ライフサイエンスコーパス: kilometer

1 degrees N over an entire hemisphere (140,000 kilometers).

2 ather than at a coarse scale (around several kilometers).

3 valved below a shallow reservoir (at about 6 kilometers).

4 vity required from each muscle to traverse a kilometer.

5 plate margins resolved down to a scale of 1 kilometer.

6 ea had values over 0.09 kilometer per square kilometer.

7 rations of particles to altitudes above ~150 kilometers.

8 ent in populations separated by thousands of kilometers.

9 mes of 20 to 80 seconds and widths of </=300 kilometers.

10 s opposed to 3% of cases separated by 1 to 5 kilometers.

11 d are consistent with partial melt below 660 kilometers.

12 on of absolute plate motion for thousands of kilometers.

13 at may migrate over hundreds to thousands of kilometers.

14 nment to permit aqueous flows across several kilometers.

15 ravity anomalies with lengths of hundreds of kilometers.

16 0,000 forest plots spanning 4,000,000 square kilometers.

17 mported to the site, possibly over dozens of kilometers.

18 Ninety percent of cases lived within 50 kilometers.

19 ng with ocean currents sometimes hundreds of kilometers.

20 o 16 seconds were detected as deep as 65,000 kilometers.

21 , when the entire ring was tilted by about 2 kilometers.

22 e structural discontinuity at a depth of 220 kilometers.

23 to 20 meters and its wavelength is 30 to 80 kilometers.

24 , and often separated by tens or hundreds of kilometers.

25 n of migratory species can span thousands of kilometers.

26 craters, to thicknesses in excess of several kilometers.

27 ng slab farther east and north by up to 1000 kilometers.

28 rium elastic lithosphere is greater than 300 kilometers.

29 observed at a spatial resolution of 11 to 45 kilometers.

30 to 9% velocity drop at depths of 130 to 190 kilometers.

31 elow the seismogenic zone by at least 3 to 5 kilometers.

32 only 7% of which are larger than 100 square kilometers.

33 l dispersal and infectivity over hundreds of kilometers.

34 ls spanning length scales from nanometers to kilometers.

35 asin at ~3.3 kilometers per second over ~140 kilometers.

36 origin at Voyager 1, located at 18.5 billion kilometers (123 astronomical units) from the Sun, decrea

37 approach, indicating an upper limit of <4.6 kilometers(-3) for the dust density in the Pluto system.

38 stal magma body has a volume of 46,000 cubic kilometers, ~4.5 times that of the upper-crustal magma r

39 f Mars with a volume of 9500 to 12,500 cubic kilometers, about 30 times that previously estimated for

40 the atmosphere to form plumes rising several kilometers above eruptive vents, which can pose serious

41 ts of the radiation belts, passed about 4000 kilometers above the cloud tops at closest approach, wel

42 ervations of Jupiter, passing less than 5000 kilometers above the equatorial cloud tops.

43 t mesoscale winds at scales of a few hundred kilometers account for more than 65% of near-inertial en

44 years on objects that traveled thousands of kilometers across the Pacific Ocean to the shores of Nor

45 hollows, range from tens of meters to a few kilometers across, and many have high-reflectance interi

46 ungest of these impact structures, about 500 kilometers across, formed about 1 billion years ago, in

47 ranules and supergranules (~1000 and ~30,000 kilometers across, respectively).

48 ic fingerlike structures of wavelength ~2000 kilometers align parallel to the direction of absolute p

49 pture propagated northward for more than 170 kilometers along both mapped and unmapped faults before

50 ng the proportions of the land uses over one kilometer altered pollination probability up to 7-fold.

51 atorial stratosphere (approximately 16 to 50 kilometers altitude), was unexpectedly disrupted in Febr

52 600 km, and at spatial scales less than five kilometers among samples of YOY.

53 geochemical data to show that the 110-square-kilometer and 65-meter-deep collapse of Bardarbunga cald

54 h indicate plains thicknesses of more than 1 kilometer and multiple phases of emplacement.

55 tches, more than half of which are <1 square kilometer and only 7% of which are larger than 100 squar

56 sity, rapidly up to 1,650 persons per square kilometer and slowly thereafter.

57 a were collected on ability of walking for 1 kilometer and use of NSAIDs at baseline and death inform

58 oduces an average of 81% more transportation kilometers and 108% more emissions offsets per unit area

59 kilometers in depth and 1900 kelvin to 2200 kilometers and 2300 kelvin in the lower mantle.

