ライフサイエンスコーパス: ridge

1 tion, and region (North versus South Hydrate Ridge).

2 nique residues align along the outer helical ridge.

3 c center encircled by a prominent peripheral ridge.

4 CAH, androgens inhibit descent of the sinus ridge.

5 r and mostly involves the maxillary alveolar ridge.

6 els and observed at the Australian-Antarctic Ridge.

7 hydrothermal vent fields on the East Scotia Ridge.

8 duration of the overlying apical ectodermal ridge.

9 is Massif oceanic core complex, Mid-Atlantic Ridge.

10 ing line retreated from a prominent seafloor ridge.

11 hosted melt inclusions from the Mid-Atlantic Ridge.

12 lease of mantle heat and carbon at mid-ocean ridges.

13 nd is the dominant process at slow-spreading ridges.

14 sing of CO2 at subduction zones and midocean ridges.

15 lower oceanic crust formed at fast-spreading ridges.

16 ridge defects were created to form atrophic ridges.

17 ut only a moderate effect on petal cone cell ridges.

18 and hydrothermal venting at the Mid-Atlantic Ridge (2-6 per cent).

19 natural mummy that lived south of the Alpine ridge ~5,200 years before present (ybp), during the Copp

20 ion and distribution patterns within Hydrate Ridge, a methane seep ecosystem off the coast of Oregon

21 , even at magmatically robust fast-spreading ridges, a substantial portion of the spreading may be du

22 Nine thousand years ago, the Alpena-Amberley Ridge (AAR) beneath modern Lake Huron was a dry land cor

23 how that for intermediate- to fast-spreading ridges, abyssal hill spacing is consistent with the peri

24 Those ridges act as a diffraction grating, producing an irides

25 (Fgf8) is produced by the apical ectodermal ridge (AER) at the distal tip of the limb bud to direct

26 s linked to defects of the apical ectodermal ridge (AER) of the developing limb buds.

27 ing activity (ZPA) and the apical ectodermal ridge (AER), are known to cause limb malformations and e

28 ior fin development via an apical ectodermal ridge (AER), whereas an alternative Homeobox (Hox)-Fibro

29 is crucial for the maintenance of cuticular ridges after they are formed.

30 tory atop Axial Seamount on the Juan de Fuca ridge allows unprecedented real-time monitoring of a sub

31 gical swirling flow, while the height of the ridge also significantly contributed to the enhanced per

32 xual differentiation of the urogenital sinus ridge, an epithelial thickening that forms where the sex

33 t Emx1, gives rise to the dorsal ventricular ridge and appears comparable to the avian nidopallium.

34 oth at the advancing edge and at the initial ridge and extraretinal fibrovascular proliferative compl

35 ells and cells within the greater epithelial ridge and is independent of cell proliferation.

36 acy over other widely used GC modeling (PGC, Ridge and Lasso) and MI-based (MRNET and ARACNE) methods

37 he older parts of this hotspot track (Walvis Ridge and Rio Grande Rise) and re-evaluate published dat

38 orizons) and permafrost samples from center, ridge and trough positions of water-saturated low-center

39 pography of the Falkland Plateau, Rio Grande Ridge and Walvis Rise, favoured deposition of thick evap

40 iscovery of ancient rocks in the mid-oceanic ridges and abyssal ocean basins.

41 to creases, wrinkles, folds, period-doubles, ridges and delaminated-buckles according to their distin

42 We find that the cutting of ridges and filling of valleys has lowered the median slo

43 ression melting similar to that at mid-ocean ridges and flux melting resembling that beneath arcs.

44 Ridges and grooves of the template are 10 microm width a

45 ning (MTM) is a form of surface mining where ridges and mountain tops are removed with explosives to

46 surge in magma and CO2 fluxes from mid-ocean ridges and oceanic hotspot volcanoes.

47 hthyans, with large plates bearing vermiform ridges and partially enclosed sensory canals.

48 deleterious intermediate mutations, fitness ridges and valleys arise in the pathogen's fitness lands

49 TPX2 uses two flexibly linked elements ('ridge' and 'wedge') in a novel interaction mode to simul

50 elapsed between the formation (at mid-ocean ridges) and destruction (at subduction zones) of ocean b

51 of teeth adjacent to the edentulous atrophic ridge, and age were shown to influence maxillary sinus L

52 ution produces a negative feature, bends the ridge, and broadens the edge.

