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Spatio-temporal changes in the seismic velocity induced by the 2011 Tohoku-Oki earthquake and slow slip event revealed from seismic interferometry, using ocean bottom seismometer's records
Seismic interferometry is one of the most effective techniques for detecting temporal variations in seismic velocity caused by large earthquakes. Before the 2011 Tohoku-Oki earthquake (Mw9.0) near the Japan Trench, a slow slip event (SSE, Mw7.0) and low-frequency tremors were observed near the trench. Here, we applied a seismic interferometry technique using ambient noise to data from 17 ocean bottom seismometers (OBSs) installed above the focal region before the main shock. We used our technique to detect temporal variations in seismic velocity caused by the main shock, SSE, and low-frequency tremors. In the region above the large coseismic slip area, we detected a 1–2% seismic velocity decrease after the main shock. In addition, we observed very small temporal increases in seismic velocity near the SSE fault during the initial SSE stage. Moreover, for most of the OBSs, we observed temporal variations in the autocorrelation functions (ACFs) during the low-frequency tremors. These may have been caused by temporal variations in the ambient noise source distributions, resulting from low-frequency tremors. These results suggest the possibility of detecting low-frequency tremors using ACF monitoring.
KeywordsAmbient noise Autocorrelation function Seismic interferometry Slow slip event
Autocorrelation Function
Cross-correlation function
Ocean bottom seismographs
Slow slip event
Seismic interferometry is one of the most powerful techniques for obtaining Green's functions. While seismic interferometry has a high temporal resolution (equivalent to analyses using an artificial source), it does not require an artificial source. Wegler et al. (2009) reported a decrease in seismic velocity of 0.5% after the 2004 mid-Niigata earthquake (Mw6.6) based on seismic interferometry applied to ambient noise. Similarly, other studies have reported decreases in seismic velocity accompanied by large earthquakes in several regions, such as Japan and Sumatra (e.g., Nimiya et al. 2017; Sawazaki et al. 2016; Takagi et al. 2012; Xu and Song 2009). A wide variety of techniques have been used in many regions, and most studies have reported variations in the seismic velocity structure accompanying large earthquakes. However, only a few studies have reported variations in the underground structure accompanying slow slip events (SSEs) (Rivet et al. 2011, 2014).
A number of studies have reported variations in seismic velocity of between 0.1 and 5% after a main shock and accompanying SSE. For example, Sawazaki et al. (2016) detected velocity decreases of 3.1% and 1.4% 1 week after the 2014 northern Nagano Prefecture earthquake (Mw6.2), and recovery to velocity decreases of 1.9% and 1.1% 4 weeks after the main shock, using KiK-net data and autocorrelation functions (ACFs). In contrast, Rivet et al. (2011) reported a velocity decrease of only 0.2% during the early part of the 2006 Guerrero SSE, and an almost complete velocity decrease recovery during the later part. Seismic velocity decreases immediately after an earthquake, and velocities recover in proportion to the time elapsed. However, during SSEs, changes are observed in seismic velocities, which decrease during the early parts of an SSE period and subsequently recover in the later parts.
The 2011 Tohoku-Oki earthquake (Mw9.0) occurred off the coast of mainland Japan on March 11, 2011, and prior slow earthquakes (Mw7.0) occurred off the coast of mainland Japan nearer the Japan trench about 1 month prior. Prior to the main shock, a clear preslip was not observed near the main shock's epicenter (Hirose 2011; Hino et al. 2013). An episodic SSE and low-frequency tremors were observed beginning 1 month before the earthquake in the region trenchward of the main shock's epicenter (Ito et al. 2013; Ito et al. 2015). The phase velocity of the Rayleigh wave decreased below 0.5%, accompanying the main shock at Tono, Iwate Prefecture (Takagi et al. 2014). Additionally, accompanying a series of earthquakes (including aftershocks), a seismic velocity decrease of approximately 2% was detected in southern Fukushima Prefecture (Minato et al. 2012). Moreover, seismic velocity decreases under the sea floor of 1–5% were reported after the earthquake (Ito and Hino 2013). However, variations in seismic velocity accompanying the preceding SSE have not been reported. Therefore, in this study, we used a seismic interferometry technique using ambient noise to data, and applied it to ocean bottom seismographs (OBSs). We aimed to detect temporal variations in the seismic velocity structure accompanying the SSE.
2011 Tohoku SSE, analysis period, and data
From January 29 to March 9, 2011, an SSE and low-frequency tremors were detected offshore from Miyagi Prefecture, Japan (Ito et al. 2013; Ito et al. 2015; Katakami et al. 2018). Low-frequency tremors were observed during three periods:
Sequence 1. January 24–January 29
Sequence 2. February 16–February 20
Sequence 3. March 5–March 9
Location and recording period of each OBS. We measured the locations of LS1 and S03 when they were collected, and the locations of other stations when they were set up
Station name
Location of OBSs
Record period
Longitude (°E)
Latitude (°N)
Depth from sea surface (m)
November 5, 2010–April 13, 2011
November 5, 2010–October 6, 2011
November 5, 2010–October 6, 2011
November 5, 2010–October 6, 2011
November 5, 2010–May 21, 2011
November 5, 2010–May 21, 2011
November 5, 2010–April 13, 2011
October 1, 2010–July 12, 2011
October 1, 2010–July 12, 2011
July 1, 2010–March 18, 2011
July 1, 2010–May 22, 2011
July 1, 2010–May 22, 2011
July 1, 2010–March 18, 2011
November 5, 2010–May 21, 2011
November 5, 2010–May 21, 2011
November 5, 2010–May 21, 2011
November 19, 2010–May 23, 2011
Data analysis
Seismic interferometry is one of the most effective techniques for detecting temporal variations in seismic velocities caused by large earthquakes. Claerbout (1968) showed that a reflected wave (generated at an observation station on the earth's surface, reflected off a boundary under the station, and returned to the station) could be obtained by calculating the ACF from the waveform observed at the station. This technique is only effective if the structure around the site is a horizontal stratified structure. In the field of helioseismology, Duvall et al. (1993) proved that the Green's function between two stations can be obtained by calculating the CCF between the stations. In seismic interferometry, this technique is applied to the field of seismology. Since Campillo and Paul (2003) reported that a CCF constructed from teleseismic coda waves corresponded to the direct wave between two stations in the scattering field, many studies using seismic interferometry have been published (e.g., Hillers and Campillo 2016; Poli et al. 2012).