60 face magma layer with a thickness of over 50 kilometers and a rock melt fraction of 20% or more is fu

61 degrees C variation extending to depths >400 kilometers and are inconsistent with variations in mantl

62 sed methane in clouds at an altitude near 30 kilometers and concomitant methane drizzle below.

63 s the resolution downward to a depth of 1500 kilometers and reveals a several-hundred-kilometer-wide

64 r-groundwater exchange on a spatial scale of kilometers and time scale of months to years suggests a

65 omography supports a much thicker root (>250 kilometers) and a gradual lithosphere-asthenosphere tran

66 o map global forest loss (2.3 million square kilometers) and gain (0.8 million square kilometers) fro

67 ntrating solar power (CSP)], area (in square kilometers), and capacity (in MW) within the global sola

68 the homopause altitude at approximately 130 kilometers, and an unexpected level of variability both

69 ing a total area of more than 245,000 square kilometers, and are probably a key stressor on marine ec

70 rary breeding sites hundreds or thousands of kilometers apart, but the behavioral adaptations that fa

71 and under cumulus clouds and then glide over kilometers at low energy costs.

72 th tectonically altered regions and 70 +/- 4 kilometers at oceanic island stations.

73 y on small spatial scales ( less, similar500 kilometers) at the footpoints of hot and dynamic coronal

74 deflating mid-crustal reservoir (at about 12 kilometers) augmented from depth.

75 dFe must have been transported thousands of kilometers away from its vent site to reach our sampling

76 azon is transported hundreds to thousands of kilometers away from the coast by surface plumes.

77 ssal Pacific, this dFe persists thousands of kilometers away from the vent source with sufficient mag

78 as to rural background values more than 100 kilometers away, varying seasonally from 4.4 to 6.1 par

79 ding 1 strain from Perth, approximately 4000 kilometers away.

80 ent wind currents to establish colonies many kilometers away.

81 open-sea locations hundreds or thousands of kilometers away.

82 ithin the subducting Pacific plate about 609 kilometers below the Sea of Okhotsk.

83 this unexplored region down to ~8 bar, ~100 kilometers below the visible clouds.

84 tectonic environment, varying from 95 +/- 4 kilometers beneath Precambrian shields and platforms to

85 recambrian shields and platforms to 81 +/- 2 kilometers beneath tectonically altered regions and 70 +

86 or and for dispersing propagules hundreds of kilometers between isolated and ephemeral communities.

87 Applying a 1-kilometer buffer to all roads, we present a global map o

88 orested region was 0.03 kilometer per square kilometer, but areas of Gabon and Equatorial Guinea had

89 pecially given that they may be carried many kilometers by currents during their planktonic phase.

90 at altitudes ranging from 150 to above 1000 kilometers by the Langmuir Probe and Wave instrument on

91 llion and a territory of >9.6 million square kilometers, China has a total of 34 provinces and munici

92 localized on a broad region of 1000 square kilometers close to the 50-kilometer Ernutet crater.

93 and fossil energy use and GHG emissions per kilometer compared to driving long distances, but the ex

94 y discontinuities in the deepest few hundred kilometers, consistent with a phase transition from pero

95 11, and for most of the 253-day, 560-million-kilometer cruise to Mars, the Radiation Assessment Detec

96 catch and require 100-200 times more square kilometer-days of closure than dynamic measures (grid-ba

97 t, Rheasilvia, is 500 kilometers wide and 19 kilometers deep and finds its nearest morphologic analog

98 through a 48-kilometers-long dike, from a 12-kilometers deep reservoir.

99 cted crystallization of magma bodies several kilometers deep within the crust.

100 Samples from a 1.76-kilometer-deep corehole drilled near the center of the l

101 harsh physicochemical conditions within the kilometer-deep hydrocarbon-bearing shale, including high

102 biodiversity fracture water collected at 2.8-kilometer depth in a South African gold mine was sequenc

103 Earth's mantle transition zone (410- to 660-kilometer depth) implies the possibility of a deep H2O r

104 mations and upper basement, between 2- and 5-kilometer depth.

105 arp, negative velocity contrast at 40- to 75-kilometer depth.

