RMRDEAA4–. The effect of structures and lake level on bluff and shore erosion in Berrien County, Michigan, 1970-74. Offshore structures; Beach erosion. I I I I I I I I I r I I I I I I I I I I I I I I I 20 - 10 Shoreline Chonge. Bluff Recession I I I I I ' I I I I -20 -30 70 80 90 100 Slotion Figure 8. Rates of bluff recession and shoreline change along reach A from 19 November 1970 to 23 November 1974. Table 5. Summary of bluff. shore, and beach data for reach A (57 stations). Date Bluff recession | Shoreline change Beach width' Period length Rate 0 Max. Rate o Max. 0 Change (m) (m/yr) (ra/yr) (ni/yr)
RMRR1ME5–. Aerographer's Mate 3 & 2. United States. Navy; Meteorology; Oceanography. AEROGRAPHER'S MATE 3 & 2. 120.8 Figure 7-12. —Radio Receiver R-1051B/URR. LINE METER LINE GAIN +ro 0 5 LINE LEVEL OFF. ANT .TRIM . > O x- —I o /*&* «R k 6*1 3F" ^ o o >? AGC MED SLOW i FAST 4 7 6 0 10 AUDIO RESPONSE SHARP WIDE OFF 10 BANDWIDTH KC BFO . PITCH + RA0K> RECEIVER R-390A/URR BREAK IN OFF ON CARRIER LEVEL * TT^ % o O o C( o -4 o (GJH UBSli) is- a Q AGC MGC STANO BY^^—*V^CAL BFO OFF ON KILOCYCLE CHANGE CAUTION READ INSTRUCTIONS PACKED WITH EQUIPMENT BEFORE USING LOCAL GAIN PHONES 0*
RMRFCKYT–. Growth of ponderosa pine poles thinned to different stocking levels in central Oregon. Ponderosa pine Oregon; Ponderosa pine Oregon Spacing. 03 200 - i— pe 180 - en 160 - E 0) i— 140 - o c "S 0 120 - o E (J 100 - 3 z o 3 > O 80 - TO 3 60 - C C n 40 - o T3 20 - 0) a 5-year growth period First | Second 0 Third 6 11 1f 30 Gross -Net 3 8 16 60 2 12 15 5 7 10 4 9 13 Plot number SO 100 120 Growing-stock level 1 14 17 150 Figure 5.—Periodic, annual net- and gross- volume increment of ponderosa pine poles thinned to six different growing-stock levels on a productive site in central Oregon
RMRF4269–. Growth of ponderosa pine poles thinned to different stocking levels in central Oregon. Ponderosa pine Oregon; Ponderosa pine Oregon Spacing. 03 200 - i— pe 180 - en 160 - E 0) i— 140 - o c "S 0 120 - o E (J 100 - 3 z o 3 > O 80 - TO 3 60 - C C n 40 - o T3 20 - 0) a 5-year growth period First | Second 0 Third 6 11 1f 30 Gross -Net 3 8 16 60 2 12 15 5 7 10 4 9 13 Plot number SO 100 120 Growing-stock level 1 14 17 150 Figure 5.—Periodic, annual net- and gross- volume increment of ponderosa pine poles thinned to six different growing-stock levels on a productive site in central Oregon
RMRGYFYX–. Bulletin. Ethnology. Figure 87.—Distribution of flint types 6, 8, 16, and 22, site Ct^ 27. FOOT FIVE FOOT TEN FOOT LEVEL 1 CUT 1 CUT 0 TOT/ 1 2 0 1 1 3 3 1 4 4 4 5 9 5 3 4 7 6 1 1 2 7 2 0 2 6 4 2 6 9 19 25 44 10 1 1 49 60 II 2 1 3 12 0 1 1 13 2 2 14 0 15 0 16 0 17 0 18 0 142. Figure -Distribution of flint type 3, site Ct° 27.. Please note that these images are extracted from scanned page images that may have been digitally enhanced for readability - coloration and appearance of these illustrations may not perfectly resemble the original work.. Smithsonian Institution. Bureau of American Ethn
RMRF426J–. Growth of ponderosa pine poles thinned to different stocking levels in central Oregon. Ponderosa pine Oregon; Ponderosa pine Oregon Spacing. Ill Q. 0.40 0.35 0.30 0.25 0.20 0.15 0.10 c c <" 0.05 - Five-year growth period [J First ] Second [I Third lilt 30 2 12 15 5 7 10 Plot number 80 100 Growing-stock level 13 14 17 120 Figure 3.—Periodic, annual growth in diameter of ponderosa pine poles thinned to six different growing-stock levels on a productive site in central Oregon. Five-year growth period. 6 11 18 3 8 16 2 12 15 5 7 10 4 9 13 1 14 17 Plot number 30 60 80 100 120 150 Growing-