Generally, the coefficient c(t) represents the correlation between the observed and calculated envelopes only after an elapsed time that is twice the travel time of the S wave. In addition, we also applied a weight of 0 before 300 s if the coefficient exceeded 0.5, because the 600 s time window included seismic waves radiating from the ordinary earthquake.
In this study, we investigate spatio-temporal variations of three functions: ACFs of ambient noise, cross-correlation coefficients of the CCFs between a 15-day ACF and a reference ACF, and phase shift based on the CCFs. These values are calculated as shown below.
First, all observation data were corrected for the instrument response before applying the band-pass filter. Then, we applied a band-pass filter at 0.25–2.0 Hz and a one-bit technique to the observed continuous data. These filters were applied to prevent the continuous data from being affected by (1) unexpected signals (such as micro-earthquakes) that could not be removed with the aforementioned weight function, or (2) mechanical or biological noise at the site.
Next, after applying the band-pass filter and one-bit technique at intervals of 0.1 s, we calculated 120 s ACFs using 5 s moving time windows. The coefficient for the time including earthquakes equaled 0 after multiplying the weight w(t) of the time window, and the earthquake effects were removed. The 15-day ACF was defined as the ensemble average of the 120 s ACFs calculated over 15 days. The reference ACF was defined as the ensemble average of 120 s ACFs calculated over a month from November 19 to December 19, the period before the occurrence of SSE and low-frequency tremors.
In addition, we calculated the CCF using a 15 s moving time window between the 15-day ACF and reference ACF with a lag time of − 2 s to 2 s, at intervals of 0.1 s, and estimated the variation in seismic velocity based on the lag time at the maximum CCF. Finally, we objectively evaluated the temporal variations in the 15-day ACFs based on the variations in the cross-correlation coefficient at zero lag time. The shape changes of the 15-day ACFs cause the coefficients to decrease. When a velocity change occurs, the phase of the 15-day ACF delays or progresses, and the shape changes. Even when a velocity change does not occur, it is possible for the shape to change, and a variation in the hypocenter distribution of the ambient noise may explain this shape changes. Therefore, we used the coefficient at zero lag time to detect the temporal variations in the 15-day ACFs caused by, not only velocity change, but also temporal variation of the ambient noise.
Temporal variations in ACF
The cross-correlation coefficient around a lapse time of 10 s decreased after sequence 1 (Fig. 2b). A decrease in the coefficient was detected at most stations installed east of 142.5° E and appeared before sequence 1 at 60% of these stations, such as S10 (Fig. 4b). At all stations, the decreases recovered after 10 days. Similar coefficient variations were detected during sequences 2 and 3, but the decreases were less than that during sequence 1. During SSE, some sustained variations in cross-correlation coefficients were not detected.
Temporal variations in seismic velocity based on variations in the 15-day ACF
In addition, we also calculated the velocity changes accompanying the SSE and low-frequency tremors from the phase changes. However, we did not detect obvious changes. Although velocities changed by a few tenths of a percent during the SSE at several stations, such as S09 and S15, the changes were equivalent to those in a normal period when no SSE, no low-frequency tremors, and no large earthquakes occurred (Fig. 5). At all stations, the velocity changes accompanying the SSE and low-frequency tremors were smaller than the velocity fluctuations in the normal period.
Regional characteristics of temporal variations in 15-day ACF
Periods used for calculation of variations in cross-correlation coefficients
November 26, 2010–December 14, 2010
January 9, 2011–January 23, 2011
III (sequence 1)
January 24, 2011–January 29, 2011
February 6, 2011–February 15, 2011
V (sequence 2)
February 16, 2011–February 20, 2011
February 22, 2011–March 3, 2011
VII (sequence 3)
March 5, 2011–March 9, 2011
At the six landward stations (S27, S22, S21, S02, S01, and LS1), the variations for each period were extremely small. This indicates that the cross-correlation coefficients at the six stations were stable in all periods (hereafter region L). However, at the other 11 stations, clear variations were observed for each period. For example, the variation from period II to period III (Fig. 6b) was equivalent to the variation induced by a low-frequency tremor occurrence. A low-frequency tremor did not occur in period II but did occur in period III. At the 11 stations, the variations basically decreased when low-frequency tremors occurred and increased (recovered) after low-frequency occurrences.
The 11 stations were classified into 2 groups. In one group, the coefficient decreased primarily in period II. The eight stations (S15, S14, S10, S04, S03, LS4, LS3, and LS2) located at the center of the OBS array (hereafter Region C) belong to this first group. In another group, the coefficient decreased primarily in period III. The three stations (TJT2, S18, and S09) located near the trench (hereafter Region T) belong to this second group. Regions C and T correspond roughly to the slip area of the largest foreshock and the SSE occurrence area mentioned in Ito et al. (2013), respectively.
Temporal variations in seismic velocity and the 15-day ACF
The observed phase delays after the main shock were larger during the later lapse times for the 15-day ACFs than during the earlier lapse times (Fig. 2c). When velocity structures change equally, the travel time increases monotonically for the wave transmitted in a region in proportion with the propagation distance, resulting in an increase in the phase delay during the latter part of the 15-day ACF. In addition, the phase in the latter part of the 15-day ACF carries information regarding waves that have traveled longer distances because of reflection and refraction around the observation station. Moreover, it is possible for the velocity to change equally around a site after the main shock. At S09, the equal velocity decreased after the main shocks were detected for the lapse times of 30–40 s, 40–50 s, 50–60 s, and 60–70 s (Fig. 5). This suggests that a wave reflected many times under S09 reaches this observation station after 60 s. In contrast, the phase delay at TJT2 appeared only for part of the lapse time (Additional file 1), suggesting that the velocity structure did not change equally, but rather in part of the region.
At S09, although phase changes appeared for only a short section around a lapse time of 10 s during sequences 1, 2, and 3 (Fig. 2c), we did not detect a velocity change corresponding to the phase changes (Fig. 5). If the phase changes are caused by an increase in the seismic velocity in part of the region, a phase (or velocity) change several times larger than a phase change at a lapse time of 10 s should appear when the wave transmitted along the same path several times returns to the station. However, such a phase change was not observed. Therefore, the phase changes were not caused by variations in the velocity structure, and it is possible that variations in the hypocenter distribution of ambient noise induced by the low-frequency tremors cause a phase change similar to that caused by a structural change. The phase progression during sequence 1 continued longer after the end of the low-frequency tremor activity and was larger than those during sequences 2 and 3. This phase progression probably included the dummy structural variation accompanying the beginning of the SSE, in addition to the dummy structural variation caused by the variation in the hypocenter distribution accompanying the low-frequency tremors.
