlap basin is closely related to the propagating eastern limb in terms of its seismic structure. By contrast, the western limb forms a distinct morphologic region that displays little structural relationship to the adjacent overlap basin and other relict basins. As the overlapping spreading center is migrating southward, the differential development of melt sills and ridge crests may be inferred from the results of this study. Ridge propagation appears to involve two major processes: the advancement of the melt sill at the ridge tip and the development of ridge-crest morphology and the neovolcanic axis to the north of the overlap basin region near the existing propagating limb. The latter process may result in the abandonment of the current neovolcanic axis, leading to the self-decapitation of the propagating limb. By contrast, the self-decapitation of the western limb is related to the receding melt sill, which lags behind the anticlockwise rotational motion of the ridge crest.
Our results from seismic anisotropy analyses reveal for the first time the complex spatial variability of the characteristics of subsurface tectonic structures associated with ridge propagation. The significance lies in the fact that these variations are found at a locality with few lineaments or fissures at seafloor level. The overlap region between mid-ocean ridge segments at 9 degrees N on the East Pacific Rise is characterized by aligned cracks that are structurally more closely related to the propagating-ridge segment. These aligned cracks, which are approximately parallel to the ridge segments, provide conclusive observational evidence for establishing the nontransform nature of overlapping spreading centers, especially those with overlap basins covered by volcanic edifices. The aligned cracks of the 9 degrees 03'N overlapping spreading center are more similar to the ridge-parallel lineaments observed between overlapping axial-summit collapse troughs than those found at larger overlapping spreading centers. Our results therefore suggest that the lithospheric deformation between overlapping ridge segments depends on ridge offset and that this dependency may be thermally related.
[1] We present a three-dimensional upper crustal model of the 9degrees03'N overlapping spreading center (OSC) on the East Pacific Rise that assists in understanding the relationship between melt sills and upper crustal structure at a ridge discontinuity with enhanced melt supply at crustal levels. Our P wave velocity model obtained from tomographic inversion of similar to 70,000 crustal first arrival travel times suggests that the geometry of extrusive emplacement are significantly different beneath the overlapping spreading limbs. Extrusive volcanic rocks above the western melt sill are inferred to be thin ( similar to 250 m). More extensive accumulation of extrusives is inferred to the west than to the east of the western melt sill. The extrusive layer inferred above the eastern melt sill thickens from similar to 350 ( at the neovolcanic axis) to 550 m ( to the west of the melt sill). Volcanic construction is likely to be significant in the formation of ridge crest morphology at the OSC, particularly at the tip of the eastern limb. On the basis of our interpretation of the velocity model, we propose that enhanced magma supply at crustal levels at the OSC may provide an effective mechanism for the migration of ridge discontinuities. This "dynamic magma supply model'' may explain the commonly observed nonsteady migration pattern of ridge discontinuities by attributing this to the temporal fluctuations in melt availability to the overlapping spreading limbs.
Spreading segments of the Mid-Atlantic Ridge show negative bull's-eye anomalies in the mantle Bouguer gravity field. Seismic refraction results from 33-degrees-S indicate that these anomalies can be accounted for by variations in crustal thickness along a segment. The crust is thicker in the center and thinner at the end of the spreading segment, and these changes are attributable to variations in the thickness of layer 3. The results show that accretion is focused at a slow-spreading ridge, that axial valley depth reflects the thickness of the underlying crust, and that along-axis density variations should be considered in the interpretation of gravity data.
A wide-aperture profile along the ridge axis from 14 degrees 29'S to 13 degrees 39'S, 120 km to 30 km south of the Garrett Fracture Zone, is analyzed to constrain the thickness of layer 2a and the depth to the axial magma chamber reflector. Five areas along the 90 km line are examined in detail, with several consecutive gathers being analyzed for each area to establish the degree of consistency within each area. A genetic algorithm code is used to find a best fit model from a comparison of the data and WKBJ synthetic seismograms. One hundred starting models are generated using a predefined set of velocity nodes, with a fixed window of allowable depth variations between nodes. An evolutionary process favors the better fitting models in each generation, and a satisfactory misfit is usually obtained within 40 generations. Within individual areas the models were in good agreement with the depth of a given velocity node, generally varying by not more than 20 m, the depth discretization interval for the models. A consistent deepening trend of the axial magma chamber (AMC) is observed across the five areas as the Garrett Fracture Zone is approached. The depth varies from 0.99 km at area 1, which is approximately 100 km south of the Garrett, to 1.23 km at area 5, which is approximately 40 km south of the Garrett. The depth to the axial magma chamber is highly sensitive to any ship wander off axis since layer 2a thickens rapidly off axis with age. For the areas examined here, layer 2a is observed to be relatively constant in thickness along the axis, although it is about 40 m thicker over area 5, where the axial magma chamber is deepest. This variation is within the scatter of previously detailed layer 2a measurements at 13 degrees N on the East Pacific Rise, where an effectively constant thickness is observed. This implies that layer 2a thickening is not a significant factor along this profile and that the AMC deepening is rear rather than apparent. Theoretical modeling suggests that the depth to the lid of the axial magma chamber is related to the rate of heat supply at a given location. Thus the gradual consistent deepening of the axial magma chamber can be taken as an indication of a slightly reduced magma supply toward the Garrett Fracture Zone, which marks a major interruption of hundreds of kilometers of continuous ridge axis. The deepening may also be interpreted as: a downward limb from a central injection point; however, there is no indication of a similar downward trend in the other (southern) direction. Furthermore, there is no accompanying systematic variation in axial depth or axial volume, both of which are proposed to be indicators of central injection and along-axis flow.