RMRHMBKJ–. The Biological bulletin. Biology; Zoology; Biology; Marine Biology. 72 s .111 IVSKI i I AL. -• "•• 00 A^-^ o :o.o v 40 - V l.V3kPa 5/5 D S->kPa 20 v 'JiJ officinalis O 4.3 kli n i i i i i i i i i > i Cv: 0.4 cvt. cvS 7.0 7.2 7.4 7.6 7.S S.O S.I 8.4 pH Kigurv 3. IVpiciion of oxygen-binding properties of ,Siii {fh'iiwlis hemocyanin at temperatures between 0 and 20 C in a pH saturation digram. Each lino indicates an oxygen isobar and shows the changes in oxygen binding depending on ,-il s vaturation: p*>ims were chosen ai regular intervals faun the continuous rcvotu low level of
RMREJMEH–. Coastal engineering studies in support of Virginia Beach, Virginia, Beach Erosion Control and Hurricane Protection Project : report 2, seawall overtopping evaluation. Sea-walls; Sea-walls. 6.5 7.5 8.5 Still Water Level (feet, NGVD) Figure B6. Swl versus overtopping rate, hurricane, 100% and 95% gain %y 0.9 - y ⢠0.8 - y / en 0.7 - 0.6 - y y ^â ^ c X ^^^ y^ ^^^ O m 0.5 - X y o 0.4 - ^^ X y'^ 0.3 - y y^ y 0.2 - y yy y y y yy y 0.1 - y 0 - ^â ^ II 1 1 1 6.5 7.5 8.5 9.5 Still Water Level (feet, NGVD) Figure B7. Swl versus overtopping rate, hurricane, 90% gain B12. Please note that these image
RMRH03XY–. Bulletin. Science; Natural history; Natural history. 1973 CLOD-CARD MI:.sui<l:MENT (il WATER MOTlOh â II iâr "iâr "iâr iâr [ii,i w.'i-.i to cr UJ. 1 i- *2 +1 0 -I -2 -3 -4 -5 -6 -7 -8 -9 -10 -II -12 -13 -14 -15 -16 -17 -18 -19 -20 -21 CLOD CARD CHANGE («) 0 6 12 18 24 30 36 42 48 54 60 66 72 78 84 90 96 102 108 114 120 126 SEDIMENT TRAPPED (°) GRAMS Figure I. Weight change of clod-cards and amount of trapped sediment plotted as a function depth. Data shown are from one 24-hour exposure period. Above the 4.2 m level, all sediment traps and some clod-cards were damaged by a boa
RMRFCM06–. Growth of ponderosa pine poles thinned to different stocking levels in central Oregon. Ponderosa pine Oregon; Ponderosa pine Oregon Spacing. Ill Q. 0.40 0.35 0.30 0.25 0.20 0.15 0.10 c c <" 0.05 - Five-year growth period [J First ] Second [I Third lilt 30 2 12 15 5 7 10 Plot number 80 100 Growing-stock level 13 14 17 120 Figure 3.—Periodic, annual growth in diameter of ponderosa pine poles thinned to six different growing-stock levels on a productive site in central Oregon. Five-year growth period. 6 11 18 3 8 16 2 12 15 5 7 10 4 9 13 1 14 17 Plot number 30 60 80 100 120 150 Growing-
RMRN9FKC–. An analysis of results of a high-resolution world ocean circulation model. Oceanography. I40E A- l/J ISOE I60E OEG ROBUST DIAGNOSTIC RUM, llHIUlt INItHYHL SCME iacIOR I t» in I 70E 3 TR REST I IH U KIN ricio mi 6 f* 27 8 11/9 AW «9 m,t IW7.75E.I5.25SI CASEA 2001 ITERATION 10000 1 PARALLEL OCEAM CLIMATE MOOEL (POCU) MALf DECREE »0B| 0 OCEAM CONf IGLMJAIION NO. 2 POTENTIAL TEMPERAT'.'KE LEVEL 37.SOU MOE I SOE I60E I 70E 180 1 70«. I40E ISOE I60E I70E *.- 1/3 OEG ROBUST DIAGNOSTIC RUM.FREE Therm UHIIXH INItHVM. • 1 tW MUX) niN • SCALE FACTOR ? 1.M FIELD "AX . 6 44 27.6 1179 AM 4| 1176 75E.