When the density of a crack near a hypocenter increases because of the formation of cracks before an earthquake, seismic velocity is expected to decrease around the hypocenter. Several studies using rocks have reported a decrease in the elastic wave velocity accompanying an increase in crack density (e.g., Nishizawa and Kanagawa 2005). According to Lockner et al. (1991), a decrease in elastic wave velocity and decrease in amplitude were detected before a rock sample broke. This was accompanied by the creation of micro-cracks formed by acoustic emissions. Therefore, we speculate that the observed phase delays and decreases in cross-correlation coefficients may have been caused by the creation of micro-cracks. We detected decreases in velocity before the main shock, and noted that these velocity decreases began earlier at the observation station nearer the hypocenter of the main shock. However, we detected no velocity changes before the SSE around the SSE region. This suggests the possibility that the crack density varied little before the SSE, although the density varied enough to change the 15-day ACF before the main shock. Overall, the results suggest that the mechanism of structural change in seismic velocity accompanying an SSE detected by seismic interferometry may differ from that associated with an earthquake.
Spatio-temporal variations in cross-correlation coefficients at each station
We classified the temporal variations in the cross-correlation coefficients around a lapse time of 10 s at all stations (Fig. 6) into three groups: region T, region C, and region L. These three regions corresponded to three slip areas: region L corresponded to the area that slipped only during the main shock (Iinuma et al. 2012), region C corresponded to the slip area of the largest foreshock (Ohta et al. 2012), and region T corresponded to the SSE slip area (Ito et al. 2013). In "Temporal variations in seismic velocity and the 15-day ACF" section, we indicated the possibility that the phase changes around a lapse time of 10 s were caused by the occurrence of low-frequency tremors. The cross-correlation coefficient between the 15-day ACF and the reference ACF at zero lag time decreases if the phase of the 15-day ACF changes. Although the coefficients decreased during sequences 1, 2, and 3, the time when the decrease of sequence 1 began was different at each observation station. In region C, where coefficient decreases started from period II before sequence 1, it is possible that low-frequency tremors occurred during period II, and that the 15-day ACF changed because of variations in the hypocenter distribution. In agreement, Katakami et al. (2018) reported that micro-low-frequency tremors occurred near region C in the same period. Therefore, the coefficient decreases during period II were caused by the occurrence of a low-frequency tremor.
Meanwhile, the widths of the lapse time section, where the coefficients decreased substantially, were different in during period II and during low-frequency tremor periods (III, V, and VII). The coefficients during period II at the stations installed in region C decreased substantially in a wide section between lapse times of 10 s and 20 s (Fig. 4b). However, the coefficients during periods V and VII at the stations installed in region C decreased substantially in narrow sections around a lapse time of 10 s. The coefficients during period III at stations installed in region T also decreased largely in a narrow range, around a lapse time of 10 s (Fig. 2b). The width of the lapse time section during period II was different from the widths of the lapse-time section during periods V and VII at the same station installed in region C. In addition, although the stations were different, the width of the lapse time section during period II at the station installed in region C was different from the widths of the lapse time section during period III at stations installed in region T. This suggests that the decrease during period II was unique in terms of the width of the lapse time section where the coefficients decreased substantially compared to the coefficient decreases for the section widths during periods III, V, and VII. Therefore, it is possible that the decrease during period II occurred not only because of low-frequency tremors, as detected by Katakami et al. (2018), but also because of an additional event, for example, the preparation process of the 2011 Tohoku-Oki earthquake.
Estimated velocity reductions during 2011 Tohoku-Oki earthquake and SSE
The decrease in velocity under an observation station represents one interpretation of the cause of a phase delay. When a wave reflects off a surface and returns to the station, a phase delay is observed if the seismic wave velocity decreases along the propagation path. The delay can also be explained by an increase in the distance between an observation station and a reflection surface, because the propagation distance of the reflected wave is determined by the distance between an observation station and a reflection surface. Assuming that the distance to the reflection surface did not change, the observed phase delays after the main shock were equivalent to a 2% or lower seismic velocity decrease at six stations (TJT2, S15, S09, S04, LS4, and LS1) near the trench. Ito and Hino (2013) studied the sea floor in the same region as the present study, and detected decreases in seismic velocity of 1–5% after the main shock in the overall analysis region. Moreover, a decrease in seismic velocity of 2% in the southern Fukushima Prefecture (Minato et al. 2012) and 0.1–0.5% in the Iwate Prefecture (Takagi et al. 2012) were reported after the main shock using land data. In the present study, the observed seismic velocity decreases were lower than those of Ito and Hino (2013), but roughly equivalent to those of other regions that shook during the main shock.
In the SSE period, we detected a perturbation in seismic velocity of a few tenths of a percent around the SSE area. At TJT2, S18 (Additional file 23), and S09, which were installed near the SSE region, the velocity changes calculated from the phase changes at lapse times of 20–30 s, 30–40 s, and 40–50 s increased slightly during the initial SSE stage, and did not change after that stage (e.g., Fig. 5). Two studies of the 2006 SSE and 2009 SSE at Guerrero, Mexico, detected decreases and recoveries in seismic velocity during the SSEs using data from stations landward of the SSE slip regions (Rivet et al. 2011, 2014). The researchers proposed that the velocity decreased by 0.8% in the former part of the SSE period and recovered almost completely in the latter part. In this study, increases in velocity were observed in the former part of the SSE period using data from both landward and trenchward stations. However, after that, we did not observe an additional decrease (recovery) during the observation period. We observed a difference between the two Guerrero SSEs and the Tohoku-Oki SSE with respect to whether or not any large earthquakes occurred at the plate boundary immediately after the SSEs. The Guerrero SSEs concluded without any large earthquakes, but the Tohoku-Oki SSE concluded with large earthquakes with foreshocks, a mainshock, and aftershocks. Because SSEs were detected by GPS data, if another crustal deformation, such as a large earthquake, occurs during an SSE, it is possible that the timing of the end of the SSE is not detected clearly. Moreover, because earthquakes release stress near the hypocenter, an occurrence of large earthquakes ends SSEs that occur near the hypocenter. It is highly likely that the Guerrero SSEs were observed from beginning to end completely because no large earthquakes occurred during the Guerrero SSEs. On the other hand, it is highly likely that the 2011 Tohoku-Oki earthquake occurred before the Tohoku-Oki SSE finished, and it is possible that the Tohoku-Oki SSE was ended suddenly by the 2011 Tohoku-Oki earthquake. If the 2011 Tohoku-Oki earthquake ended the Tohoku-Oki SSE before the velocity recovery period in SSE, it is not surprising that we could not detect velocity recovery in the latter part of the Tohoku-Oki SSE.
