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Aarwin’s Guide to CFA level 1 Quantitative Methods notes gives you the much needed guidance before your exam. The Quantitative Methods is a very important and pivotal section unique to the CFA Level 1 exam. For more information check our blog.
CP 9750 and CP 9740 lead a westbound potash train as it starts to cross the High-Level Viaduct in Lethbridge, Alberta. At the rear of the train was CP 9778 - photographed on the CP Taber subdivision in August 2016
Planovergang ved Skulerud stasjon på Urskog-Hølandsbanen
Level crossing at Skulerud station on the abandoned Urskog-Høland line
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Oval Spring is a geyser in the Sawmill Group of Yellowstone's Upper Geyser Basin. It is located about 40 meters north-northeast of Sawmill Geyser and 13 meters north-northwest of Penta Geyser. The circular basin is about 9 meters in diameter. A centrally-located, irregularly elongated vent is oriented northeast-southwest and is about 1 by 2 meters in size. The basin is floored by geyserite, which varies in surface morphology from nodulose to smooth-but-slightly-undulating to terracetted. Shallow, irregularly dendritic channels are present in the geyserite floor that drain water toward the central vent.
Water levels in Oval Spring vary depending on the nature of eruptive activity in other Sawmill Group geysers. Observed conditions include: low to very low water levels (but still visible), moderately high water levels, and a water-filled basin with slight overflow. Observed behaviors range from calm pools to pulsing/undulating to splashing eruptions (see pictures elsewhere in this photo album).
From 2013 to 2016, eruptions at Oval Spring were often reported. It had a years-long dormancy from fall 2016 to spring 2021. Eruptions have since been reported from June 2021 to summer 2024 at least.
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I've put too many filters on and that's why there is vignetting. Why there is building tilt is a question best answewred by the architects.
High Level Segment of the 2015 Conference on Disarmament, Palais des Nations. Monday 2 March 2015. Photo by Violaine Martin
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