RMRHN2H3–. The Biological bulletin. Biology; Zoology; Biology; Marine Biology. 152 L. A. LEVIN W j 600- O o 500J O -i go 0> 400- z 300- 200- 100- 0 O o o o o. A A O 6 7 LENGTH (mm) 10 ? 700 n i LJ | 600- Q 5 500 40°" 300- 2OO- •k B O O O A A OA 34 36 38 40 42 44 46 48 50 52 NUMBER Of SETIGERS 54 56 56 60 62 64 FIGURE 2. Streblospio benedicti brood size as a function of: A) length and B) setiger number in the MERL eutrophication experiment, 12 May 1983. • = controls (Tanks 5 and 8); O = 8X enrichment (Tank 1); A = 32X enrichment (Tank 7). Evaluation of enrichment level effects on female trait
RMRGYG13–. Bulletin. Ethnology. FOOT LEVEL I 2 3 4 5 6 7 8 9 10 I I 12 13 14 15 16 17 18 FIVE FOOT TEN FOOT CUT CUT TOTA 1 0 1 0 2 2 1 2 3 10 6 16 3 3 6 3 3 6 7 6 13 30 1 1 41 69 85 154 45 29 74 1 1 1 12 3 4 7 5 0 5 0 1 0 0 0 1 0 1 1 0 0 0 0 0 0 342 Figure 84.—Distrib ution of. flint type 26, site Ct° 27,. Please note that these images are extracted from scanned page images that may have been digitally enhanced for readability - coloration and appearance of these illustrations may not perfectly resemble the original work.. Smithsonian Institution. Bureau of American Ethnology. Washington : G. P. O.
RMREHBRK–. Collected reprints / Atlantic Oceanographic and Meteorological Laboratories [and] Pacific Oceanographic Laboratories. Oceanography Periodicals.. • EB4I AT 20 M — BELLE FORECAST I i I I so *o I '° • *' ' 10 0 ?90 RADIUS Or MAXIWUM V/IND VS TIME BELLE o FliqM level (meosyred) * Sbrfccc (eitimaii) q 0 Q 0 o 0 O 0 « 0 0 00 0 J — • -»— "("fw oo —1—1—1—1—1—>—1—1—1—1 1 1- 1.. 1 1 , CENTRAL PRESSURi VS. TIKE 8&LLC * A Eai5 A eB4l * LANDFALL • • 9 *• * (forccotr). 08 10 12 K IG IS JO 22 CO C2 0« C6 06 10 12 14 16 18 20 22 00 02 QA 06 AUCUSI 8 ymj ,5„j, AUGUST 9 AUGUST 10 Figure 3
RMRR91DK–. Florists' review [microform]. Floriculture. :•/; ?-Jr.- 146 The Florists' Review June 8. 1922 PAPER POTS NBPONSET PAPER POTS. Theie are the new reduced f. o. b. Chicago Srices; down to pre-war level. Ize Grate Holds 2%-ln 1000 2%-ln 1000 8 -In 1000 8H-ln 1000 4 -In SOO 0 -In 500 6 -In 600 AMERICAN BtriiB CO., 172 N. Wabash Ave., Per 1000 I 4.00 4.76 6.26 8.26 10.60 16.00 21.00 Chicago, m. NBPONSET PAPER POTS. SAVE ON EXPRESS CHARGES. 2^-in., $3.85 per 1000; 2t,-ln., $4.60 per 1000; 8-ln., $6.10 per 1000; 3^-in., $8.00 per 1000; 4-ln., $8.95 per 1000; 6-ln., $15.55 per 1000; 6-ln., $20.86 pe
RMREJMEA–. Coastal engineering studies in support of Virginia Beach, Virginia, Beach Erosion Control and Hurricane Protection Project : report 2, seawall overtopping evaluation. Sea-walls; Sea-walls. 1 - 0.9 - %y ^^ > 0.8 - â¢â ⢠y 0.7 - ⢠y^ y y^ 0.6 - X ^^y y y y 0.5 - ^ y^ ^ ^ y ^ y y y 0.4 - y^ /^ y â ^ / ^ y y^ y 0.3 - '' y y"^ y y y 0.2 - ^ y^ -^ ⢠/ y y ^y y 0.1 - yy y / y yy y ^y y ^ O n - ^ t 1 1 1 6.5 9.5 Still Water Level (feet, NGVD) Figure B8. Swl versus overtopping rate, hurricane, 80% gain 0.6 - > 3. 8.5 Still Water Level (feet, NGVD) 9.5 Figure B9. Swl versus overtopp
