Dating sites can Thames New Zeland

Non-smoking hotel. Non-smoking rooms.

Auckland Intl Airport 42 mi See all flights. Rental Cars See all Thames rental cars. Thames School of Mines and Mineralogical Museum. Write a review. Traveler rating. Selected filters. All reviews were lucky to get a table the main street fish and chips guinness. Auckland Central, New Zealand 25 contributions 3 helpful votes. Pleasing Place. Taking an old friend for lunch we were looking for some close to him. Well that didn't work out so we headed to Thames.

Went to a couple of place that only offered burgers and pizzas with craft beer. Walked straight back out. Heade into the main street and saw the Junction. We were lucky to get a table as they were fairly busy. Then I remembered it was fathers day , so we were very lucky. We saw some nice dishes on the menu which we would of had fore dinner but all three of us decided on fish and chips.

We waited a little longer than expected but they were busy so no problem. We had drinks, one each , two beers and a Guiness. The waiters were friendly although noone mentioned the pork belly special which we might have liked. I noticed it when I was paying. The meals came and were of a decent size.

The fish was battered, fine by us, and was very nice , chips were very good and the salad was okay but we all thought it needed something extra.

But all in all it was a good meal in a nice place. Definitely the best place I saw in Thames and will certainly eat there again and recommend it also. Date of stay: September Cleanliness. Helpful Share. Corinne K wrote a review Sep Auckland Central, New Zealand 18 contributions 4 helpful votes. Great Food.

Stopped here for two meals, and both were superb.

This enables you to find exactly what you're after. Join our growing Waikato community and get connected with free mail, forums, blogs, IM, and chat. Meet singles worldwide looking for online dating, love, marriage, romance, or just someone to chat or hang out with. Quick search I am man woman. Seeking for man woman. Quick Statistics If you are a numbers nerd or love data, you will love these Thames members statistics that we have prepared in visually easy-to-understand manner. Password recovery.

Te Awamutu. Due to its weight and the very soft sediments in the Firth of Thames, the QR Vibracore was deployed in a gravity corer mode in order to recover undisturbed sediments from the very top layers. After cutting the —cm-long sediment cores into 1-m-long core segments, these were split along the c -axis into working and archive halves.

After opening, all cores were described sedimentologically and logged immediately with a handheld X-ray fluorescence XRF device see below. Archive halves of the principal cores also have been rescanned prior sampling with a XRF core scanner. Single-stage accelerator mass spectrometry was used to obtain radiocarbon ages on bulk organic matter Hirabayashi et al. Carbon incorporated in the sample was recovered as CO 2 Ishizawa et al. Pre-treatment of marine shell samples followed the protocol of Yokoyama et al. Nineteen samples from core NZ-M-4 were prepared for palynological analysis using the standard laboratory procedures Faegri and Iversen Samples were checked for Pinus spp.

Sample preparation and measurements were carried out with deionised, degassed and filtered water filter mesh size: 0. The obtained results provide the particle-size distribution of a sample from 0.

All provided statistic values are based on a geometric statistic. Limits of detection for elements analysed by pXRF are in the ppm range. From a range of elements analysed, only Pb and Zn are used. Each scan took 90 s with calibration checks made every 30 samples on a reference material Stainless Steel Calibration Check Reference Coin provided by Olympus for evaluation of accuracy.

Expecting anthropogenic impact only in the youngest sediments, sample spacing was 5 cm for the upper 21 cm of the cores and 10 cm further downcore. For quantification, 28 discrete samples of 20 g wet sediment were taken from the three principal cores at positions that cover the full range of Zn and Pb values according to the semi-quantitative XRF core scanner measurements. The net intensities for Pb and Zn in counts per second cps measured with the XRF Core Scanner were divided by the total cps from the according 30 kV run to normalise the data i.

These normalised net intensities from the XRF Core Scanner data were converted to element contents using linear regressions between XRF scanner-derived intensities and element contents measured on the corresponding 28 discrete samples measured quantitatively e.

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Jansen et al. The obtained data of the pXRF were calibrated using the same equation, but normalisation was not conducted as values given by the instrument were already in ppm. These cores consist of a dark greenish mud Munsell 5Y colour chart with only minor internal textures, which include thin layers of fine sand or shell debris. No lamination, burrowing or change in colour was observed. Core NZ-M-3 near Waihou river mouth is dominated by black middle to coarse sand with fine shell debris and had a smell of rotten fish.

In the sediments below cm depth, the sand alternates with black muddy layers similar to those described from the other cores, but very compact. For all three principal cores NZ-M-2, NZ-M-4, and NZ-M-7 , the 33 obtained 14 C dates show generally a consistent trend to become younger towards the top with the exception of only a few samples Table 2. Core NZ-M-7 shows slightly older ages and shows an age of years in cm sediment depth. Therefore, the pre-human era is covered in all three cores.

The 14 C data from mixed benthic foraminifera are generally younger than those obtained on bulk organic matter. Core NZ-M-4 has been analysed for the occurrence of pollen from Podocarpus spp. For the amount of Podocarpus spp. The first specimen of Pinus spp. In the very top sample at 17 cm depth, an extensive increase in Pinus spp.

Additionally, this is the only sample were a specimen of Olea europaea was found, another exotic plant to New Zealand with the earliest records of naturalisation in the s Heenan et al. Pollen data of core NZ-M-4 showing the absoluteabundances number per grams of the counted pollen types Podocarpus, Pinus, Olea europaea.

Core NZ-M-2 displays the already macroscopic observed change in grain size. Grain-size distribution of the three principal cores NZ-M-2 near river, coastal , NZ-M-4 near river, offshore and NZ-M-7 far from river , colour coding gives percentage of each grain-size class, varying from Therefore, lower contents of Pb and Zn are only resolved in the XRF Scanner data, giving a different linear regression equation for the two applied methods.

The lower beam energy results additionally in lower analytical precision of the pXRF Young et al. Calibrated pXRF data show a distinct and sudden peak in Pb and Zn in the upper part of six of the eight cores with varying contents and depths of onset Fig. Values below the peaks are very constant within the cores as well as between the cores with values around 12 ppm for Pb and 50 ppm for Zn.

Regional and vertical distribution pattern of Pb and Zn contents in the Firth of Thames sediments obtained by calibrated portable XRF data.

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Circles represent core locations, red circles—three high-resolution principal cores, black circles - other cores. The cores NZ-M-7 and NZ-M-8 located furthest north have less pronounced peaks with lower contents and onsets of the peaks higher up in sediment column. Nevertheless, all these four cores show the same pattern in peak structure with a pronounced increase and a following decrease in Pb and Zn content towards the core top. In the lower part of core NZ-M-4, rather constant values around 12 ppm for Pb and 57 ppm for Zn can be observed.

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At 54 cm core depth, both values increase steeply to a maximum at 34 cm depth and show from there a general declining trend towards the top of the core. The heavy metal content at the sediment surface is still clearly above the background values found in the lower part of the core. The average content of this section is 82 ppm for Pb and ppm for Zn. Core NZ-M-7 shows a very similar pattern, but with generally lower values and the onset of the strong increase higher up in the core at 26 cm. High-resolution calibrated XRF Scanner data for the three principal cores with the interpreted age zonation of the pre-human, Polynesian and European Era.

Averaged Pb and Zn contents were calculated from all values above the peak onset and below the peak onset respectively. Solid lines are based on the stratigraphic frameworks.