53 er species are known from the Central Indian Ridge, and morphological and molecular analyses show tha

54 posterior extension of the apical ectodermal ridge, and this also allows the additional digit to aris

55 etic features (including concretions, raised ridges, and fractures) at high spatial resolution indica

56 attice of diamonds connected by steep, sharp ridges, and we experimentally demonstrate the evolution

57 bone allografts (FDBAs) are used in alveolar ridge (AR) preservation; however, each material has adva

58 ctions and lateral input from the urogenital ridges are required to drive HSC development in the aort

59 ng rates, we reemphasize that fast-spreading ridges are the best potential recorders of a sea level s

60 s the appearance of the respiratory eggshell ridges, are caused by changes in the spatial distributio

61 etric spectra from an intermediate-spreading ridge as evidence for a primary contribution of sea leve

62 Likewise, buccal-lingual width of alveolar ridge as well as thickness of buccal wall was compared w

63 l disorder among the identical, multilayered ridges as the critical factor for producing angular inde

64 inferred to have caused breaching of a rock ridge at the Dover Strait, although this hypothesis rema

65 he Lau Basin, with an abundance of spreading ridges at different distances from the subduction zone,

66 Surprisingly, cuticular ridges at first form normally in the cus2 mutant, but ar

67 silla with the stage of development; (c) the ridges at the tips of the mandiblar stylets become more

68 through a microchannel designed with angled ridges at the top of the channel and coated with adhesiv

69 ozen bone allografts (FFBAs) during alveolar ridge augmentation and to assess 1-year survival of dent

70 upturing along at least 35 kilometres of the ridge axis, where tectonic stress had built up to a crit

71 thermal vents is lost from solution close to ridge-axis sources and is thus of limited importance for

72 om Mauna Kea are more oxidized than midocean ridge basalt (MORB) magmas, suggesting that the upper ma

73 per thousand), than the canonical mid-ocean ridge basalt value of -6.0 per thousand.

74 Chemical differences between mid-ocean ridge basalts (MORBs) and ocean island basalts (OIBs) pr

75 We also find that mid-ocean-ridge basalts (MORBs) have (238)U/(235)U ratios higher t

76 dge depths, and the composition of mid-ocean ridge basalts can all be used to determine variations in

77 r (3)He/(4)He ratios identified in mid-ocean-ridge basalts that form by melting the upper mantle (abo

78 eneath the upper mantle sampled by mid-ocean-ridge basalts, and that buoyantly upwelling plumes from

79 do not produce appreciable changes in ocean ridge bathymetry on time scales less than 100,000 years

80 introducing a deep-subwavelength dielectric ridge between a dielectric slab and a metallic substrate

81 575) is N(7)-methylated by Bud23-Trm112 at a ridge between the P- and E-site tRNAs.

82 ound the body-axis, and stimulation near the ridge between ventral and dorsal striatum caused freezin

83 n the cathode was placed on the supraorbital ridge (bipolar-unbalanced montage).

84 s (Bathymodiolus spp.) from the Mid-Atlantic Ridge by using high-resolution ocean modeling and popula

85 chanism of recognition of the ZEDIII lateral ridge by VH3-23/VK1-5 antibodies.

86 nanowires imprinted with helical grooves or ridges can be used efficiently to generate plasmonic vor

87 he persistence of an exceptional atmospheric ridge, centred over the Arctic Ocean, was responsible fo

88 tudy is to radiographically compare alveolar ridge changes with and without RP with cone-beam compute

89 ntial expression of PSGL-1 ligand by using a ridged channel coated with P selectin.

90 Here we show that a film-terminated ridge-channel structure can strongly enhance sliding fri

91 At ocean spreading ridges, circulation of seawater through rock at elevated

92 rs, we re-sampled P. flexilis twigs at Niwot Ridge, CO and characterized needle endophyte communities

93 inders with northern hemisphere air at Niwot Ridge, Colorado.

94 lly assumed that elongated creases form when ridges connecting two d-cones fold beyond the material y

95 ingival recession, papilla loss, collapse of ridge contour, and other esthetic complications.

96 A ridge cortical thickness >0.75 mm and a normal appearanc

97 Microfluidic ridges could be fabricated with dimensions as small as 2

98 sferase6 (gpat6), and defective in cuticular ridges (dcr) were grouped in three separate classes base

99 Experimental ridge defects were created to form atrophic ridges.

100 Seismic wave velocities, ocean ridge depths, and the composition of mid-ocean ridge bas

101 In females, the sinus ridge descends posteriorly to allow the vaginal opening

102 signals to reconstruct 2D maps of fingermark ridge details.