106 for enigmatic seismic features beyond ~2000 kilometers depth and suggests that the lower mantle may

107 e mantle transition zone between 410 and 660 kilometers depth, a result that is in agreement with pri

108 ect an increase in viscosity at 800- to 1200-kilometers depth, far greater than the depth of the mine

109 nd a conductive anomaly at approximately 100 kilometers depth, in conjunction with the occurrence of

110 Below 400 kilometers depth, velocity structure is organized into f

111 velocity, most prominent between 200 and 350 kilometers depth, which extends below the well-developed

112 of these undifferentiated, large (50- to 100-kilometer diameter) CAI-rich bodies suggests that they m

113 eserved by sedimentary rocks inside the 150-kilometer-diameter Gale impact crater.

114 ENGER's second Mercury flyby revealed a ~715-kilometer-diameter impact basin, the second-largest well

115 SSENGER's third Mercury flyby revealed a 290-kilometer-diameter peak-ring impact basin, among the you

116 e efficacy, increasing at a rate of 4.5% per kilometer distance.

117 ions in the same agro-ecosystem, but several kilometers distant from any oilseed rape fields.

118 eases in density over 7000 people per square kilometer do not lead to additional chains.

119 Several kilometers downhole, these organic chemicals are exposed

120 soil/runoff related signals, even at tens of kilometers downstream the city.

121 ttenuation, these compounds were transported kilometers downstream, and thus additive concentrations

122 ing that aviation impacts on PNC extend many kilometers downwind of Logan airport.

123 in western Maryland that is several (>50 km) kilometers downwind of power plants in Ohio, Pennsylvani

124 ithin a few fault lengths (approximately 300 kilometers), during times that high-amplitude surface wa

125 along the profile is characterized by a 5.2-kilometer dynamic range and 930-meter root-mean-square r

126 increase in the Moon's radius by 0.6 to 4.9 kilometers early in lunar history, consistent with predi

127 of 1000 square kilometers close to the 50-kilometer Ernutet crater.

128 , with equivalent spherical diameters of ~40 kilometers for Nix and Hydra and ~10 kilometers for Styx

129 of ~40 kilometers for Nix and Hydra and ~10 kilometers for Styx and Kerberos.

130 ess, which significantly increased with each kilometer from DES [carbon, 0.2 Mgxha(-1); 0.1 species p

131 ostris male that originated on Espanola >100 kilometers from Daphne Major.

132 al populations were depleted within 7 and 40 kilometers from hunters' access points (roads and settle

133 smometers at distances between 1000 and 2000 kilometers from the source of the 2011, moment magnitude

134 th and aviation also at several thousands of kilometers from the volcanic source.

135 table in radar interferometric data up to >8 kilometers from the wells.

136 g habitats that are hundreds or thousands of kilometers from their natal sites.

137 are kilometers) and gain (0.8 million square kilometers) from 2000 to 2012 at a spatial resolution of

138 yield are dominated by broad-scale (100s of kilometers) GCM systematic errors that RCMs cannot compe

139 ination, highly reflective zone in Oxo, a 10-kilometer, geologically fresh crater, on five occasions

140 A 350-kilometer-high volcanic plume was seen to emanate from t

141 field at the submesoscales (100 m to tens of kilometers, hours to days) remain unresolved due to a la

142 ii of 291 (+/-9), 278 (+/-9), and 250 (+/-9) kilometers, implying a density of 2400 (+/-250) kilogram

143 dissolved methane plume that is hundreds of kilometer in length.

144 ge bright-point group that is 430,000 square kilometers in area and located near the solar disk cente

145 -temperature range extending from about 1000 kilometers in depth and 1900 kelvin to 2200 kilometers a

146 oduced a catalog of all impact craters >/=20 kilometers in diameter on the lunar surface and analyzed

147 Chondritic impacts as small as 2 kilometers in diameter should produce observable excursi

148 late terrestrial impactors, at 2500 to 3000 kilometers in diameter, potentially modified Earth's obl

149 ted impact produced a transient crater, ~390 kilometers in diameter, that was not maintained because

150 e presence of an impact feature, 240 (+/-25) kilometers in diameter, within Pallas's ultraviolet-dark

151 e of a continuous plume of oil, more than 35 kilometers in length, at approximately 1100 meters depth

152 e, and variability at altitudes down to ~130 kilometers in the subsolar region.

153 l the earthquake rupture as a slip pulse ~20 kilometers in width, ~6 seconds in duration, and with a

154 istances (hundreds of meters to thousands of kilometers) in the atmosphere.

155 e changes (spanning more than 500,000 square kilometers) in the wake of this storm.

156 mation at high altitudes (approximately 1000 kilometers) in Titan's atmosphere.