A method is presented for reducing travel time data from multiple offset borehole seismic experiments to velocity-depth structure. The technique, which treats simultaneously data from any number of depths in the borehole in addition to surface data, is based on the linear inversion scheme of Dorman and Jacobson (1981). Given the parameters ζ(p) = T(p) + pX(p) and τ(p) = T(p) − pX(p), the method solves for depth to specified slownesses, assuming linear gradients (in velocity) between slowness values. A practical limitation on the use of surface travel time measurements to resolve velocity-depth structure is the necessity of assuming a surface velocity. This is not necessary for the case of borehole data. For a borehole receiver the velocity at the depth of the receiver can be obtained from the slope of the inflection point of the travel time curve. Thus a direct measure of the uppermost velocity of a section can be obtained from the travel time data of a shallow borehole receiver. Estimation of velocities from the inflection points of deeper receivers improves the resolution of the velocity-depth function, which would be obtained from surface data alone. The technique is applied to data from three borehole seismic experiments in oceanic crust. The experiments were carried out in the western Atlantic (crustal age ∼110 m.y.), the Gulf of California (crustal age ∼1 m.y.) and the Costa Rica Rift Area (crustal age ∼6 m.y.). All three experiments show relatively high upper crustal velocities ( >4.0 km/s), suggesting that layer 2A is not present even in the very young crust. All sites had over 100 m of sediment thickness, and it is postulated that sediment thickness and sediment permeability, not merely age, govern the velocity of the upper crust by accelerating the cementation of fractures and cracks.
The first three-dimensional (3-D) seismic reflection survey of a mid-ocean ridge was shot in 1997 and, while it is still too early for firm interpretations of the data, it can be confirmed that significant crustal melt bodies have been located and one widely accepted model does not seem to apply to the presence of a robust magma supply there. The survey the Anatomy of a Ridge-Axis Discontinuity (ARAD) experiment, was centered over an overlapping spreading center (OSC) system that offsets the ridge axis at 9 degrees 03' north latitude on the East Pacific Rise (EPR) (Figure 1). It was conducted aboard the R/V Maurice Ewing during September and October and included a coincident 3-D crustal seismic tomography experiment.
The determination of melt distribution in the crust and the nature of the crust - mantle boundary ( the 'Moho') is fundamental to the understanding of crustal accretion processes at oceanic spreading centres. Upper-crustal magma chambers have been imaged beneath fast- and intermediate-spreading centres(1-4) but it has been difficult to image structures beneath these magma sills. Using three-dimensional seismic reflection images, here we report the presence of Moho reflections beneath a crustal magma chamber at the 9 degrees 03' N overlapping spreading centre, East Pacific Rise. Our observations highlight the formation of the Moho at zero-aged crust. Over a distance of less than 7 km along the ridge crest, a rapid increase in two-way travel time of seismic waves between the magma chamber and Moho reflections is observed, which we suggest is due to a melt anomaly in the lower crust. The amplitude versus offset variation of reflections from the magma chamber shows a coincident region of higher melt fraction overlying this anomalous region, supporting the conclusion of additional melt at depth.
A full-waveform inversion of two-ship, wide-aperture, seismic reflection data from a ridge-crest seismic line at the southern East Pacific Rise indicates that the axial magma chamber here is about 50 m thick, is embedded within a solid roof, and has a solid floor. The 50-60-m-thick roof is overlain by a 150-200-m-thick low-velocity zone that may correspond to a fracture zone that hosts the hydrothermal circulation, and the roof itself may be the transition zone separating the magma chamber from circulating fluids. Furthermore, enhanced hydrothermal activity at the sea floor seems to be associated with a fresh supply of magma in the crust from the mantle. The presence of the solid floor indicates that at least the upper gabbros of the oceanic lower crust are formed by cooling and crystallization of melt in magma chambers.