103 -ice loss and the North Pacific geopotential ridge development.

104 Facial gingival thickness and gingival ridge dimension could be increased after IMITG.

105 l level, facial gingival thickness, gingival ridge dimension, and width of keratinized gingiva were t

106 f residual graft, percentage of CT/other, or ridge dimensional changes.

107 raphic examinations were performed to assess ridge dimensional changes.

108 The same ridge dimensions were measured at time of implant placem

109 Vertical ridge dimensions were measured from a tooth-supported st

110 evation of a full-thickness flap, horizontal ridge dimensions were measured with a digital caliper at

111 the lost buccal plate, maintain theoretical ridge dimensions, and allow for implant placement 5 mont

112 robe sonifier was placed on the supraorbital ridge directly above the entrance of the optic nerve int

113 Here, we analyzed the dorsal ridge (DR), a lumen-like structure along the dorsal side

114 far from the magmatic influence of mid-ocean ridges, driving large flows of water, heat and solutes t

115 The dorsal ventricular ridge (DVR) is one of the main components of the saurops

116 nto a distinct SVZ in the dorsal ventricular ridge (DVR) of turtle forebrain and in the cortices of c

117 ng function, theoretical models of mid-ocean ridge dynamics that include melt transport predict tempo

118 orced interactions between the cells and the ridges ensure that a high flow rate can be used without

119 ns (in order of increasing elevation): Ebony Ridge (ER), Cloudmaker (CM), and Meyer Desert (MD).

120 glass, the actual contact made by finger pad ridges evolved over time following a first-order kinetic

121 Hydrothermal venting along mid-ocean ridges exerts an important control on the chemical compo

122 a temporal window of development when sinus ridge fate is determined.

123 e we create three-dimensional simulations of ridge-flank hydrothermal circulation, flowing between an

124 nd solutes through volcanic rock outcrops on ridge flanks.

125 Ridge formation also coincides with the reduction in gro

126 Our results reveal the dynamics of both ridge formation and maintenance as the sepal grows.

127 n of cellular growth, we find that cuticular ridge formation progresses down the sepal from tip to ba

128 reporter expression coincides with cuticular ridge formation, descending the sepal from tip to base.

129 evelopment coincides with that of carapacial ridge formation, suggesting that the development of dors

130 and noninvasive means of promoting alveolar ridge formation.

131 We interpret each obstacle as an esker ridge formed from sediments deposited by subglacial wate

132 tact line depins and slides down the wetting ridge, forming a new one after a transient.

133 ion of marine water beyond the crest of this ridge, forming an ocean cavity beneath the ice shelf, oc

134 The study was conducted at the Jasper Ridge Global Change Experiment (JRGCE), California where

135 asalts from, for example, Pitcairn or Walvis Ridge has been variously attributed to recycled pelagic

136 stence of ancient rocks in present mid-ocean ridges have long been observed but received less attenti

137 ct fill, and significantly more bone gain in ridge height (P <0.05) than controls.

138 jective is to compare dimensional changes in ridge height and width after grafting with these two mat

139 test) at days 0, 7, 14, and 28 for alveolar ridge height and width and for markers of inflammation a

140 Clinical measurements were made to evaluate ridge height and width.

141 e- and postoperatively to evaluate change in ridge height and width.

142 between groups was a greater loss of lingual ridge height in the cancellous group.

143 without RP, significantly more reduction in ridge height occurred, and the majority of ridge width l

144 l bone augmentation in sites with a residual ridge height of 5 to 8 mm.

145 Significantly greater loss in alveolar ridge height was found in molar sites allowed to heal wi

146 ridge width and change in buccal and lingual ridge height.

147 ek 1 inflammation positively correlated with ridge height; thereafter, a more intense inflammatory re

148 active submarine volcano on the Juan de Fuca Ridge in the NE Pacific Ocean, from 2013 to 2015 at thre

149 incide with positions of protruding membrane ridges in proximity to the callose wall.