157 core having an average radius of 107 to 113 kilometers, indicating sufficient internal melting to se

158 y glaciers reaching hundreds to thousands of kilometers inland over the entire continent.

159 and marine environments can begin up to 100 kilometers inland, extend to the continental shelf, and

160 produced effects that penetrated hundreds of kilometers into Saturn's stratosphere (to the 1-millibar

161 , low-frequency sound signals that penetrate kilometers into the Earth's crust.

162 try did not change appreciably until several kilometers into the urban environment, where concentrati

163 ne 2011) from the upper troposphere (9 to 14 kilometers) into the lower stratosphere.

164 er atmosphere (at altitudes of less than 200 kilometers) is consistent with ground-based stellar occu

165 Emission extended down to ~60 kilometer (km) altitude (1 microbar), deeper than confir

166 gravitational field of Orientale at 3- to 5-kilometer (km) horizontal resolution.

167 ical phase changes approximately 410 and 660 kilometers (km) deep within Earth beneath South America

168 nd mean equatorial radii of 2574.32 +/- 0.05 kilometers (km), 2574.36 +/- 0.03 km, and 2574.91 +/- 0.

169 h long-distance (on the order of hundreds of kilometers) larval dispersal distances, making it very d

170 Across an 11,660-kilometer latitudinal gradient spanning six continents,

171 ) to 2 x 10(4) kilometers wide and 1 x 10(5) kilometers long and last from 100 to 2500 seconds.

172 ribution, rupture along the approximately 60-kilometer-long Carrizo segment was thought to control th

173 3, a magnitude 8.3 earthquake ruptured a 180-kilometer-long fault within the subducting Pacific plate

174 volved the formation of a approximately 1000-kilometer-long lobate scarp, a product of the global coo

175 Mayor-Cucapah earthquake that produced a 120-kilometer-long multifault rupture through northernmost B

176 ntawai islands, Sumatra, imply that this 700-kilometer-long section of the Sunda megathrust has gener

177 earthquake of 1857, with a approximately 350-kilometer-long surface rupture, was the most recent majo

178 Using an 800-kilometer-long, densely spaced seismic array, we have co

179 of magma, and lateral migration through a 48-kilometers-long dike, from a 12-kilometers deep reservoi

180 A 3200-kilometers-long profile of Mercury by the Mercury Laser

181 y vagile and can disperse up to thousands of kilometers, making it difficult to identify the factors

182 , whereas those for the Moon, at ~250 to 300 kilometers, may have delivered water to its mantle.

183 s and the best-available data from our 7,000-kilometer mega-transect survey and open access data, we

184 016, delays rose from 2.1 to 3.1 minutes per kilometer (min/km) in the morning peak and from 2.8 to 5

185 centers up to 499 miles (to convert miles to kilometers, multiply by 1.6) away, 6.7% at centers 500 t

186 d rapid range expansion by the butterfly (79 kilometers northward in Britain in 20 years).

187 c equator and reveal an offset of 484 +/- 11 kilometers northward of the geographic equator.

188 of SO2 and 1 teragram of HCl for every cubic kilometer of lava erupted.

189 ielding up to 5.4 teragrams of SO2 per cubic kilometer of lava.

190 Over 1.1 kilometers of a specially designed optical fiber that mi

191 leogene boundary and that >1.1 million cubic kilometers of basalt erupted in ~750,000 years.

192 Processes within the lowest several hundred kilometers of Earth's rocky mantle play a critical role

193 -density plasmasphere (roughly within 20,000 kilometers of Earth) that is known to remove the high-en

194 lateral viscosity variations in the top 200 kilometers of Earth, together with forces associated wit

195 bservational data showing that ~87,000 cubic kilometers of ice have accumulated at the poles since th

196 s are embedded into a preform and drawn into kilometers of microstructured multimaterial fibre device

197 period from 1976 to 2003, we measured 51,916 kilometers of new logging roads.

198 to form blooms that cover hundreds of square kilometers of ocean.

199 dea exulans) forage over thousands of square kilometers of open ocean for patchily distributed live p

200 ct across 103 salt marsh sites spanning ~430 kilometers of shoreline in coastal Louisiana, Alabama, a

201 an family distributed within several hundred kilometers of the expanding and retracting glaciers of t

202 In the deepest tens of kilometers of the mantle, isolated pockets of ultralow s

203 SSEs occurring close to the trench (within 2 kilometers of the seafloor), where very low temperatures

204 hytoplankton populations across thousands of kilometers of the surface ocean.