We detected decreases in seismic velocity of no more than 2% at six stations near the hypocenter of the 2011 Tohoku-Oki earthquake. These decreases were detected after the main shock using seismic interferometry with ambient noise. The largest velocity reduction was observed at S09, located between the hypocenter of the main shock and the slip region of the SSE before the main shock.
In addition, we detected temporal perturbations in the seismic velocity during the SSE at three stations around the SSE region. The velocities increased a few tenths of a percent immediately after the SSE began and did not change after that. Velocity decreases in the early parts of SSEs and recoveries in the latter parts of SSEs were reported in previous studies; however, we did not detect any velocity recoveries in the latter period.
We observed variations in the 15-day ACFs before a lapse time of 15 s at most stations installed east of 142.5° E. These variations were accompanied by low-frequency tremors, although no variations in seismic velocity were detected. Specifically, the 15-day ACFs showed substantial, long-lasting variations during sequence 1. The variations during sequence 1 included not only the effects of the low-frequency tremors but also the effects of the SSE. All stations were classified based on their characteristics when variations in the 15-day ACFs were observed. Variations in the 15-day ACFs at stations installed between 142.5° E and 143° E were observed 15 days before sequence 1, and variations at stations installed east of 143° E near the trench were observed during sequence 1. These regions roughly corresponded to the slip areas of the largest foreshock and SSE. Moreover, the variations in the 15-day ACFs indicated the possibility that low-frequency tremors occurred before sequence 1 between 142.5° E and 143° E.
We thank Masatoshi Miyazawa for helpful discussions. We thank Masa Kinoshita, and two anonymous reviewers for their constructive comments. We also thank Editage for the English language revision.
This work was supported by the Japan Society for the Promotion of Science (JSPS) KAKENHI grant (#26257206) and Japan Science and Technology Agency—Japan International Cooperation Agency Science and Technology Research Partnership for Sustainable Development (JST-JICA SATREPS) (#15543611) grants to M. U. and Y. I., and a JSPS KAKENHI grant (#26000002) grant to R. H., M. S., Y. I., K. O., and M. U.
Availability of data and materials
Please contact author for data requests.
Authors' contributions
MU conceived the study, analyzed the data, and interpreted the analysis results. YI proposed the topic, collected the data, and helped the interpretation. KO collected the data and helped the interpretation. RH and MS collected the data and collaborated with the corresponding author in the construction of manuscript. All authors read and approved the final manuscript.
Authors' information
M. U. is a student in a doctor's course in division of earth and planetary sciences at Kyoto University. Y. I. is an associate professor at Disaster Prevention Research Institute, Kyoto University. K. O. is an assistant professor at Disaster Prevention Research Institute, Kyoto University. R. H. is a professor at International Research Institute of Disaster Science, Tohoku University. M. S. is a professor at Earthquake Research Institute, The University of Tokyo.
Competing interests
The authors declare that they have no competing interests.
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Supplementary material
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Clinical and pathological features of pediatric dermatofibrosarcoma protuberans.
@article{Keshen1995ClinicalAP, title={Clinical and pathological features of pediatric dermatofibrosarcoma protuberans.}, author={Tamir H Keshen and Paul S. Cederna and Van H. Savell and Charles E. Platz and Patricia Chang and Edward J. Ricciardelli}, journal={Annals of plastic surgery}, year={1995}, volume={35 6}, pages={ 633-7 } }
- Published in Annals of plastic surgery 1995
Dermatofibrosarcoma protuberans (DFSP) is an uncommon malignant mesenchymal tumor characterized by local invasion and recurrence. Fewer than 50 cases have been reported in the pediatric population. We reviewed our experience in the treatment of children with DFSP to define clinical and pathological characteristics. Seven pediatric patients were included in the study (mean age, 11.7 yr). Clinically, the tumors were described as firm nodules fixed to the skin but mobile over the deep fascia, with… CONTINUE READING

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Hire Children's Magician in Lewes
Browse Children's Magicians
About: Welcome to Acting Moon Events, a circus entertainment agency based in Eastbourne, East-Sussex. Specialist in providing highly creative and professional entertainment. We have everything you need to make sure that your event is successful, memorable and fun! With a wide range of professional acts we
Recent review: Absolutely amazing!! So so happy with the entertainment and the entertainer, she was just great and have to children so hooked with everything she did, every parent told me that the party was just incredible. Booking my package was very straightforward and lily lou was so accommodating to what i wan
Recent review: Steve was brilliant he kept all of the children at my son's 5th birthday party very entertained and kept them all focused.i would definitely recommend and would definitely use again.thank you Steve. Lisa
Recent review: Book Jamie the Magician now if you want to have a super duper oh so awesome kids party. We had Jamie at our daughters 4th birthday who kept 25 kids sitting (yes I did say sitting) and actively engaged and excited to see what magic would appear! And something the adults will enjoy too!