150 n these deep-rooted upwellings and mid-ocean ridges in pulses separated by approximately 10-20 Ma, to

151 Eastern Lau Spreading Centre and the Valu Fa Ridge, in contrast to the inferred increase in magmatic

152 ion systems have been discovered at midocean ridges, in forearc settings of subduction zones, and at

153 trabeculae, compared to lower values on the ridges, in the wild type suggest oscillatory forces as a

154 places TS8 well below TS6, making the valley-ridge inflection point (VRI or bifurcation) and direct f

155 ng reaction path bifurcations through valley-ridge inflections.

156 We find that while the ridge is necessary but not sufficient for the formation

157 data that indicate that the subducting Nazca Ridge is necessary for the development and continued sup

158 The Southwest Indian Ridge is the longest section of very slow to ultraslow-s

159 f the oceanic crust formed at fast-spreading ridges is composed of plutonic rocks whose mineral assem

160 ell differentiation in the embryonic gonadal ridge, is initiated by SRY, a Y-encoded architectural tr

161 t of the Eurasian plate following a westward ridge jump in the direction of the Iceland plume.

162 Hypolimnas butterflies is caused by complex ridge-lamellar architectures in the upper lamina of the

163 averaged interfacial structure consists of a ridged lateral arrangement of adsorbed water molecules h

164 pact layer that concentrically encircles the ridge-like inner trabecular layer.

165 id (23,000 to 100,000 years) fluctuations in ridge magma supply caused by sealevel changes that modul

166 ed, however, precluding a clear link between ridge magmatism and Pleistocene climate transitions.

167 Mid-ocean ridge magmatism is driven by seafloor spreading and deco

168 ated by variations in volcanism at mid-ocean ridges modulated by Milankovitch cycle-driven changes in

169 ents S/(3)He ratios of vesicles in mid-ocean ridge (MOR) basalt glass together with the ratios of hig

170 de mineral precipitation occurs at mid-ocean ridge (MOR) spreading centers, both in the form of plume

171 c basalt in hydrothermal systems at midocean ridges (MOR).

172 ion of mesenchymal cells that regulate sinus ridge morphogenesis.

173 M power PC Blue BioU at Rice and Rhea at Oak Ridge National Laboratory (ORNL) for the computation.

174 ns from the Spallation Neutron Source at Oak Ridge National Laboratory.

175 utron Scattering (GP-SANS) instrument at Oak Ridge National Laboratory.

176 mpositional boundary established at midocean ridges, not a rheological boundary.

177 final ungrounding of the ice shelf from the ridge occurred in 1970 (+/-4 years).

178 f reef fishes that are endemic to a volcanic ridge of seamounts and islands to understand their relat

179 h assemble into rows along the highly curved ridges of lamellar cristae.

180 were observed on the deep Ka'ena and Necker Ridges of the Hawaiian Archipelago, and in a nodule-abun

181 outhwest) orientation and the spacing of the ridges of this bladed terrain.

182 s molecule is amphiphilic with a hydrophobic ridge on the surface enriched in aromatic residues and s

183 which causes a great reduction in cuticular ridges on the mature sepal epidermis, but only a moderat

184 d cell surface topography (which forms micro-ridges on the neutrophil surface) provides the resource

185 hrough cartilages, cartilaginous cristae and ridges on the plantar side of the distal tibiotarsus and

186 On impinging on the lithosphere at spreading ridges or in intra-plate settings, mantle plumes may gen

187 allow (<10 m) lenses of water perched behind ridges orientated transverse to ice flow.

188 teral, both buccal-lingually in the alveolar ridge (P = 0.007) and in buccal wall thickness (P = 0.00

189 nts is based on the fundamental premise that ridge patterns from distinct fingers are different (uniq

190 posterior division of the dorsal ventricular ridge (PDVRVM ).

191 ds at 500 hPa and of the maximum latitude of ridge peaks of the 5,700+/-50 m isohypse over the Arctic

192 The ridged portion on the upper surface of the petal is enri

193 to seleniferous soils, the S. ericoides Pine Ridge (PR) population was compared with the nearby Cloud

194 rd tissue dimensional changes after alveolar ridge preservation (ARP) using two membranes consisting

195 vidence is available specifically evaluating ridge preservation (RP) and implant placement in molar s

196 Several materials have been used for ridge preservation after tooth extraction.

197 fts (FDBA) are available for use in alveolar ridge preservation after tooth extraction.