205 ns Ice Stream is observed to drain 2.0 cubic kilometers of water into the ocean over approximately 3

206 .81 pM for B(1)) in extensive areas (100s of kilometers) of the coastal ocean, and thus may exert imp

207 rated to within 0.146 solar radius (~100,000 kilometers) of the solar surface before its EUV signal d

208 rapid (1 to 4 million years) changes of 1.5 kilometers or more.

209 e atmosphere (at altitudes of less than 1800 kilometers or so), whereas methane (CH4), acetylene (C2H

210 imately 10 R(E) (R(E): Earth radius, or 6374 kilometers), or by the process of magnetic reconnection

211 ry lobes, which extended tens to hundreds of kilometers over gently sloping plains and boundary crate

212 emerged with an average speed of 0.3 to 0.6 kilometer per second and caused high peaks in the photos

213 of roads across the forested region was 0.03 kilometer per square kilometer, but areas of Gabon and E

214 n and Equatorial Guinea had values over 0.09 kilometer per square kilometer.

215 ncident AMD versus average running distance (kilometers per day), cardiorespiratory fitness (10-km fo

216 to higher latitudes at a median rate of 16.9 kilometers per decade.

217 ve greater field-to-wheels efficiency (e.g., kilometers per gigajoule biomass or per hectare) compare

218 iHVCs with 90 </= |v(LSR)| less, similar 170 kilometers per second (where v(LSR) is the velocity in t

219 eas iHVCs with |v(LSR)| greater, similar 170 kilometers per second are at larger distances.

220 The surface rotation rate, approximately 2 kilometers per second at the equator, predicts an oblate

221 s survived a record high-speed entry of 28.6 kilometers per second from an orbit close to that of Jup

222 nt small-scale jets with speeds of 80 to 250 kilometers per second from the narrow bright network lan

223 These oscillations, 2.6 kilometers per second in amplitude, are coupled with chr

224 h plasma is propelled at speeds of 50 to 150 kilometers per second into the corona.

225 ropagated toward the Kathmandu basin at ~3.3 kilometers per second over ~140 kilometers.

226 ional waves, which can give kicks up to 4000 kilometers per second to the merged black hole.

227 ne near the Alfven speed ( approximately 800 kilometers per second) and another near the sound speed

228 S-wave velocity of approximately 2.0 to 2.7 kilometers per second).

229 econd) and another near the sound speed (200 kilometers per second).

230 d redshifted with a Doppler velocity of ~700 kilometers per second, direct evidence of large-scale as

231 in-belt asteroids at velocities exceeding 10 kilometers per second, enough to heat and degas target r

232 Traveling with a velocity of ~1200 kilometers per second, it is the fastest unbound star in

233 dipping fault plane at an average speed of 8 kilometers per second, suggesting efficient seismic ener

234 e than do typical main belt collisions at ~5 kilometers per second.

235 rs, assuming a typical grain velocity of ~18 kilometers per second.

236 d by transverse waves with amplitudes of ~20 kilometers per second.

237 velocities with an average blue shift of 23 kilometers per second.

238 cceleration of the solar wind to hundreds of kilometers per second.

239 hout the Peruvian Amazon averaged 632 square kilometers per year and 645 square kilometers per year,

240 ated from negligible loss at 25 +/- 64 cubic kilometers per year for 1994-2003 to rapid loss of 310 +

241 1994-2003 to rapid loss of 310 +/- 74 cubic kilometers per year for 2003-2012.

242 e and required range shifts of up to several kilometers per year, raising the prospect of daunting ch

243 32 square kilometers per year and 645 square kilometers per year, respectively.

244 , with forest loss increasing by 2101 square kilometers per year.

245 d as dikes into the shallow mantle of a ~200-kilometer-radius protoplanet.

246 ming, extreme marine heat waves forced a 100-kilometer range contraction of extensive kelp forests an

247 Orbiting Carbon Observatory-2 (OCO-2) at the kilometer scale reveal distinct structures of atmospheri

248 e is not exposed at the lunar surface at the kilometer scale.

249 f highly evolved, silica-rich lunar soils in kilometer-scale and larger exposures, expanded the compo

250 erential elevation changes show distributed, kilometer-scale bending strains as large as ~10(3) micro

251 e-shot remote identification of chemicals at kilometer-scale distances is experimentally demonstrated

252 al analysis of protected areas, we show that kilometer-scale edge effects may compromise the ability

253 surface water descend as coherent, 1- to 10-kilometer-scale filamentous features, often along the pe

254 nce remote comparison of optical clocks over kilometer-scale urban distances, a key step for developm

255 mical change and topographic behavior at sub-kilometer scales is not self-similar.