RMRHN0P1–. The Biological bulletin. Biology; Zoology; Biology; Marine Biology. POLYP-LEVEL PREY CAPTURE EVENTS 97 Umean = 2-7 cm/s LI 60 • 50 ' 40 • 1 30 ' u 01 ft, 20 • 10 ' n = 207 ==£±1 1 I 1 1 mean = 12.2cm/s 60 n = 205 50 • T *- 40 | 30" a* ft. 20 ' 10 ' 1 0 1 = 19'8 80 • 70 ' 60 ' £ 50 ' 01 £ 40 ' £ 30 * 20 ' 10 ' n = 70 1 1 0 ' 0.0 0.2 0.4 0.6 0.8 1.0 0.0 0.2 0.4 0.6 0.8 1.0 0.0 0.2 0.4 0.6 0.8 1.0 Pharynx > Tentacle Tip (X/L) Figure 2. Location of prey capture events along the length of tentacles of polyps in the octocoral Alcyonium at three different flow speeds. See Figure IA for inte
RMREYTB2–. Effects of a power plant discharge into Monterey Bay at Moss Landing.. Oceanography. m m m m u ::::: $r» » ::::: m ft LEVELS 1 2 3 0^3 PiiS ^ 5 6 7 Id It 12 13 LEVEL 1 2 J 4 6 1 8 S ie a 1Z 13 TEflP. ( 56.93 - 58. M - 6».ee â 62. M - 64.ee - 66.ea - 68.81 - 69.39 â 72.ee â 74.ee â 76.ee - 78.8* ⢠8e.ee - DEC. F> 58.eo 6e.ee 62.ee 64.ee 66.ee 68. ei 69.9? 72. e« 74.ee 76.ee 7a.ee 8e.ee 32.ee AREA OF ONE ELEMENT (SO. FT.) 'TinE OF PASS ' 1326 ALTITUDE (FEET l 2eee HEADING (DEC. FROfl NORTH/ 29 SPEED (HPHi iee coin size in feet ⢠ieee nOSS LANDINC IR TEST 12/6/78 NUTI8EP OF ARE" E
RMRFW9CR–. The Canadian record of science. Natural history. ST, 1901 M^ feet. C. H. McLEOD, StiperintendenU. Sunday. SUNDAT. 86 oS 0.00 77 7b 0.00 88 74 07 0.28 41 .... 54 0.12 33 0.87 03 0.02 Means.. 1149 •» 17 Yearsmean^ for and including 57-»i this month - 0.24 1-34 3-57 "5 & DAY. " 0.00 0.04 1.11 0.0s 0.04 1.33 0,00 0.00 0.28 0.12 0.87 0.02 0.24 1-34 I 2 3 4 Sunday 1 7 8 9 10 12 '3 M IS 16 17 '9 20 21 22 23 24 126 >7 23 29 30 31 5-44 3-57 ( 37 Years means • 'for and including / this month. ^-level and Direction. Lken from Miles Duration in hrs. being 100. ours. Mean velocity... 1
RMRFW9BM–. The Canadian record of science. Natural history. IBER, 1901, feet, C. H. McLEOD, SuperintendenU DAY Sunday. Sunday. Sunday. 27 Yearsmea for and includir this month â. o .01 0 .04 23.8 [28.69 5 C 0.0 0.6 4 4 9-7 3-2 0.0 4.1 2.0 0.5 0.2 o o O. 1 â 5 S A 2 O.OI 0.04 I .02 0.44 0.99 0.32 o. 10 0.14 0.03 0.05 o.oo O. 12 o. 10 0.41 0.20 0.05 0.02 o.co 0.01 DAY. .Sunday 10 Sunday 17. lii 19 23 .SUNDAV 24 Sunday 25 26 27 28 29 30 3-74 27 Years means [for and including ' this month. â level and cen from. Mean velocity. 1st: the a range Greatest m|t day wa: 9tli, ISth and 2' Greatest vj on the hour on
RMRGYG08–. Bulletin. Ethnology. 254 BUREAU OF AMERICAN ETHNOLOGY [Bull. 129 FOOT FIVE FOOT TEN FOOT LEVEL 1 CUT 2 CUT 0 TOTAL 2 1 m 2 1 1 2 ; 3 2 1 3 i 4 0 6 6 ^ 5 6 2 5 2 3 7 7 8 4 9 19 12 3 1 2 24 6 1 5 II 43 18 4 i ^ 9 #^^^i^«^ 10 1 1 12 0 1 1 13 1 0 1 14 0 0 0 15 0 0 0 16 0 1 1 17 0 0 0 18 0 0 0 107 Figure 85.—Distribution of flint type 23, site Ct" 27. FOOT FIVE FOOT TEN FOOT LEVEL 1 CUT CUT TOTAL 1 2 3 4 1 1 5 0 0 6 1 1 7 3 3 8 2 3 5 9 5 6 1 1 10 4 0 4 1 1 0 0 0 12 0 0 0 13 1 1 O 14 15 16 17 18 Q. Figure 27 -Distribution of flint types 30 and 34, site Ct° 27.. Please note that these images a