198 n is well documented, but models to evaluate ridge preservation are neither standardized nor cost-eff

199 ence to date is limited concerning timing of ridge preservation healing and reentry for implant place

200 ogic changes following tooth extraction with ridge preservation in humans using cortical versus cance

201 ly and histologically evaluate healing after ridge preservation in non-molar sites using 50%/50% cort

202 FDBA, and 100% cancellous FDBA when used in ridge preservation of non-molar tooth sites.

203 eeks after extraction of non-molar teeth and ridge preservation using demineralized freeze-dried bone

204 Forty-four patients had tooth extraction and ridge preservation with DFDBA that was obtained from a s

205 formation occurs after tooth extraction and ridge preservation with DFDBA when sites healed for 18 t

206 ts randomized into two equal groups received ridge preservation with either 100% mineralized FDBA (ac

207 and randomized into three groups to receive ridge preservation with the following: 1) 100% cortical

208 h a 100% cortical or 100% cancellous FDBA in ridge preservation.

209 ri-implant tissue regeneration, and alveolar ridge reconstruction.

210 c fabric of the seafloor formed at mid-ocean ridges records rapid (23,000 to 100,000 years) fluctuati

211 als on both the white/smooth and anthocyanic/ridged regions, and on the lower (abaxial) surface, whic

212 BLUP, Bayes A (BA), Cpi (BC), Lasso (BL) and Ridge Regression (BRR).

213 Furthermore, the ridge regression (rrBLUP) and BayesCpi (BCpi) models bot

214 unders via regularized regression, including ridge regression and lasso regression.

215 RR-BLUP, Bayesian A, B, Cpi, LASSO, Ridge Regression and two machine learning methods (SVM a

216 fications), fitted using Bayesian, Lasso and Ridge regression approaches; and (ii) to decompose genom

217 A ridge regression best linear unbiased prediction strateg

218 ed equal, and better PA than the generalized ridge regression heteroscedastic effect model for the tr

219 Our optimal predictive Bayesian LASSO and ridge regression models were similar and on average 37%

220 lized Regression (DiPR), which uses standard ridge regression software to combine sets of covariates

221 Ridge regression was used to identify MPWL-associated no

222 by employing regularized linear regression (ridge regression), using temporal changes in the distrib

223 ral widely used prediction models, including Ridge Regression, LASSO and Elastic Nets estimated from

224 entations of atomic neighborhoods and Kernel Ridge Regression, we show that an accurate and transfera

225 shrinkage and selection operator (LASSO) and ridge regression.

226 hods for discrimination, including lasso and ridge regression.

227 od, viz., CGC-2SPR (CGC using two-step prior Ridge regularization) to resolve the problem by incorpor

228 ustralian Bight and groundwater from the Oak Ridge Reservation in Oak Ridge, TN.

229 e in maintaining soft tissues and minimizing ridge resorption in all dimensions after ARP.

230 el prosthetic graft, which utilises internal ridge(s) to induce spiral flow.

231 er plutonic crust formed at a fast-spreading ridge, sampled by the Integrated Ocean Drilling Program

232 -5600 nM) and tungsten (0.3-8 nM) in Hydrate Ridge sediment porewaters.

233 opulations occupying the plains and mountain ridges separating Europe from Asia has been eventful, as

234 We found a ridge-shaped response surface in which NPP is humped (un

235 ects steered wind direction for certain dune ridge shapes.

236 New bathymetry from the Australian-Antarctic ridge shows statistically significant spectral energy ne

237 The ridges slightly compress passing cells such that adhesiv

238 center and trough than the relatively drier ridge soils.

239 ed before sex determination and most genital ridge somatic cells differentiated into steroidogenic ce

240 urrent convergence zone and the Mid-Atlantic Ridge southwest of the Azores.

241 revealed protective activity of DIII-lateral ridge specific neutralizing mAbs in a mouse model of ZIK

242 signals from the trunk and apical ectodermal ridge specify the stylopod and zeugopod/autopod, respect

243 s continental rifts evolve towards mid-ocean ridges, strain is accommodated by repeated episodes of f

244 ies are covered with intricate, hierarchical ridge structures that produce a bright, blue reflection

245 ng the Peruvian plate boundary, suction, and ridge subduction.

246 egions separated primarily by major mountain ridges, suggesting that mountains played a role in the g

247 eaflet phospholipids to bind to a pronounced ridge surrounding the channel, followed by diffusion tow

248 that were dredged from the Southwest Indian Ridge (SWIR) in the Gallieni fracture zone.

249 because 98 per cent of the global mid-ocean-ridge system is below the ocean surface.