About: OUTSTANDING, FUN and ACTION PACKED children's entertainment for 3-11 year olds! We are proud to be one of the South East's most loved and well established children's entertainment party providers, bringing magical, memorable party entertainment that the kids love and creating memories the grown-ups
About: Catty Watty Boom Boom will make your children's party fabulously fun, magical and extremely memorable. Expect silliness, joy, magic, a very interactive and funny show where the children help throughout and join in with words & actions, modelling balloons, bubbles, games and disco. Cat is very exper
About: Andy is a fantastic, friendly and fun entertainer for children's birthday parties and family events. He entertains with an amazing magic show, aimed to dazzle and delight, filled with fantastic routines that will both impress and also make his audience laugh out loud from start to finish. His sho
About: I have been performing parties since 1989, and in UK and Europen circuses for over 20 years. I now offer magician, comedy pirate, circus clown, comedy chef, comedy waiter, and Christmas elf characters, for all events from corporate, promotions, stage and arena shows, mix and mingle, weddings and par
Recent review: Adam was great - he captivated his audience of 20 six year olds (plus a few older and younger siblings), for a full 1.5 hours. He involved the adults that were there too, with one parent deciding to stay to watch the whole thing rather than drop thier kids off. 24 hours later and a couple of parents
About: A typical 2 hour programme includes a 50 min fun magic show in which the children participate, plus music & movement games and puppetry. While the children have their tea I do balloon modelling so that every child can take a balloon home, followed by face painting if required. But I am flexible
Recent review: Hello Prof I just wanted to say a big thank you for today. There was so much cheering and shouting from the children who were completely enthralled by your show! It was all Annabelle could talk about when she got home and lots of children and patent said how great your were. I would certainly not h
Recent review: We had a fantastic NYE 6th birthday party yesterday with Sherine - it so was nice to only worry about the snacks/greet guests and actually get to enjoy the party this year rather than running around after the kids! Sherine had a group of about 12 kids dancing, playing and generally just having a gr
Recent review: I wanted to say a huge thank you for making my son's and my daughter birthday party so much fun All the kids loved you & Everyone had an amazing time,You were fantastic.Would definitely recommend you to family and friends. Thank you again.. Tama
About: I am an award-winning variety entertainer, with over 20 years experience, in cabaret, theatre, film, TV and international festivals I do a full variety show with magic (for both adults and children) comedy puppetry, circus skills guitar and also run dance events As a dj
Recent review: Thank you for doing such a wonderful job at Kieran's party. You managed to achieve exactly what I had envisaged, 20 happy, busy children and relaxed parents. Thank you for keeping them entertained throughout the two hours. We have received some lovely comments back saying that the children really en
Recent review: Fantastic entertainer. We had a Frozen themed party for my daughter 5th birthday party on 24/8/17 and Elsa went way and above the line of duty. She captured everyone's imagination for 2.30 hours and the girls and boys were both equally mesmerised. She also did additional face painting and made sure
Recent review: An incredibly charming and thoroughly talented magician who wowed and entertained our guests throughout our drinks reception at our wedding. We would definitely recommend Dean and were over the moon with how he interacted with our guests! Thank you so much!
About: Magic Mike magic shows are guaranteed to bring a smile to every occasion Magic Mike will provide the perfect entertainment at birthday parties for children from 3 years upwards
Recent review: Hannah was AMAZING, Kept to the theme, had the kids entertained the whole time and all the mummys said how fantasic she was. I would deffo book her again. Becky
Recent review: Jasmine was fantastic. I was nervous because it's the first time I've organised a kids' party at home, but she put me at my ease and kept the kids very well entertained for the duration. I wouldn't hesitate to recommend her.


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CCE BPO job vacancies. Inbound and outbound BPO call center hiring for voice process in Central Delhi
BPO Call Center Jobs, Delhi, Delhi NCR City 0 Comments 1525 total views, 0 today
Briefing of the Job Opening
|Job location- City
|City (Other)
|Educational Qualifications
|12th pass
|Salary Range
|1-2 Lacs CTC
|Work Experience Required
|Total number of openings for the Hiring
|The Job Opening is being Published by
|Independent recruiter
Company/Consultancy Address as for the Interview place
ADDRESS- F-105, First floor, Aman chamber opposite to pillar no. 144 , near to RAJENDRA PLACE METRO STATION, CENTRAL DELHI
Full Job Description
Inbound and outbound BPO call center hiring in Delhi
Graduates with outbound call center experience 0-2 years
Walkin interview address-
F-105, First floor, Aman chamber opposite to pillar no. 144 , near to RAJENDRA PLACE METRO STATION, CENTRAL DELHI
Job opening description
Customer care Executive (Outbound/Inbound )
Any Graduate (Willing to work in this profile)
Good communication skills in English and Basic Excel knowledge
Outbound calling experience approx 0-2 years
Computer Windows XP, WinWord, Excel, etc.
Related Entries:
- Hindi Call Center (Inbound Voice Process) Jobs in Delhi NCR
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Posted by Wendy Trotter, Education Program Consultant - Autism, Iowa Department of Education in CCR&R Blog on 11/22/2018
We need to change our thinking to "let's just see" and evaluate any child who might be falling behind so that they can benefit from additional support if needed. We need to ensure that our infants and toddlers have a strong start in life and the support they need to reach their maximum potential.
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Iowa Family Child Care Association professional development seminar with an emphasis on the unique needs and environments of Family Child Care providers.
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Volume 4, Issue 1, DHS Child Care Newsletter
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Cape Coral Property Search
Condos for Sale in the Isles of Porto Vista
One of the best residential condo complexes in Cape Coral is called the Isles of Porta Vista. Surrounded by water, it's gated and the only access is a bridge entrance, so the security is extra strong. There are 216 condominiums in the complex which has an Italian architecture with Boca Raton terracotta colors of yellow and orange - blended with beautiful lush tropical landscaping and lots of green.
Community amenities include a large clubhouse, resort style pool, fitness and exercise facilities, and sparkling lakes scattered throughout the development along with walking trails and a park.
The two-bedroom, two bath condos range in size from 1270-1460 square foot, depending on the floorplan, and are priced from around $120,000 to $160,000 depending on the size. Built in 2006, they have all the upgrades and extras, such as stainless steel appliances, decorative mosaic backdrops, balconies or porches, and a garage. Low HOA fees and a well operated homeowner's association is a plus.
If you're looking for a quiet and secure community with a great outdoor experience, the Isles of Porto Vista are worth a look. Let me know when you'd like to tour this beautiful complex!
Condos in Isles of Porto Vista
3947 Del Sol LN Unit 102, Cape Coral
Welcome Home to South Florida! Come check out this very clean GROUND floor 2 bedroom, 2 bath Condo with a single car GARAGE. Updates are NEW A/C and Hot Water Heater July...
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3968 Pomodoro CIR Unit 304, Cape Coral
THIS UNIT CURRENTLY REQUIRES 48-72 HOURS NOTICE...... Don't miss your opportunity to own a REMODELED THIRD FLOOR 2 bedroom, 2 bath with a single car GARAGE. One of a kin...
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3944 Pomodoro CIR Unit 304, Cape Coral
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3940 Pomodoro CIR Unit 202, Cape Coral
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Restaurant Verbena at Discovery Country Suites is a top choice for your Valentine's date or any other romantic occasion. I share our experience, plus a promo.