The determination of along-axis variations in melt properties within the crustal axial magma chamber beneath fast spreading axes is important for understanding melt delivery from the mantle, eruption history along the ridge crest, and the process of crustal accretion. Seismic reflection images(1-4) have shown the molten sill to be continuous along the ridge crest for many tens of kilometres with varying widths (250-4,500 m), but variations in its seismic properties and thickness have remained elusive, despite several attempts to constrain these properties(5-7). Here we report that the melt sill along the southern East Pacific Rise, which is about 50 m thick, undergoes abrupt changes in its internal properties, ranging from pure melt to mush. The 60-km-long ridge-crest segment near 14 degrees 00' S is characterized by three 2-4-km sections containing pure melt embedded within a magma chamber rich in mush. These small pure melt pockets may represent a fresh supply of magma from the mantle, capable of erupting and forming the upper crust. Conversely, the 80-90% of the magma chamber which is mushy is unlikely to erupt and may influence the lower-crustal accretion.
The southern San Andreas fault (SSAF) accommodates a significant amount of strain between the Pacific and North American plates; thus, the fault represents a major geohazard to the populated areas of southern California, in particular the larger Los Angeles metropolitan area. Paleoseismic chronology of ruptures along the SSAF segment suggests this fault is near the end of its interseismic period (similar to 180 years), because it has not ruptured in historic times (similar to 320 years). A recent active-source seismic experiment performed in the Salton Sea west of the SSAF provides evidence for extensional deformation along the northeastern shore of the Salton Sea. This study posits that the extensional deformation is due to a previously unmapped fault, here named the Salton trough fault (STF). The seismic reflection data image a divergent sediment package that dips toward the northeast with thicknesses up to at least 2 km. Refraction inversion produces a southwestward-dipping velocity discontinuity that crops out east of the SSAF surface trace, consistent with the existence of a southwest to northeast gradient in lithology. If present, the existence of the STF has scientific and societal relevance. First, the STF appears to control the recent Salton trough architecture north of Bombay Beach. Second, from a seismological hazards perspective, the presence of this structure could alter the current understanding of stress transfer and rupture dynamics in the region, as well as community fault models and ground-motion simulations on the SSAF.
The Newport-Inglewood/Rose Canyon (NIRC) fault zone is an active strike-slip fault system within the Pacific-North American plate boundary in Southern California, located in close proximity to populated regions of San Diego, Orange, and Los Angeles counties. Prior to this study, the NIRC fault zone's continuity and geometry were not well constrained. Nested marine seismic reflection data with different vertical resolutions are employed to characterize the offshore fault architecture. Four main fault strands are identified offshore, separated by three main stepovers along strike, all of which are 2km or less in width. Empirical studies of historical ruptures worldwide show that earthquakes have ruptured through stepovers with this offset. Models of Coulomb stress change along the fault zone are presented to examine the potential extent of future earthquake ruptures on the fault zone, which appear to be dependent on the location of rupture initiation and fault geometry at the stepovers. These modeling results show that the southernmost stepover between the La Jolla and Torrey Pines fault strands may act as an inhibitor to throughgoing rupture due to the stepover width and change in fault geometry across the stepover; however, these results still suggest that rupture along the entire fault zone is possible.
Multichannel reflection and coincident wide-angle seismic data collected during the 2002 Premier Experiment, Sea of Cortez, Addressing the Development of Oblique Rifting (PESCADOR) experiment provide the most detailed seismic structure to date of the southern Gulf of California. Multichannel seismic (MCS) data were recorded with a 6-km-long streamer, 480-channel, aboard the R/V Maurice Ewing, and wide-angle data was recorded by 19 instruments spaced every similar to 12 km along the transect. The MCS and wide-angle data reveal the seismic structure across the continent-ocean transition of the rifted margin. Typical continental and oceanic crust are separated by a similar to 75-km-wide zone of extended continental crust dominated by block-faulted basement. Little lateral variation in crustal thicknesses and seismic velocities is observed in the oceanic crust, suggesting a constant rate of magmatic productivity since seafloor spreading began. Oceanic crustal thickness and mean crustal velocities suggest normal mantle temperature (1300 degrees C) and passive mantle upwelling at the early stages of seafloor spreading. The crustal thickness, width of extended continental crust, and predicted temperature conditions all indicate a narrow rift mode of extension. On the basis of upper and lower crust stretching factors, an excess of lower crust was found in the extended continental crust. Total extension along transect 5W is estimated to be similar to 35 km. Following crustal extension, new oceanic crust similar to 6.4-km-thick was formed at a rate of similar to 48 mm a(-1) to accommodate plate separation.
