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The area with a highest sand movement activity is characterized by small dunes, with overlapping reflector packages exhibiting reflections which dip up to 25°.
To make removal easy, only dip up to the base of your hand, before it starts narrowing to your wrist.
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Pronounced westerly (seaward) dips up to 25° unlike the horizontal lava pile of the Western Ghats (Auden 1949; Sheth 1998).
When dune activity is moderate, dunes are higher (up to 5 m height) and their internal structure shows low-angle dip reflections except for the avalanche face, where dips up to 22° are identified.
The slopes of Dharamshala region are steeply dipping up to > 41° with upper 5 m to 10 m cover of fluvial deposits or the debris cover which is easily prone to sliding under adverse conditions.
Fully frosted microscope slides (SuperFrost Plus® Menzel GmbH, Braunschweig, Germany) were dipped up to one-fourth the frosted area in a hot 0.9% normal-melting-point agarose (Roth, 2268.2; Karlsruhe, Germany) in PBS.
By performing spectrally resolved transmission measurements pronounced Bragg grating behaviour is observed, with the transmission dip increasing (up to ∼12 dB) with the increasing grating length.
The locations of these observatories, shown in Fig. 1(a), are located from the dip equator up to the Sq focus near Sabhawala (30.37°N Geographic Latitude).
A 7-m-thick succession of inclined heterolithic stratification (IHS) is developed in the middle intertidal portion, where it consists of thinly interlaminated sands and muds with a dip angle up to 10°.
Considering the results reported by Moudden and Forbes (2013), who found larger TDT amplitudes in SABER temperatures from 2002 to 2011 near the equator, a link between TDT and 8-h ES at very low southern latitudes might be possible, because the magnetic field lines reveal dip angles up to 60°.
It can recharge USB devices and will survive a 30-minute dip in up to 3.3 feet of fresh water.
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