The gesture of referencing Kuti's performance forms a line between Aspen and Berlin; Berlin and Lagos; the lines continue to be rendered.
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If the "ka" is moving vertically (up and down), it can only capture tokens in a horizontal direction that it forms a line with. Likewise, if the "ka" moves horizontally (left and right), then it can only capture tokens in a vertical direction that it forms a line with. The game is unrelated to any other board game. It is perhaps remotely related to Fanorona.
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Loch Ness lies along the Great Glen Fault, which forms a line of weakness in the rocks which have been excavated by glacial erosion, forming the Great Glen and the basins of Loch Lochy, Loch Oich and Loch Ness.
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Rhinconichthys is an extinct genus of bony fish which existed during the upper Cretaceous period. Along with its close cousins the great-white-shark-sized or larger Bonnerichthys and the immense Leedsichthys, Rhinconichthys forms a line of giant filter-feeding bony pachycormid fish that swam the Jurassic and Cretaceous seas for over 100 million years.
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There is no central peak at the crater's midpoint. A widely spaced row of tiny craters forms a line westwards from the north rim of Schröter. Professor W. H. Pickering produced drawings of this crater displaying eruptions of steam that he believed he witnessed. This transient lunar phenomenon was not confirmed by other observers.
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First, one team is designated as a Khar () team, and the other team is designated as the Polis () team. The Khar team forms a line in this manner: First, one person leans his back against a wall. This person is called Mikh (). The Mikh person forms a lock with his hands, and keeps his locked hands in front of himself.
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A closed human mouth. While shut, the orifice of the mouth forms a line between the upper and lower lip. In facial expression, this mouth line is iconically shaped like an up-open parabola in a smile, and like a down-open parabola in a frown. A down-turned mouth means a mouth line forming a down-turned parabola, and when permanent can be normal.
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The Hudsonian whiteface has a length of . Male dragonflies are black and marked with red on the thorax and the abdomen. The elongated spots on the abdomen are possibly pointed on one end, this forms a line along the length of the top side of the abdomen. The female is a dark brownish color and marked similarly to the male except the markings are yellow instead of black.
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At the western edge of Cody, a deep canyon formed by the Shoshone River provides the only passage to Yellowstone's Eastern Entrance. At its mouth and rising above Cody are Rattlesnake Mountain on the north side and Cedar Mountain on the south side. Much of Cody has views of Heart Mountain, whose peak is directly north of Cody, and the Carter Mountain massif, which forms a line with peaks above , some to the south.
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In this case, 1D filtering is not sufficient, since clutter can overlap the desired target's Doppler from multiple directions. The resulting interference is typically called a "clutter ridge," since it forms a line in the angle-Doppler domain. Narrowband jamming signals are also a source of interference, and exhibit significant spatial correlation. Thus receiver noise and interference must be considered, and detection processors must attempt to maximize the signal-to-interference and noise ratio (SINR).
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The clivus is an important landmark for checking for anatomical atlanto-occipital alignment; the clivus, when viewed on a lateral C-spine X-ray, forms a line which, if extended, is known as Wackenheim's clivus line. Wackenheim's clivus line should pass through the dens of the axis or be tangential to it.McKenna DA, Roche CJ, Lee KW, Torreggiani WC, Duddalwar VA. Atlanto-occipital dislocation: case report and discussion. Can J Emerg Med 2006; 8(1):50-3.
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A French squadron forming the line of battle circa 1840. Drawing by Antoine Morel-Fatio. British and Danish ships in line of battle at the Battle of Copenhagen (1801) In naval warfare, the line of battle is a tactic in which a naval fleet of ships forms a line end to end. Its first use is disputed, variously claimed for dates ranging from 1502 to 1652, with line-of-battle tactics in widespread use by 1675.
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The dual of a line (a curve of degree 1) is an exception to this and is taken to be a point in the dual space (namely the original line). The dual of a single point is taken to be the collection of lines though the point; this forms a line in the dual space which corresponds to the original point. If is smooth, i.e. there are no singular points then the dual of has the maximum degree .
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Similarly, offshore to the west, the eroded limestone outcrop forms a line of small rocky islets called (from east to west) The Bull, The Blind Cow, The Cow, and The Calf. As the coastline in this area is generally an eroding landscape, the cliffs are subject to occasional rockfalls and landslides; a particularly large slide occurred just to the east of Durdle Door in April 2013, resulting in destruction of part of the South West Coast Path.