RMRGX8J9–. Bulletin. Ethnology. Riv. Bas. Sur. Pap. No. 4] ADDICKS BASIN—WHEAT 169 in a grid of 1 m. (3.28 feet) squares numbered from the datum north along the base line and east or west along lines intersecting the base line at right angles. The stake nearest the datum became the desig- nator for that square. Excavation was by arbitrary levels of 15 cm. (0.49 foot). All material from each 15 cm. (0.49 foot) level and 1 m. (3.28 feet) square was screened and the artifacts segregated.. Figure 8.—Contour map and plan of excavation, Doerlng site (42/66A6-2). Depth was measured from surface at the level o
RMRJX2MN–. Atoll research bulletin. Coral reefs and islands; Marine biology; Marine sciences. 10 CM +8.0 +4.0 - 0 - -4.0 - -8.0 - -12.0. 1880 1900 1920 1940 1960 1980 2000 Figure 5. World rise in sea-level since 1880 from tide gauge records. Curve A based on Gornitz and Lebedeff (1987); Curve B based on Barnett (1988). Zero is taken as mean sea-level for the period 1951-1970 (From Gornitz 1991) level curves of Chappell (1982) for the northern Great Barrier Reef and of Scholl and Stuiver (1967) and Scholl et al. (1969) for the Gulf coast of peninsular Florida. In northern Queensland, the sea reached its
RMRPXMJJ–. Airborne radar. Airplanes; Guided missiles. 6-8] INFRARED SYSTEMS 343 100 Ji? 40- Background Predominantly Scattered Sunlight Mbsent at' V Night + Background Predominantly Black Body Radiation Night and^ Day U Energy Distribution ^ From Black Body at 600°K 4 rx Transmission of 10 mi. of Sea - Level Air Containing 6 cm 0 Vapor. Jb Cloud and Heavy Haze Background (^Energy Distribution' From 300°K Black vBody 4 X Exaggerated. Please note that these images are extracted from scanned page images that may have been digitally enhanced for readability - coloration and appearance of these illustrati
RMRGE433–. Bulletin of the Museum of Comparative Zoology at Harvard College. Zoology; Zoology. woodworth: geological expedition to brazil and chile. 131. no e> ^ o o ^V'c^^::yc Malvoa Station, 79 kms., alt. 43 M. (141.0 ft.). Good terrace on opposite or southwest side of river. At railway station there are clays. San Rosendo Station, 85 kms. alt. 46 M. (154.8 ft.). East of the Station there was in 1908 an excellent exposure of gravels and sands in a deep cut, rising about sixty-five feet above the railway, or to an elevation of 220 feet above sea-level. The annexed section is from a drawing made on
RMRJWYJ7–. Atoll research bulletin. Coral reefs and islands; Marine biology; Marine sciences. â 8 - S -12- £-16^ -20- â 24 -. -28 0 Twin Cays, Belize Mangrove Peat Wood Halimeda Sand Sea-Level Curve (Toscano & Macintyre, 2003) 2000 4000 6000 AgecalBP 8000 10000 12000 Figure 6. Calibrated age data from peat, wood, and Halimeda sand taken from Twin Cays cores in relation to the corrected western Atlantic sea-level curve of Toscano and Macintyre (2003).. Please note that these images are extracted from scanned page images that may have been digitally enhanced for readability - coloration and appear