The Earth's oceanic crust crystallizes from magmatic systems generated at mid-ocean ridges. Whereas a single magma body residing within the mid-crust is thought to be responsible for the generation of the upper oceanic crust, it remains unclear if the lower crust is formed from the same magma body, or if it mainly crystallizes from magma lenses located at the base of the crust(1-3). Thermal modelling(4-6), tomography(7), compliance(8) and wide-angle seismic studies(9), supported by geological evidence(3,10-18), suggest the presence of gabbroic-melt accumulations within the Moho transition zone in the vicinity of fast- to intermediate-spreading centres. Until now, however, no reflection images have been obtained of such a structure within the Moho transition zone. Here we show images of groups of Moho transition zone reflection events that resulted from the analysis of similar to 1,500 km of multichannel seismic data collected across the intermediate-spreading-rate(19) Juan de Fuca ridge. From our observations we suggest that gabbro lenses and melt accumulations embedded within dunite or residual mantle peridotite are the most probable cause for the observed reflectivity, thus providing support for the hypothesis that the crust is generated from multiple magma bodies.
Recent P wave velocity compilations of the oceanic crust indicate that the velocity of the uppermost layer 2A doubles or reaches similar to 4.3 km/s found in mature crust in < 10 Ma after crustal formation. This velocity change is commonly attributed to precipitation of low-temperature alteration minerals within the extrusive rocks associated with ridge-flank hydrothermal circulation. Sediment blanketing, acting as a thermal insulator, has been proposed to further accelerate layer 2A evolution by enhancing mineral precipitation. We carried out 1-D traveltime modeling on common midpoint supergathers from our 2002 Juan de Fuca ridge multichannel seismic data to determine upper crustal structure at similar to 3 km intervals along 300 km long transects crossing the Endeavor, Northern Symmetric, and Cleft ridge segments. Our results show a regional correlation between upper crustal velocity and crustal age. The measured velocity increase with crustal age is not uniform across the investigated ridge flanks. For the ridge flanks blanketed with a sealing sedimentary cover, the velocity increase is double that observed on the sparsely and discontinuously sedimented flanks (similar to 60% increase versus similar to 28%) over the same crustal age range of 5-9 Ma. Extrapolation of velocity-age gradients indicates that layer 2A velocity reaches 4.3 km/s by similar to 8 Ma on the sediment blanketed flanks compared to similar to 16 Ma on the flanks with thin and discontinuous sediment cover. The computed thickness gradients show that layer 2A does not thin and disappear in the Juan de Fuca region with increasing crustal age or sediment blanketing but persists as a relatively low seismic velocity layer capping the deeper oceanic crust. However, layer 2A on the fully sedimented ridge-flank sections is on average thinner than on the sparsely and discontinuously sedimented flanks (330 +/- 80 versus 430 +/- 80 m). The change in thickness occurs over a 10-20 km distance coincident with the onset of sediment burial. Our results also suggest that propagator wakes can have atypical layer 2A thickness and velocity. Impact of propagator wakes is evident in the chemical signature of the fluids sampled by ODP drill holes along the east Endeavor transect, providing further indication that these crustal discontinuities may be sites of localized fluid flow and alteration.
Detailed studies of the morphology of the East Pacific Rise axis have shown that its linearity is disrupted by many small but distinct non-transform offsets, including overlapping spreading centres (OSCs) and deviations from axial linearity (devals), which display variable geochemical signals1–9. Using multichannel seismic reflection profiling, we have mapped the distribution of a bright, shallow reflector that Detrick et al. 10 have associated with an axial magma chamber. We have found that it is neither continuous across the 9°03' OSC6, nor separated into two parallel bodies2, and that its lateral offset does not conform to that of the topographic offset associated with the 9° 17' deval. These observations provide important insight into a causative relationship between morphological and petrological segmentation in this region of the East Pacific Rise, and we speculate that the discontinuities may be the morphological response to fluctuations in the spatial pattern of magma delivery.
Marine Geology and Geophysics
Mailing Address: IGPPScripps Institution of OceanographyUC San Diego9500 Gilman Drive #0225La Jolla CA, 92093-0225
Location: 328 IGPP/Munk LabTel: 858-534-4301Fax: 858-534-5332
aharding at ucsd.edu


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c5416 datasheets
TI altereddocumentation. C5416 DSP Starter Kit ( DSK) TMDSDSK5416 Product Information Description The TMS320C5416 DSP starter kit ( DSK) is a low- cost development platform designed to speed the development of power- efficient applications based on TI' s TMS320C54x DSPs. The kit, which provides new performance- enhancing features.