Clean and simple but feature-rich, the Ignite sets a new benchmark for fitness watches that recommend workouts and track sleep and recovery. This is a serious all-round fitness tool at a very reasonable price. The Polar Ignite is a workout partner with a difference. The Ignite does exactly that. It still tracks those mainstay fitness activities like running, cycling and swimming as well as any other Polar watch, but the Ignite is geared towards the simple common goal of getting you into better shape. These brand new features combine to help you stay inspired with daily workout ideas for different sessions, and to maintain good balance, helping you spot when and how hard to train. Including plenty that even sport-specific goal-chasers will like. It sits in the middle of the budget sports and fitness watches bracket alongside the likes of the Garmin Forerunner 45 and the Coros Pace. The Ignite has a striking simplicity. The display itself is bright and crisp.
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The Samsung Galaxy Note 10 delivers epic battery life and a super-bright screen in a phenomenally compact design, though its software features could use some work. Samsung built the Galaxy Note brand on delivering the best big-screen phones around, but the best thing about the Samsung Galaxy Note 10 is how delightfully small it is. The 6. The Note 10 also boasts several S-Pen enhancements including gestures , introduces helpful video recording features and a new way to mirror the phone on a PC.
The idea of a compact phablet might sound crazy, but it actually makes a whole lot of sense when you use it. However, there are some trade-offs. Today the Note 10 is still a great device, even with the Samsung Galaxy Note 20 looming on the horizon. The new Note raises the screen size to 6. It also features half the storage and no microSD slot for expandability.
In other respects, the Note 20 seems like a worthy update; you can read our Samsung Galaxy Note 20 vs.
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A lmost everyone I know who has tried out dating apps or sites has had encounters that have not been quite as advertised, from the married man on Grindr who revealed plenty about — and of — himself, but never his face, to the date who was a decade older than her profile pictures, and lied about the children she could not have had were she the age she said she was. These days, it seems to be part of the deal to expect these small-scale scams, and to sift through them on the promise that there might be a good one in the pack.
And often, there is.
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With increased battery life, bigger screen and better menu system, the Garmin Fenix 6 Pro is a definite improvement over its predecessor. It might be a bit too heavy for some runners, though. By Matt Kollat TZ. Sometimes the stars align and you get to test a top Garmin multisport smartwatch when you are training for a half marathon , doing long distance runs and hitting the gym multiple times a week. This is exactly what happened to me when I was offered a chance to write a Garmin Fenix 6 Pro review.
Let me start with a disclaimer: there is no way you can test all the functionality in a multi-sport smartwatch like the Garmin Fenix 6 Pro in span of weeks. It caters for a variety of activities and some features take months to test — for example the Garmin Coach, a feature not exclusive with the Garmin F6 Pro, but available on it. Here’s the latest. Saying that, a lot can be and w as tested during this last few weeks, including running and cycling metrics, GPS and heart-rate precision, build-quality, battery life and performance, and so on.
Not only is the Garmin Fenix 6 Pro one of the best running watches , it’s actually one of the best outdoor watches , too. This high-end smartwatch packs features that’ll keep everyone from golfers, to gym-bunnies, to skiiers and hikers happy. Read on for our full Garmin Fenix 6 Pro review. The Garmin Fenix 6 Pro has a bigger screen and more efficient power saving options compared to its predecessor.
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It’s been eight years since the FZ50 was introduced, so we can’t imagine too many people are still waiting, but in some respects it appears Panasonic has finally created a replacement for that much-missed model. Taken as a whole, the FZ can almost be seen as a synthesis between the two cameras. Like the RX10, the FZ features a 20MP 1″-type MOS sensor and the suspicion has to be that it’s a Sony chip , but, rather than the Sony’s mm equivalent zoom range, the Panasonic reaches from 25 to mm equivalent.
To stop the whole thing becoming enormous, the FZ’s lens is slower than the Sony’s: its maximum aperture rapidly drops from F2. The FZ is a similarly sized camera but the eight years of technological development that underpin it mean it’s able to offer significantly higher resolution in terms of its viewfinder, rear screen, pixel count and video output.
Panasonic has recently been pushing the superzoom sector with the likes of its constant F2.
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If you would like to be involved in its development, let us know – external link. A Miocene continental section in Spain: the light and dark couplets reflect 23, year precession cycles. Astounding new techniques let geologists date events that happened hundreds of millions of years ago to within , years. Dan Condon explains. For geologists, it’s all about timing. Questions we often ask when trying to understand geological processes or events that occurred millions of years ago are quite simple: when did it happen, how fast and in what order?
The answer can be straightforward if you are only interested in rough estimates, say within the nearest million, or ten million years. But, if we need to piece together the order of events to recreate past climates then rough estimates aren’t good enough. Researchers are using increasingly sophisticated models to simulate past climates as well as to explore how the Earth system will change in response to increasing CO 2 levels. Testing these models requires equally sophisticated calibration of the geologic record to assess that the models accurately simulate the various components of the Earth system.
A new international initiative is helping with this calibration. Quantifying geological time has been central to understanding the Earth system and its evolution. Knowing the age of certain rocks, be it a thick accumulation of volcanic lava or an extinction layer, allows us to say something about causality. The extinction of the dinosaurs at the end of the Cretaceous period, ‘about’ 66 million years ago, is a good example of such cause-and-effect arguments.
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The decision hinges on what size the market for the product will be. Possibly demand will be […]. Possibly demand will be high during the initial two years but, if many initial users find the product unsatisfactory, will fall to a low level thereafter. Or high initial demand might indicate the possibility of a sustained high-volume market. If demand is high and the company does not expand within the first two years, competitive products will surely be introduced.
If the company builds a big plant, it must live with it whatever the size of market demand. If it builds a small plant, management has the option of expanding the plant in two years in the event that demand is high during the introductory period; while in the event that demand is low during the introductory period, the company will maintain operations in the small plant and make a tidy profit on the low volume. Management is uncertain what to do. The new product, if the market turns out to be large, offers the present management a chance to push the company into a new period of profitable growth.
The development department, particularly the development project engineer, is pushing to build the large-scale plant to exploit the first major product development the department has produced in some years. The chairman, a principal stockholder, is wary of the possibility of large unneeded plant capacity. He favors a smaller plant commitment, but recognizes that later expansion to meet high-volume demand would require more investment and be less efficient to operate.
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Research article 17 Apr Correspondence : Paul D. Zander paul. The ability to measure smaller samples, at reduced cost compared with graphitized samples, allows for greater dating density of sediments with low macrofossil concentrations. Radiocarbon samples analyzed using gas-source techniques were measured from the same depths as larger graphitized samples to compare the reliability and precision of the two techniques directly.
The reliability of 14 C ages from both techniques is assessed via comparison with a best-age estimate for the sediment sequence, which is the result of an OxCal V sequence that integrates varve counts with 14 C ages. No bias is evident in the ages produced by either gas-source input or graphitization. The effects of sample mass which defines the expected analytical age uncertainty and dating density on age—depth models are evaluated via simulated sets of 14 C ages that are used as inputs for OxCal P-sequence age—depth models.
Nine different sampling scenarios were simulated in which the mass of 14 C samples and the number of samples were manipulated. The simulated age—depth models suggest that the lower analytical precision associated with miniature samples can be compensated for by increased dating density.