RMRGF94M–. Bulletin of the Museum of Comparative Zoology at Harvard College. Zoology. WOODWORTH: geological expedition to BRA.ZIL AND CHILE. 131. , * X s ,⢠â ⢠⢠* f < ^V'cf::^ Malvoa Station, 79 kms., alt. 43 M. (141.0 ft.). Good terrace on opposite or southwest side of river. At railway station there are clays. San Rosendo Station, So kms. alt. 46 M. (154.8 ft.). East of the Station there was in 190S an excellent exposure of gravels and sands in a deep cut, rising about sixty-five feet above the railway, or to an elevation of 220 feet above sea-level. The annexed section is from a drawing made
RMRMJA5X–. Annals of the South African Museum = Annale van die Suid-Afrikaanse Museum. Natural history. HOLOCENE SUBMERGENCE ON REUNION ISLAND 73. Fig. 4. years IP. X1000 Rates of rise of sea-level on Reunion. appear too high if one considers those suggested for other subsiding volcanic areas: Micronesia (0,03 cm/year during the last 10 000 years: Bloom 1969), Mururoa (0,006 to 0,012 cm/year during the last 8 m.y.: Labeyrie et al. 1969) and atolls in the Pacific Ocean (average rates of submergence 0,002 to 0,004 cm/year: Hess 1965). The rates generally accepted for the degree of subsidence appear to be
RMRG89GN–. Bulletin - United States National Museum. Science. Nd.l Sea level, No,2 Sea level SABA ISLAND "B-B Sea level ^M^m^%%mm>%m^. 0- 1,000- A Sea level- "^^^MMM^^M^M^^t^ B NORTH SIDE OF ST THOMAS. 0 2 4 6 8. Please note that these images are extracted from scanned page images that may have been digitally enhanced for readability - coloration and appearance of these illustrations may not perfectly resemble the original work.. United States National Museum; Smithsonian Institution; United States. Dept. of the Interior. Washington : Smithsonian Institution Press, [etc. ]; for sale by t
RMRG89G9–. Bulletin - United States National Museum. Science. Nd.l Sea level, No,2 Sea level SABA ISLAND "B-B Sea level ^M^m^%%mm>%m^. 0- 1,000- A Sea level- "^^^MMM^^M^M^^t^ B NORTH SIDE OF ST THOMAS. 0 2 4 6 8. Please note that these images are extracted from scanned page images that may have been digitally enhanced for readability - coloration and appearance of these illustrations may not perfectly resemble the original work.. United States National Museum; Smithsonian Institution; United States. Dept. of the Interior. Washington : Smithsonian Institution Press, [etc. ]; for sale by t
RMRHTYH1–. Between-year movements and nest burrow use by burrowing owls in southwestern Idaho 1996 annual report. Burrowing owl; Burrowing owl; Burrowing owl; Bird populations; Burrowing owl. ground level. angle of interest (deviation from horizontal) nest burrow tunnel b) Kuna Butte Study Area nest burrows unused burrows ?0 degrees 50 20 degrees J I L •«: •:: — • m Grand View Study Area nest burrows unused burrows 20 de9reeS 50 20 de9reeS 50 •:• :*•••: 8 ° i 8°° i • 0 0 Figure 3. (a) Illustration depicting tunnel entrance angle and its measurement, (b) distribution and mean (*) of tunnel angles for us