250 w-spreading seafloor in the global mid-ocean ridge system, but the biogeography and ecology of its hy

251 from California by a persistent atmospheric ridging system in the North Pacific.

252 The device uses a channel with repeated ridges that are diagonal with respect to the direction o

253 epidopteran wing scales are the longitudinal ridges that run the length of the mature (dead) cell, ga

254 ong the ridge, while to the northwest of the ridge, the slab is sagging, tearing, and re-initiating n

255 and detectable, the CO2 fluxes at mid-ocean ridges, the depth of the lithosphere-asthenosphere bound

256 drop on a soft substrate moves by surfing a ridge: the initially flat solid surface is deformed into

257 Mean residual ridge thickness was 2.78 +/- 1.37 mm in the perforation

258 ntaminated soil situated downstream from Oak Ridge, TN, in the United States.

259 dwater from the Oak Ridge Reservation in Oak Ridge, TN.

260 (6.5-26.2; q1-q3), ranging from 5.1g at the ridge to 29.8g at the roof.

261 ain geochemical differences with the Valu Fa Ridge to the south, which has no distinct deep low-seism

262 marine environments extending from mid-ocean ridges to subduction zones.

263 , with low functional richness at a mountain ridge under specific environmental conditions.

264 e of the petals on different portions (i.e., ridged vs smooth) is needed to understand whether distin

265 ork and the trailing edge orientation of the ridge was identified as the most important parameter to

266 The alveolar ridge was measured pre- and postoperatively to evaluate

267 llular model of the rat embryonic XY gonadal ridge) was reduced by 2-fold relative to wild-type SRY a

268 e) from naturally seleniferous habitat (Pine Ridge) was shown previously to have selenium (Se) hypera

269 Experimentally, we demonstrate ridge waveguide devices electrically tunable between 3.4

270 Ridge waveguides are designed with appropriate dimension

271 Thin films and ridge waveguides based on large-diameter semiconducting

272 GeSbS ridge waveguides have recently been demonstrated as a pr

273 Using multimode ridge waveguides, guided s-SWCNT photoluminescence is de

274 ethane seep sediments collected from Hydrate Ridge, we provide insight into the role of iron oxides i

275 s and simulations indicated that valleys and ridges were created by an out-of-plane grain rotation dr

276 nosis, while hyperkeratosis and fissures and ridges were independent risk markers of dermoscopically

277 omposed of dissociated edge dislocations and ridges where partial dislocations have recombined.

278 male baby born with growth on his mandibular ridge which was excised and was proved to be epulis on h

279 d that the flat slab is shallowest along the ridge, while to the northwest of the ridge, the slab is

280 flat solid surface is deformed into a sharp ridge whose orientation angle depends on the contact lin

281 atal, and interproximal height (P <0.05) and ridge width (P <0.01).

282 terproximal bone height (P <0.01), increased ridge width and bone density (P <0.01), enhanced 7-day p

283 nd at implant placement, including change in ridge width and change in buccal and lingual ridge heigh

284 Loss of alveolar ridge width and height after tooth extraction is well do

285 is to compare dimensional changes including ridge width and height at the two healing time points.

286 onths (6.0 versus 4.62 mm), and radiographic ridge width at 3 mm from the alveolar crest (6.17 versus

287 regeneration (4.75 versus 1.85 mm), clinical ridge width at 5 months (6.0 versus 4.62 mm), and radiog

288 The crestal ridge width for the CAN group had a mean gain of 2.0 +/-

289 No significant difference in ridge width loss was found between groups.

290 n ridge height occurred, and the majority of ridge width loss was localized to the buccal aspect.

291 When RP was performed, ridge width loss was not significantly decreased, but th

292 Two-thirds ridge width reduction was experienced on the buccal aspe

293 Loss of augmented ridge width was 34% +/- 17% for the CAN group and 28% +/

294 Reductions in ridge width were most pronounced on the coronal aspect,

295 inant for amount of change in crestal GT and ridge width.

296 owed scalloping over the right supra-orbital ridge with an intact bone.

297 ssions that are conceivably cryovolcanic and ridges with complex bladed textures.

298 Regular ridges with spacings of 3,000 to 5,000 metres and depths

299 cross a fitness valley or traverse a fitness ridge, without reverting to more complicated mathematica

300 nvelope protein corresponding to the lateral ridge (ZV-54 and ZV-67), C-C' loop (ZV-48 and ZV-64), an