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The only way to get into Gatorland is to walk straight into an alligator's toothy maw. The giant mouth provides entrance to 110 acres of marshy wildlife preserve––home to a vast ecosystem populated by thousands of alligators, crocodiles, and birds, including rare wading birds and four rare white alligators.
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New to the park is the Stompin' Gator Off-Road Adventure, which takes guests off-road for a 15-minute ride that is full of adventure, comedy – and, of course, lots of alligators! Come see for yourself why Gatorland is nicknamed "The Alligator Capital of the World."
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- RESET your scene by replacing and repositioning all your 3D models as you see fit.
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- REMOVE the selected 3D model from your scene
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- LINK allows users to visit the webpage associated with the 3D model.


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Fish Maw - Swim bladder - wikipedia, The swim bladder, gas bladder, fish maw, or air bladder is an internal gas-filled organ that contributes to the ability of many bony fish (but not cartilaginous fish) to control their buoyancy, and thus to stay at their current water depth without having to waste energy in swimming. also, the dorsal position of the swim bladder means the center of mass is below the center of volume, allowing. Fish maw (dried) | chinese soup lady & chinese soup, What is the cost? fish maw prices vary widely depending on the size and type of fish; at a recent herbal shop in hong kong (timing at april 2018), prices ranged from $500 hkd per catty to $5000 hkd per catty.. Recipe: fish maw soup chinese year - 8 ingredients, Fish maw soup is normally served during special occasion such as chinese new year. some of the ingredients (such as fish maw and scallops) are considered as delicacies, and high-grade ones can be expensive.. Fish names tamil — spiceindiaonline, Usually nei meen is a fresh water fish, whose full name is nei keluthi. tilapia should be its equavalent english name. i really hate this fish.. hard skin / hard flesh and its pathetic habitat... Jaw - wikipedia, The vertebrate jaw probably originally evolved in the silurian period and appeared in the placoderm fish which further diversified in the devonian.the two most anterior pharyngeal arches are thought to have become the jaw itself and the hyoid arch, respectively. the hyoid system suspends the jaw from the braincase of the skull, permitting great mobility of the jaws.. Five star chicken rice, Crisp to the last bite rolled in fragrant cereal, curry leaves, and chilli padi, discover the finger-licking satisfaction of this crowd favourite.. Thailand seafood fishing industry companies - | information, Siam canadian foods co., limited supplying a wide range of shrimp, fish, cephalopods and value added seafood products from thailand, including raw and cooked vannamei white shrimp, squid, cuttlefish, baby octopus, seafood mix, seafood skewers, co tuna loins, steaks and saku blocks, red mullet fillets and many more. Red grouper fish soup recipe | noobcook., Fish soup (鱼汤) is one of the few singapore hawker dishes which is easy and worthy to recreate at home. if you are willing to take a few short-cut here and there, you can whip up a delicious fish soup even on weekdays after work.. Creative smocking - sewing, smocking, pleaters, sewing, Creative sewing & smocking is your one stop shop for the classic sewing magazine, read pleater/smocking machines, smocking supplies, sewing supplies, sewing notions, susie's piping for mini-piping, jane mcpherson little labels, read pleater needles, amanda jane needles, sally stanley general purpose pleating needles, hand sewing needles, smocking design plates, smocking graphs, smocking books.
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Honeyblood performing at Leeds Festival 2017 on day three at Bramham Park - Leeds, United Kingdom - Sunday 27th August 2017
2016 looks doomed to be the year that a millionaire, pig's-head-porking Prime Minister decided to 'let the people speak', blithely assuming to the bitter end that the good people of Sunderland must speak like he does.
Those from across the pond, will probably write it off as the year they ended up hiring a billionaire, tiny-handed, Shredded-Wheat-haired fanny-grabber as Commander-in-Chief. Oh, brave new world, that has such people in it...
Praise be, then, for the gift of music, and all of its artistry, its erudition and its social commentary. What more welcoming and uplifting distraction could we have had than the musical creativity that graced us in the last twelve months? Here are ten antidotes to the malaise that was 2016.
Continue reading: Jon Kean's Top Ten Albums Of 2016
Here's 10 of our must-see emerging international artists for South by Southwest 2014.
South by Southwest Music Festival (SXSW) is widely known as THE festival for emerging musical talent with artists both established and up-and-coming flocking from around the globe to Austin, Texas to offer the musical experience of a lifetime to eager festival goers. Having begun in 1987, the weekend event has seen some exciting acts, virtually all of which have shot to international recognition since their slot on the SXSW bill - and very deservedly.
It's a huge opportunity for fledgling bands across the world with such a vast line-up that takes over the whole of Austin for over a week. Unlike most festivals were an artist has to be signed or at least have an agent to feature in the line-up, SXSW does a great job at embracing unsigned talent. The weekend even sees dozens of secret gigs dotted around the city as no-one is ever quite sure of who is and who isn't playing. Prince, Arcade Fire and Jay-Z are just a few of many who have surprised and delighted event goers with their unexpected appearances, so make sure you keep an eye out this year. For now though, we're excited to give you ten top acts from across the planet that are well worth your time this March.
Continue reading: 10 Upcoming International Acts You Should Watch At SXSW 2014
Anima Animus is the third album from Siouxsie Sioux's The Creatures, released exactly 20 years ago today.
Peter Doherty once again highlighted his talent as a musician, lyricist and performer during a very entertaining evening.
Edinburgh four-piece Gypsy Circus talk about their inspirations and their music in exclusive interview.
It doesn't take long to appreciate you are in the presence of rock music royalty when you are offered an audience with Paul McGuinness.
Zedd and Katy Perry team up for a sci-fi themed video which sees the latter play an android who falls in love with her human partner - who doesn't...
Happy Valentine's Day! Lots of couples will celebrating this cheesy AF but lovely day, and will most likely celebrate well into the night too.
As it's almost Valentine's Day, you'll be looking for that perfect romantic playlist to set a dinner date to, right?


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Glasses Usa
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Irony: the Rust-Oleum can is rusted
Recent Posts
- Two weeks on non-stop repeat. What a great album.