RMRE95PN–. The Earth beneath the sea : History. Ocean bottom; Marine geophysics. --â iTc,- cA=«; /«- -'«- -> Profile 1 Profile 3 Profile 2 Profile 8 Profile 7^?°° Profiled 'â¢Â° ,'" t^-' Profile 4 Profile 5 50° 160° 150°. - X^â!l :^^^^ Sea level . "^^ ^^^-- -iooo f m:'???iT::: Profile imm Wm^^m^M:::^ "^ ^ Sea level mmm^ 1000 fm '----^- ?000 fm-- â â -,--;; Profile 4 ^"S-^â-T"^ 500 y 500; Nautical miles 0 20 40 60 I- SCALE VERTICAL SCALE. Please note that these images are extracted from scanned page images that may have been digitally enhanced for readability -
RMRGJ0KF–. Bulletin of the British Ornithologists' Club. Birds. [Bull. Brit. Orn. CI. 1988 108(1)]. I9e L9c 111 74< 73< 72° 7l« 221 Figure 1. Sketchmap of southwest Peru to show habitat zones and localities with their departments and altitudes (m). 1. Chala (Arequipa) 2. Pucchun (Arequipa) 3. Mollendo (Arequipa) 4. Mejia (Arequipa) 5. Ite (Tacna) 6. La Yarada (Tacna) 7. Tacna (Tacna) 8. Locumba (Tacna) 9. Moquegua (Moquegua) 10. Arequipa (Arequipa) 11. Huanca (Arequipa) 12. Sumbay (Arequipa) 13. Chivay (Arequipa) 14. Laguna del Indio (Arequipa) Sea-level 15. Crucero Alto 5 m (Arequipa) 4470 m 0-1
RMRJX26C–. Atoll research bulletin. Coral reefs and islands; Marine biology; Marine sciences. > (0 0) DC. -20 8 7 6 5 4 3 Years BP (xiOOO) Figure 15. Relative sea-level models for the 'far field' as a function of ice load, mantle viscosity and lithospheric thickness (after Nakada and Lambeck 1987). Ice-melt models: ARC 1,2: Arctic ice only; ANT1,2: Arctic and Antarctic ice. (4, 50): Upper mantle viscosity = 10^1 Pa, lower (>670 km) mantle viscosity = 10^3 Pa; 50 km thick lithosphere. Observed sea levels (closed circles) = N.W. Tuamotu archipelago (Pirazzoli and Montaggioni 1986).. Please note tha
RMRJM7JD–. Beach and inlet changes at Ludlam Beach, New Jersey. Beach erosion; Coast changes; Littoral drift. COUNTRY U. S. A. LOCALITY Spa jsie city Ludlcm Island TYPC OF M*Hf COE disk set in conc.mon. STAMPING ON MARK BE-H "0+33 STATION Profile line 8 BE-H Sta.-0+33 AGENCY (CAST IN MARKS) Corps of Engineers ELEVATION "OT (FT) LATITUDE 39°10'39. 59" (NORTH INC l(£AiLiIK&]M 125 403 LONGITUDE 7A"A0'28.07" DATUM Sea Level Datum 192 (f T) XM' (E A S TIN G iWofif KJHBT 1 997 789 IFTl GRID AND ZONE NJ Trans. Merc. INORTHINGIIEASTINCI (EASTINGXNORTMlNGt GRID AND ZONE ESTABLISHED
RMRJKW3Y–. Beach changes at Atlantic City, New Jersey (1962-73). Beach erosion; Coast changes. Derived from experienced record of NOS tide goge at Atlantic City (9-11 Mor. 1962) An arbitrary extension passing through the standard project hurricane volue of 16 feet assumed at 0.2 percent frequency J L 10 20 50 80 90 95 98 99 Frequency in Events / 100 Years 99.8 99.9 100 Figure 18. Frequency of maximum monthly high tides at Atlantic City (from U.S. Congress, 1964a). 20 r- 15 10 Trend Line. -10 1910 Figure 19. 1920 1930 1940 Yr 1950 I960 1970 Change in sea level with respect to adjacent land for Atlantic