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Almanon is a lunar impact crater that lies in the rugged highlands in the south-central region of the Moon. It was named after Abbasid Caliph and astronomer Al-Ma'mun. Image of Almanon (crater) It is located to the south-southeast of Abulfeda, and to the north-northeast of the smaller crater Geber. The crater chain designated Catena Abulfeda forms a line between the south rim of Abulfeda and the north rim of Almanon, continuing for a length of about 210 kilometers to the Rupes Altai scarp.
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The most intact section of the rim is the western quadrant, which now forms a curved ridge. There is a shorter segment of surviving rim to the northeast, which is bisected by the crater Gould P. Only small, low ridges remain to outline the original crater to the north and southeast, and the southern rim has been completely destroyed. A catena, or chain of tiny craters, forms a line running from the southern part of the crater floor towards the eastern part. The craters are probably secondaries from Bullialdus.
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For the second phase, each player chooses a "ka" from among the tokens next to the passage, or tokens one column away from the passage whichever method both players agree upon. The "ka" then enters the passage and captures any odd number of tokens of the same color that it forms a line with from any orthogonal direction. From there on (third phase), each player's "ka" moves any number of vacant spaces in an orthogonal direction provided it can capture an odd number of tokens of the same color. However, the "ka" at this phase of the game captures tokens differently.
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As early as 1822 he published a paper on the classification and distribution of fossil plants. This was followed by several papers chiefly bearing upon the relation between extinct and existing forms - a line of research which culminated in the publication of the ' ("History of fossil plants"), which has earned for him the title of "father of paleobotany." This classification arranged fossil plants with their nearest living allies; it formed the basis of much subsequent work in paleobotany. It is of especial botanical interest, because, in accordance with Robert Brown's discoveries of the fundamental difference between Gymnosperms and Angiosperms, the Cycadeae and Coniferae were placed in the new group the gymnosperms.
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Lunar Orbiter 4 image Oblique view of Almanon, the satellite crater Almanon C and its surroundings including Geber and Azophi, Apollo 16 image Almanon is a lunar impact crater that lies in the rugged highlands in the south-central region of the Moon. It was named after Abbasid Caliph and astronomer Al- Ma'mun. It is located to the south-southeast of Abulfeda, and to the north- northeast of the smaller crater Geber. The crater chain designated Catena Abulfeda forms a line between the south rim of Abulfeda and the north rim of Almanon, continuing for a length of about 210 kilometers to the Rupes Altai scarp.
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Spring tides, when the sun-earth-moon system forms a line, cause the largest tidal amplitudes during lunar monthly tidal variations. In contrast, neap tides, when the sun-earth-moon system forms a right angle, are muted, and in a semi-diurnal tidal system (such as that seen at the CBBT site) this can be seen as a lowest intertidal range. Two interesting points that arise from comparing these two sites at opposite ends of the Bay are their tidal characteristics - semi-diurnal tide for CBBT and mixed tide for Baltimore (due to resonance in the Bay) - and the differences in amplitude (due to dissipation in the Bay).
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Although it lives in a 4-dimensional space, it forms a line segment (a 1-dimensional polytope) within that space. Similarly, the associahedron K4 can be realized in this way as a regular pentagon in five-dimensional Euclidean space, whose vertex coordinates are the cyclic permutations of the vector (1, 2 + φ, 1, 1 + φ, 1 + φ) where φ denotes the golden ratio. Because the possible triangles within a regular hexagon have areas that are integer multiples of each other, this construction can be used to give integer coordinates (in six dimensions) to the three-dimensional associahedron K5; however (as the example of K4 already shows) this construction in general leads to irrational numbers as coordinates.
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The Pembrokeshire Dangler is a convergence zone which forms a line of continuous showers aligned north-south across the Irish sea; often as snow occurring during late autumn and winter, since the environmental factors required for its formation such as warm sea temperatures and cold Arctic air aloft are usually only met at this time of year. It is initiated as a northerly flow is forced between the Rhins of Galloway and the Antrim Plateau. This is then augmented by land breeze effects producing winds blowing from east of north off England and Wales and from west of north off Ireland; these winds then converging down the length of the Irish Sea. As the convergence line spawns deep convective cells, they flow over progressively warmer waters creating further instability and prime conditions for prolonged convection across Pembrokeshire, Cornwall and west Devon.
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