- Aesop Rock & TOBACCO are Malibu Ken
- Sunday funday
- Outdoor fun in the 9" of snow ❄
- Grab your milk, fight for bread, scramble for eggs. I'll be hanging out over here
- Exploring games at the Science Center with Oliver 🕹
- Kids these days have it so well
- Love that @4handsbrewingco Chocolate Milk Stout. 🍻


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Wonder Wave Slide for 1.5m platforms
Sale price $299 Regular price
No playground is complete without a slide. This super popular model is suited for attaching to 1.5m high platforms.
It securely attaches at the top with 3 screws. It is a solid double walled design with divots at the base for extra strength and to allow rain run off.
- Wonder Wave slide for 1.5m high platforms
- designed to take up to 80kg of weight (tested to 200kg)
- this slide is 2.65m long top to bottom in a straight line
- it is 55cm wide
- it is made of super reinforced molded plastic with added UV resistance
- rounded edges for children's safety
- made in the USA
- comes with a 1 year warranty
Designed for residential use only.
For extra excitement you could also add a tube slide or look at our 1.8m slide models
Green sold out. Yellow now available ex Christchurch. The green Alpine wave slide is available ex Pukekohe.


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Give in to the exotic confluence of today and tomorrow in this beautiful attire. You are sure to make a strong fashion statement with this multi colour art silk lehenga choli. It is uniquely crafted with embroidered, patch border and resham work. Comes with matching choli and dupatta. (Slight variation in color, fabric & work is possible. Model images are only representative.)
Style: A - Line Lehenga
Fabric: Art Silk
Color: Multi Colour
Work: Embroidered, Patch Border Work, Resham Work


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By being a part of PAUA I have gained a stronger relationship with my sisters.
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Hire Mobile Caterer in Shepton Mallet
Browse Mobile Caterers
Recent review: I hired Smoulder and Scotch for a BBQ at my 50th birthday celebrations and they were fantastic. The food was exceptional and Keiron was very helpful and efficient. I would highly recommend them for any event and would certainly use again
Recent review: Ed Dibbles recently catered for guests here at Croydon Hall (Country House for Hire) who were full of praise for the fresh, delicious Mediterranean lunch they provided. Happily I got to sample their awesome dishes, highly recommended!
About: Been a chef for 27 years, got out of pubs and restaurants as there simply isn't enough staff or decent suppliers, it's to corporate, so now I but it local, prep it, bring it, cook it, serve it, clear up and wash up. Just me and a smile. I love my job. I love feeding people and meeting people. I can
Recent review: Michel and his team were absolutely brilliant. A pleasure to deal with and really accommodating. They made brilliant menu suggestions and the final one we went with was perfect. The set up and serving was very well organised and they left the kitchen extremely tidy, taking all of the hassle out of s
Recent review: Great Tastes very happily took on the challenge of catering for my husband's 60th birthday party for 40 guests in a private wood. Tricky access, no running water, mud, likelihood of more rain - etc. To say they rose to the challenge was an understatement! They were calm, efficient and professional t
Recent review: This is a little overdue but I just wanted to say a big thank you for the food at our wedding. It really was incredible!! Lots of people have commented that it is the best food they have had at a wedding!! It was exactly what we wanted and tested amazing!! I know a few people will be keeping you in
About: Ethic Street Pizza and Grill is a family run pop-up caterer serving delicious pizzas and BBQ using our wood fired pizza oven and drum BBQ. We are experienced providing corporate catering, weddings, pop up street events and parties.
About: La Champagnerie is a mobile bar available for hire at private events, corporate events, weddings, markets and festivals. Our speciality drinks menu is adaptable to all needs being able to provide from a fully stocked bar to a sparkling wine only or cocktails only bar, to a variety of home made sangr
Recent review: Russ did an absolutely blinding job catering our wedding with help from his family. The day went incredibly smoothly and everyone commented on how much they loved the food! I couldn't recomend them highly enough, Russ was accommodating every step of the way and as a result it felt very relaxed. A pa
About: At Pickled Pig we pride ourselves in providing the best quality hog roasts and BBQ. Our innovative menus are sure to be a winner with your guests We strive for the best quality produce locally sourced and outstanding customer service.
About: After completing a degree in creative writing, Fred decided to pursue his real passion and embark on a career in the restaurant industry as a chef. Starting as a complete rookie, he secured a job in the best restaurant in Bristol and learnt the hard way! Moving to London, Fred grew his experience
Recent review: Excellent service from Delivita Catering - Pizza's were delicious, everyone catered for. Set up very efficient and the guys were professional and very friendly! Would definitely recommend and would use again! Thank you.
Recent review: La Bonne Crepe catered our wedding yesterday providing crepes for guests as they arrived. There was universal approval and the guys remained happy and smiling the whole time despite the very hot weather and being surrounded by gas burners! I would highly recommend them for events like ours; especial
About: Everyone wants their guests to enjoy their event and bring a smile to their faces. We understand this and have therefore made it our mission to offer event catering services that are fun, unique, and interactive to truly add the wow factor to your function. Impress your guests with everything from
About: Ripple & Roll is a young and fun brand whose aim is to bring ice cream to the people of the UK in a they've never seen before. The show begins with our signature West Country cream being poured onto - 30-degree plates. This is then combined with your choice of ingredient, ranging from fresh fruit
Recent review: We have been using Jamie and the Team @ Dorset Catering for 4 years now and have never been disappointed. They can cater for intimate events for 10 or for our yearly Car Show for 2500 there capabilities have no limits. Would not hesitate to recommend.
About: We are the South West's most popular authentic Mexican and Central American street food trader and we are famous for our tacos. We love a wedding, party or whatever your reason for serving your guests fresh delicious tacos. You may have seen our beautifully restored 1978 Renault Estafette roaming
About: Napkin Catering is a relatively new company, Launched in early 2015, re-branded in 2018 we set our focus on becoming one of the best catering companies in the south west! What makes us stand out from the rest is our ethics when it comes to food & the environment! We only use free range, fair trade &
About: We are now trading from Sturminster Newton North Dorset but have been established in Dorset for 15 years and have been providing high quality fast food to our customers across the southwest and beyond.... We are also currently running a unit at Thruxton Motorsport Centre next to the kart track so i


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Arc la Rambla
Property Details
Property Location
In the heart of Barcelona, Arc la Rambla is within a 5-minute drive of Centre d'Art Santa Monica and Columbus Monument. This hotel is 0.4 mi (0.7 km) from Barcelona Wax Museum and 0.5 mi (0.8 km) from Palau Guell.Rooms
Make yourself at home in one of the 98 air-conditioned guestrooms. Complimentary wired and wireless Internet access keeps you connected, and satellite programming provides entertainment. Bathrooms have bathtubs or showers and hair dryers. Conveniences include phones, as well as safes and desks.Amenities
Make use of convenient amenities, which include a television in a common area and tour/ticket assistance.Dining
Buffet breakfasts are available daily from 7 AM to 11 AM for a fee.Business, Other Amenities
Featured amenities include a computer station, a 24-hour front desk, and multilingual staff.Attractions
Distances are displayed to the nearest 0.1 mile and kilometer.