256 A rupture velocity of ~4.0 to 4.5 kilometers/second is determined by back-projection of sh

257 At diameters less than or equal to 8 to 10 kilometers, secondary impact craters on Mercury are more

258 buted across approximately 50 million square kilometers, similar to well-known impact strewnfields an

259 Here, we argue that numerous kilometer-sized ejecta fragments from that event struck

260 bilities transfer energy to nonaxisymmetric, kilometer-sized magnetic features, in which the local fi

261 individuals migrate hundreds to thousands of kilometers south in midsummer to breed a second time dur

262 Thirty kilometers south of the island of Hawai'i lies the Lo'ih

263 minid-bearing unit, now exposed across a > 9-kilometer structural arc, is sandwiched between two volc

264 e smoother terrains (over hundreds of square kilometers) suggests that potential ground-ice presence

265 planetesimals, which are all larger than 35 kilometers, supporting the view of asteroids being born

266 n of ethanol increased 10-fold in metric ton-kilometers (t-km) from 2000 to 2009, the portion of t-km

267 atmospheric winds on scales of thousands of kilometers, the most energetic of such fluctuations, are

268 gest a chemical continental lithosphere 175 kilometers thick, whereas seismic tomography supports a

269 s that ascend to form basaltic crust 6 to 7 kilometers thick.

270 kite lens about 2300 kilometers wide and 250 kilometers thick.

271 igh less than a gram and travel thousands of kilometers to a site they have never seen.

272 that penguins traversed thousands of square kilometers to areas of low sea surface temperatures (14.

273 te Vallis, and it extended an additional 180 kilometers to the east before the emplacement of the you

274 tions with depth mimic those approximately 6 kilometers to the north and demonstrate that water-induc

275 More patients traveled long distances (>100 kilometers) to receive specialty services than to receiv

276 d, we conducted aerial surveys along a three-kilometer track line at Ostional, Costa Rica during a ma

277 water column density structure along an 8000-kilometer transect in the South Pacific Ocean.

278 ive transport would be 79 g CO2e per vehicle-kilometer traveled, a 71% reduction relative to 2013.

279 ycle fossil energy use (~ 100 MJ/100 vehicle kilometers traveled (VKT)) and net GHG emissions (~5 kg

280 ter if it occurs "many hundreds of meters to kilometers underground".

281 strong lower crust thrusting several tens of kilometers underneath Qilian.

282 These events migrated northward for ~50 kilometers until the 1 April earthquake occurred.

283 ter-wavelength ripples and hundred-meter- to kilometer-wavelength dunes: bedforms of two distinct siz

284 MESSENGER) spacecraft at altitudes below 150 kilometers, we have detected remanent magnetization in M

285 older community-dwelling adults who lived 80 kilometers west of the epicenter (59.0% response rate).

286 older community-dwelling adults who lived 80 kilometers west of the epicenter 7 months before the ear

287 es and glacier-front changes along the ~1000-kilometer western coastline.

288 volume is estimated to be 1.6 x 10(6) cubic kilometers, which is equivalent to a global water layer

289 millions of insects travelling thousands of kilometers while devastating vegetation and crops.

290 x-ray jets are about 2 x 10(3) to 2 x 10(4) kilometers wide and 1 x 10(5) kilometers long and last f

291 The youngest, Rheasilvia, is 500 kilometers wide and 19 kilometers deep and finds its nea

292 the base of a postperovskite lens about 2300 kilometers wide and 250 kilometers thick.

293 Observations at a 1-kilometer-wide front within the Kuroshio Current indicat

294 Rheasilvia obliterated half of another 400-kilometer-wide impact basin, Veneneia.

295 500 kilometers and reveals a several-hundred-kilometer-wide region of low velocities beneath and sout

296 The presence of an 800- to 2000-kilometer-wide thermal anomaly (DeltaT(max) ~300 to 400

297 birds can navigate over tens of thousands of kilometers with an accuracy unobtainable for human navig

298 ge and tracks earthquakes to distances of 35 kilometers, with a triggering threshold of ~0.07 megapas

299 elocity layer (USL) varies spatially (3 to 5 kilometers, with an S-wave velocity of approximately 2.0

300 was 0-30,860 vehicles/day x length of road (kilometers) within 100 m; 281 (13%) women lived </= 200