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CITY HOOKUP PONDICHERRY INDIA

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CITY HOOKUP PONDICHERRY INDIA

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Watch the sunrise or take a stroll in the Promenade or Rock Beach as it is also
called. The main Pondicherry beach has no sand stretching into the ocean but
rather a wall of jagged rocks. The pavement is clean, lined with trees, benches,
and free of traffic.

Watch the sunrise at dawn and streets lights twinkle at night. Head out of the
city to find many beaches ideal for swimming, sunbathing, and even surfing. The
Chunnambar Boat house located 8 km away from the main city is a popular tourist
spot.

Go boating in the backwaters; take a boat to the Paradise Beach which is an
island beach ideal of relaxing, and enjoy a picnic surrounded by waters.
Chunnambar also offers tree houses for overnight stays, and a restaurant for
meals and snacks. It is a perfect adventure spot. Go rowing, fishing, swimming,
bird watching, trekking or view the sunrise from a tree house, or simply
meditate. Paradise beach is good enough to figure in any itinerary of places to
visit in Pondicherry in one day. That aside it is a very well maintained park. A
flower show is conducted every year attracting large crowds.

Not easy to find, Serenity Beach is short drive from city. Nothing special but
this is the nearest beach with some sand.


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This is a beautiful 17th century Our Lady of the Immaculate Conception Cathedral
built by the French and renovated many times in it long history. Do visit in the
evening little before sunset for perfect photo opportunity. It is one of the
Pondicherry Beach that does not see much crowds. These places to visit in
Pondicherry can part of your 2 days or 3 Days trip itinerary. Ruins of ancient
era — Arikamedu , the only site India to have confirmed Roman Empire connections
in India.

In it time this place must have been an important center for jewelry and glass
work. At 7 Kms from the city is the town of Arikamedu, an excavation site where
the Roman artifacts displayed in the Pondy museum were found. Though abandoned,
this site attracts curious visitors. Close to Chidambaram are the Mangrove
forests of Pichavaram , which is one of the largest in the world.

Backwater country boat rides take visitors into the dense forests for
unparalleled experience. Pichavaram mangrove forest are the second largest
mangroves in India after the Sunderbans. Pichavaram is 78 Kms from Pondicherry.
The backwaters of Pichavaram are a great place for water activities such as
kayaking.

Be a day or a week, down here is a list of things to do while holidaying in
Pondicherry. The Boulevard is one of its kind — series of shaded cobbled streets
lined with colonial houses. Most of them in the hues of white, grey, and yellow
surrounded by the promenade on one side, and typical bustling streets of south
India on the other. The French quarter is furthermore, the home to some of the
finest attractions of the town. The French consulate is a fine place to start
the tour by having a peek into the French connection of the city.

The busiest part of the French quarter also happens to be the calmest one — Shri
Aurobindo Ashram. An apt place for meditation amidst deafening silence,
alongside the Manakula Vinayagar Temple.

Manakula Vinayagar Temple is the most famous temple of the city. It is known for
the blessings given by its resident elephant.


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The tranquil parts of the town are the Bharathi Park, and the nearby museum
which is small but even so, has many artifacts on display. A church is the most
expected sight from a colonial town and not to disappoint Pondy has its own
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We stopped our car and walked down to the sandy beach to book our stay at the
popular Auroville Waves resort. Also, it had been nine long hours since our last
meal and we were very hungry. In front of us was a stretch of beach filled
mainly with foreigners.

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And there was a rope running from the road towards the waters separating that
part of the beach from the stretch of the coast opposite the Auroville Waves. It
seemed like some sort of demarcation and there was a board with a message
written in Tamil. None of us knew Tamil and we walked towards the other side of
the rope. At that moment, we heard whistles from a nearby shack. There were two
men in Security uniform and a hefty man who resembled like some of the bouncers
in Bangalore Pubs.

All the three men were Indians. They made signs which indicated us to keep away
from this stretch of Beach. Confused, we decided to walk up to them and find out
what was the issue. But we are very hungry and have travelled a long way from
Bangalore. We will have lunch here. Come from the back entrance facing towards
the road. At this point, we felt humiliated and walked out of that place. It was
shocking to receive such a treatment in India for the simple reason of being an
Indian.