La Rambla - 0.1 km / 0.1 mi
Centre d'Art Santa Monica - 0.1 km / 0.1 mi
Maritime Museum - 0.3 km / 0.2 mi
Columbus Monument - 0.4 km / 0.2 mi
Barcelona Wax Museum - 0.7 km / 0.4 mi
Rambla del Raval - 0.8 km / 0.5 mi
Palau Guell - 0.8 km / 0.5 mi
Rambla del Raval - 0.9 km / 0.5 mi
Placa Reial - 1 km / 0.6 mi
Teatre Principal - 1 km / 0.6 mi
World Trade Center Barcelona - 1.2 km / 0.7 mi
Port Vell - 1.4 km / 0.8 mi
Maremagnum - 1.6 km / 1 mi
Basilica de Santa Maria del Mar - 1.6 km / 1 mi
Sant Antoni Market - 1.6 km / 1 mi
The preferred airport for Arc la Rambla is Barcelona (BCN-Barcelona Intl.) - 15.3 km / 9.5 mi
Hotel policy
Bed Types are requests only and may not be honoured at the hotel if availability does not permit.
Property Policies
Extra-person charges may apply and vary depending on property policy.
Government-issued photo identification and a credit card or cash deposit are required at check-in for incidental charges.
Special requests are subject to availability upon check-in and may incur additional charges. Special requests cannot be guaranteed. No onsite parking is available. Please note that cultural norms and guest policies may differ by country and by property. The policies listed are provided by the property. Additional policies and fees may apply when booking more than 5 rooms. For more details, please contact the property using the information on the reservation confirmation received after booking.
Important Information
Please note, there is important information about this property to know before you arrive.
Know Before You Go
- Cash transactions at this property cannot exceed EUR 2500, due to national regulations. For further details, please contact the property using information in the booking confirmation.
- Only registered guests are allowed in the guestrooms.
The following fees and deposits are charged by the property at time of service, check-in, or check-out.
- Fee for buffet breakfast: EUR 12 for adults and EUR 6.00 for children (approximately)
- Crib (infant bed) fee: EUR 25 per day
- Rollaway bed fee: EUR 25 per day
The above list may not be comprehensive. Fees and deposits may not include tax and are subject to change.
Mandatory Fees and Taxes
You'll be asked to pay the following charges at the property:
- A tax is imposed by the city: EUR 0.72 per person, per night, up to 7 nights. This tax does not apply to children under 17 years of age.
We have included all charges provided to us by the property. However, charges can vary, for example, based on length of stay or the room you book.
- -Roll-in shower
- -Accessible bathroom
- -24-hour front desk
- -Safe-deposit box at front desk
- -Breakfast available (surcharge)
- -Elevator/lift
- -Television in common areas
- -Computer station
- -Multilingual staff
- -Tours/ticket assistance
- -Number of floors - 5
- -Total number of rooms - 98
- -Luggage storage
^ Earn 9 Qantas Points per AU$1 spent on eligible Qantas Hotels worldwide. Offer ends 11:59pm (AEDT) Thursday 21 February 2019. Eligible Qantas hotels excludes Classic Hotel Rewards. Qantas Points are not earned on any amounts payable directly to the hotel. Conditions apply
* Businesses earn 1 Qantas Point per AU$1 spent on eligible Qantas Hotels worldwide. Eligible Qantas hotels excludes Classic Hotel Rewards. A business must be a Qantas Business Rewards Member to earn Qantas Points for your business. Qantas Points are not earned on any amounts payable directly to the hotel. Conditions apply
∼ Saving is off the hotel's generally available rate for the same property, room type, days, inclusions and conditions
† Includes fees payable in local currency direct to hotel. Prices in AUD are approx and based on today's exchange rate.
Hotel ratings and reviews provided by TripAdvisor


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We have blocked your Writing essays about literature acheson pdf address, please contact us to find out more. Enter the characters you see below Sorry, we just need to make sure you're not a robot. American novelist, short-story writer, and playwright.
Born February 7, 1885, in the village of Sauk Centre, Minnesota, Sinclair Lewis began reading books at a young age and kept a diary. Lewis, was a physician and a stern disciplinarian who had difficulty relating to his sensitive, unathletic third son. Lewis's mother, Emma Kermott Lewis, died in 1891. Lewis's earliest published creative work—romantic poetry and short sketches—appeared in the Yale Courant and the Yale Literary Magazine, of which he became an editor. After graduation Lewis moved from job to job and from place to place in an effort to make ends meet, write fiction for publication and to chase away boredom. Lewis's first published book was Hike and the Aeroplane, a Tom Swift-style potboiler that appeared in 1912 under the pseudonym Tom Graham.
Sinclair Lewis's first serious novel, Our Mr. On May 14, 1928, he married Dorothy Thompson, a political newspaper columnist. Later in 1928, he and Dorothy purchased a second home in rural Vermont. They had a son, Michael Lewis, in 1930. Their marriage had virtually ended by 1937, and they divorced in 1942.
As early as 1916, he began taking notes for a realistic novel about small-town life. Work on that novel continued through mid-1920, when he completed Main Street, which was published on October 23, 1920. Sinclair Lewis's former residence in Washington, D. It was awarded the Pulitzer Prize, which Lewis declined, still upset that Main Street had not won the prize. The novel was denounced by many religious leaders and banned in some U.
He portrayed them as leading essentially pointless lives in spite of great wealth and advantages. During the late 1920s and 1930s, Lewis wrote many short stories for a variety of magazines and publications. In 1930 Lewis won the Nobel Prize in Literature, the first writer from the United States to receive the award, after he had been nominated by Henrik Schück, member of the Swedish Academy. In the Academy's presentation speech, special attention was paid to Babbitt.