It is high time we stopped pointing fingers at the West for racial
discrimination we are subjected to in foreign countries. We ourselves are
discriminating our own people based on race. This definitely was the worst, but
not the first time I had experienced racial discrimination. In the past, I had
faced a similar issue in Goa, which coincidentally is also another beach holiday
destination drawing lot of foreign tourists and is also a former European
colony. And incidents of such racial discrimination are experienced by other
Indian domestic travelers too. In a restaurant, when he questioned the waiter
for overpricing a meal, the waiter shot back at his taxi driver telling him not
to bring Indians as they only want to serve foreigners.

It is hurting to know that such incidents are happening in some of the most
famous holiday destinations of our country. Copper Wires Pondicherry.

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DATING OVER 40 NEAR TOLUCA MEXICO

Contents:

TOLUCA EDITIONS Association between dating violence and personality type in
Mexican university students Daily life and social customs Original Research
ARTICLE Mexico - Daily life and social customs | Britannica



BHVO-2 and several in-house standard materials were used for quality control
during the analytical session. Trace element contents in the whole rock samples
were obtained on the same fused glass beads by laser ablation inductively
coupled plasma mass spectrometry.

After XRF analysis, glass beads were crushed and mounted on adhesive tape with
the side of the bead not analyzed by XRF facing to the top. On each glass bead,
we collected and averaged 3 spot analyses. The largest differences for averaged
spots were obtained on Mo RSE: In this study we present mineral and glass
chemistry for 19 eruptions from Nevado de Toluca, which were selected to cover
the entire eruptive history of the volcano. For each of the studied eruptions,
we analyzed one petrographic section, for which between 8 and 15 BSE images each
were obtained in order to reveal textures and internal mineral zonation
features.

Typically, we analyzed linear rim to core profiles of 10—20 crystals for each
mineral phase in the individual petrographic sections.

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Mineral phases plagioclase, pyroxenes, Fe—Ti oxides and amphiboles were analyzed
using the wavelength-dispersive x-ray spectrometer of the electron probe
microanalyzer. The raw amphibole totals outside the range Compositions that
indicated mixed analysis of silicate minerals and glass were also discarded. In
total, 2, plagioclase, 2, pyroxene, and 1, amphibole analyses are presented in
this study.

In each section, typically 15 groundmass analyses were carried out and averaged.
Melt inclusions were hosted in either pyroxene or amphibole. Alkali element
measurements were performed first in the sequence to mitigate diffusive loss.


TOLUCA EDITIONS

Dowgwillo, E. Inthe Spanish conquered the Valley of Toluca. Cashman, K. The
covariates considered as potentially confounders in multivariate models were:
age, smoking, alcohol consumption, childhood abuse, drug use other than tobacco
and alcohol Blom et al. Edward Barber and Jay Osgerby have designed a special
quadrilateral box in ebony wood as a container for this work. Blatter, D.
Further, the sample surface was cleaned by 10 laser pulses prior to each
measurement. The long-term dating over 40 near Toluca Mexico trend toward more
silicic compositions observed in bulk-rock and mineral chemistry may be
explained by a range of changing conditions either related to the rates of magma
recharge, the relation of eruptive to intrusive fluxes, and the modalities and
rates of magma reservoir growth. Petrology, magma mixing, and immediate sources
of volatiles for the present eruption. Of these, one simulation at relatively
high magma flux of Each side has its own. However, quantitative estimates of
average rates of magma input are difficult to obtain from the volcanic record as
only a fraction of magma injected into the plumbing system is erupted 2633

The mineral, glass and groundmass compositions analyzed in this study were used
to estimate the pressures, temperatures, and oxygen fugacity of Nevado de Toluca
magmas using a range of geothermobarometric techniques. Amphibole
crystallization temperatures and pressures were calculated for euhedral
outermost amphibole rim compositions using Equation 7b from Putirka by iterative
solution, which requires input of amphibole and liquid composition, as well as
an estimate of water content.


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STUDENTS

Of the 30 biotite grains that were step-heated for 40Ar/39Ar dating (methods are
described in Appendix A). A ka History of Dacitic Magmatism at Nevado de Toluca,
Mexico: Petrological, 40Ar/39Ar Dating, and Experimental Constraints on.

We used average groundmass for each of the studied eruptions to approximate the
input liquid composition. In order to assess equilibrium between the assumed
liquid and outermost rim amphibole, we discarded amphibole-liquid pairs with
mineral-melt exchange coefficient K D Fe t —Mg outside the range 0. However, the
resulting average differences in pressures and temperature calculations of 0.
Amphibole crystallization temperatures can also be estimated independent of
liquid composition and pressure, not necessarily with worse precision and
accuracy when compared to amphibole-liquid thermometers Ridolfi and Renzulli, ;
Putirka, We calculated liquid-independent amphibole temperatures using Eqn.

Several samples contain both clino- and orthopyroxenes, but equilibrium between
outermost rim compositions based on a instead of an Kd Fe—Mg of 1. We thus
calculated 2-pyroxene temperatures only on these samples, using Eq. The
composition of coexisting titanomagnetite and ilmenite was used to constrain
temperatures and the oxygen fugacity for various eruptions of Nevado de Toluca.
We used the model of Ghiorso and Evans to calculate the temperatures of Fe—Ti
exchange between touching equilibrium pairs Bacon and Hirschmann, of
titanomagnetite and ilmenite.

Oxygen fugacity is reported as values relative to Nickel-Nickel-Oxide buffer. We
used heat conduction modeling, in order to simulate the temporal evolution of
temperatures in crustal rocks subjected to repeated magma injection. An explicit
finite difference scheme was used to solve the axisymmetric formulation of the
heat equation, which can be written as:.

As we do not aim to model the particular phase equilibria of Nevado de Toluca in
this study, but to investigate the general controls on compositional modes, we
used a hypothetical linear melt fraction temperature relation in the presented
model calculations. While the specifics of melt-fraction temperature relations
impact on compositional distributions Caricchi and Blundy, a , it does not
impact the direction of compositional change as a function of magma recharge or
extraction rate Weber et al.

A temperature dependent thermal conductivity k was implemented in the model
based on the experiments of Whittington et al. The numerical code used in this
study has been benchmarked against existing models Caricchi et al. In order to
investigate the impact of changing extrusive:intrusive E:I ratio of a magmatic
systems compositional diversity, we implemented heat and mass removal in the
model.

In such simulations, sills were removed at a rate that is equivalent to E:I
ratio of 0. This was accomplished by removing sills matching the previous
injection site and dimension, which ensures removal of magma at the highest
temperature in the reservoir, by advecting the temperature field upwards.

We performed petrological modeling, in order to invert the computed temperature
distributions into potentially eruptible magma chemistry. All petrologic
calculations were carried out using the hypothetical liquid line of descent
presented in Supplementary Table 7.

For a detailed description of the calculation procedure, the reader is referred
to Weber et al. We present and analyze a combined dataset of 97 bulk rock major
and trace element analysis for the long-term eruptive history of Nevado de
Toluca volcano. In agreement with previous studies of the long-term history of
the volcano, the major element geochemistry is focused on dacite throughout the
history of the volcano with an average SiO 2 content of Andesites are less
frequently erupted from Nevado de Toluca but occur in all eruptive stages.

Samples erupted from the main volcano show typical trends of increasing
incompatible major element components e. Different eruptive stages show slight
differences in slope and variance in bivariate plots of MgO vs.


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FeO total Figure 4B. Melt inclusions, hosted in amphibole and orthopyroxene, are
consistently rhyolitic in composition with average silica contents of Summary of
major and trace element systematics of Nevado de Toluca volcano. A Total alkali
vs. Shown are Pre-Nevado group black squares , Monogenetic cones orange
triangles , Old Nevado stage gray rhombus , Domes gold triangles , Recent Nevado
stage red circles , and Young Pyroclastics beige squares. Matrix glasses and
melt inclusions are plotted as turquoize and light blue circles, respectively.

Crystalline groundmass measurements are indicated by small light green circles.
Dashed circle indicates samples with elevated K 2 O contents corresponding to
alkaline cones. C Primitive mantle normalized trace element variation diagram
Sun and McDonough, Primitive mantle normalized trace element pattern of all
analyzed samples show typical features of subduction related magmatism such as
negative Nb—Ta anomalies and enrichment of large ion lithophile elements LILE
like Cs, Ba or Sr Figure 4C.

This group contains samples from all eruptive stages, including some monogenetic
cones. Chemical differences between these samples and the main volcano are also
evident in major elements, in particular higher K 2 O contents Figure 4A.


ORIGINAL RESEARCH ARTICLE

These distinct compositions are only evident in three samples from silicic Domes
surrounding the main volcano and are consistent with an important role of
amphibole fractionation during magma evolution Davidson et al. Representative
selection of petrographic features of basaltic andesite to dacitic volcanic
rocks in the Nevado de Toluca area.

All photomicrographs were imaged with back-scattered electrons BSE A Typical
phase assemblage of zoned plagioclase plag , zoned hornblende hbl ,
orthopyroxene opx and Fe—Ti oxides ox in unit 34 Ombligo Dome in the central
part of the crater. The groundmass gm is mostly composed of plag, glass and
oxides. Note also the resorption and overgrowth textures of plag crystals dashed
lines.

The gm is composed of plag and qtz and ox.

C Biotite bt , hbl and strongly zoned plag in U18 Lava with gm consisting of
plag, qtz and ox. D Strongly zoned opx with mafic cores dark and evolved
overgrowth rim compositions bright in crater unit Note the euhedral appearance
of plag, opx and hbl. E Reaction rims on mafic hbl and opx in U5 Raices lava.
The gm is composed of plag, qtz and ox. F Qtz xenocrysts with reaction corona of
cpx, opx and plag dominated groundmass and sparse disequilibrium olivine ol in
Tenango lava.

The gm is glassy with abundant elongated plag. We collected petrographic images
and determined the modes of macro-crystal and groundmass phases in 17 eruptions
from Nevado de Toluca volcano and two peripheral cones, spanning its entire
eruptive history of 1. A representative selection of BSE images Figures 5A—F
shows that the predominant phase assemblages are comprised of plagioclase,
orthopyroxene, amphibole and Fe—Ti oxides. Occasionally, quartz, clinopyroxene
and biotite are observed in the eruptive products. The mineral textures are
complex but similar in all studied eruptions from the main volcano.

Plagioclase textures are characterized by multiple resorption and overgrowth
zones, while pyroxenes and amphiboles show strong, but generally binary core to
rim zonation. The analyzed monogenetic eruptive products contain two-pyroxene
macro-crystal assemblages and a groundmass dominated by plagioclase microlites.
Average fractions of phenocrystals are 0. Samples from the early eruptive stages
i.

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Major and minor elements in silicate and oxide mineral phases from 19 eruptions
have been analyzed. FeO total contents in plagioclase show a large range between
0. Greater variation between the eruptive stages of Nevado de Toluca is evident
in FeO total contents, which show average values of 0. Amphibole crystals in the
studied eruptions are Ca-rich and can be classified as magnesio-hornblende and
pargasite. Individual eruptions show large differences in amphibole compositions
both in central tendency and variance for several elements Supplementary Figure
2.

For example, Al T per formula unit p. Much of this range is for instance
captured by amphibole from the 31 ka cal. BP BAF28 eruption average: 1. In
accordance with zonation pattern in BSE images Figures 5A—E , chemical
compositions of Nevado de Toluca amphiboles are often bimodal with different
compositions of crystal cores and rims Supplementary Figure 2.

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Systematic differences between the eruptive stages and amphibole compositions
are, however, not evident. However, high En and Cr 2 O 3 in heavily zoned
crystal cores c. Similar to opx, cpx crystal show strong compositional zoning
with Cr 2 O 3 contents of up to 1. A Data spanning the entire 1.


MEXICO - DAILY LIFE AND SOCIAL CUSTOMS | BRITANNICA

Clino- and orthopyroxene cores show elevated Cr 2 O 3 contents that are
developing toward lower values in two main trajectories for both pyroxenes black
arrows. Dashed areas indicate the silicic composition typically found in crystal
rims. Symbols and color coding reflect different eruptions.

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