RMRE94DX–. The Earth beneath the sea : History. Ocean bottom; Marine geophysics. V'H>^ Crystalline basement i'^V/V, Sub-basement Newfoundland C.St. l^ory NNE Nautical miles (c) Grand Bonks Sea level SSW. wsw 100 200 Nauticol miles Celtic Seo section 300 Water t r I III IA..„..,n hasementi,,.,^—X—---- P e - Per mianboseme^,,.^^-;^^^ 300 J L 200 J J I I L 100 80 60 40 20 0 (d) 10,000 - 20,000 Nouticol miles Fig. 8. Probable geological structure of the shelf and slope in north-eastei'n North America and in North-west Europe (Celtic Sea), according to geophysical investigations. (After Ewing, Bentley,
RMRFR05K–. Case histories of Corps breakwater and jetty structures. Breakwaters; Jetties; Breakwaters; Jetties. OCEAN SIDE (ALL SECTIONS) ™«ni umisr" 3000-5000 LB 20'± rrrmn 1/: } 1.5'Ml N -RESTORE EXISTING FOUNDATION BLANKET GROUND LEVEL STONE 2"-12" TOP CONC SHEET PILE EL VARIES 7—irai Bar NATURAL GROUND VARIES +6T0+12MLW Tr TYPICAL SHORE ANCHORAGE SECTION STATION 0+00- 7+00 NOTE: TOE PROTECTION ON BOTH SIDES FROM STA 7+00 TO 8+00 TOP CONC SHEET PILE EL +7.0 CREST ELEV +9' MLW 5-8 TON 15'±. UNDERLA YER STONE - FOUNDA TION BLANKET 1000-1600 LB STONE , 2"-12" NOTE: ELEVATIONS V
RMRG2M21–. The Canadian field-naturalist. 522 The Canadian Field-Naturalist Vol. 101 Table 2. Average temperature (°C, center) and wind speed (right) at three different altitudes on a west-facing slope entirely covered by coniferous stands in Whitemud Creek, Edmonton. The wind speed is expressed as a percentage of the speed that was recorded concurrently in an open field above. Position in slope Time (MST) Wind direction and speed (km/h) in the open Altitude above sea level (m) 08:00 14:00 20:00 02:00 SE 24.4 NE 26.1 NW 19.4 664 649 635 top middle' bottom -5.4 -6.6 -8.4 2.7 0.1 1.3 -1.6 -3.4 -3.3 -4.3
RMRFW9R8–. The Canadian record of science. Natural history. ABSTRACT FOR THE MONTH OF MARCH, 1899. Meteorological Observations, McGill College Observatory, Montreal, Canada. Height above sea level, 187 feet, C. H. McLEOD, Superintendent. THERMOMETER. Mean. Max. Min. Range,. BAROMETER. 30.583 30.538 30.283 30.456 76.64 S.W. N.E. N.E. 23.41= â 7.66 ANALYSIS OF WIND RECOED. N. N.E. E. S.E. S. 1 S.W. w. N.W. Calm. 2.03 1263 634 â 455 491 24,0 224i 995 '3.39 49 .02 58 107 loa 5> â 7 12.50 "94 .4.26 8.64 23.08 21.97 19.51 QwatDat Telooity in gustB 66 miles per hour o ResultaQt mileage, 2215 Resultant
RMRDYTJR–. The ecology of Tijuana Estuary, California : a national estuarine research reserve. Estuarine ecology -- California Tijuana River Estuary. b.7P Cen^ orV I â â â â i â â â â i â â â â l â â â â f â â ' )â ' ' â | " ' 'I ' ' ' M " ' ' I '' ' ' t " ' ' I ' ' ' ' i ' ' ' ' ' ' " ' 1 -t â â â â ! m 0.9 0 8 0.7 - 0.6 1905 1910 1915 1920 1925 1930 1935 1940 1945 1950 1955 1960 1965 1970 1975 1980 1985 Year Figure 2.2. Data on sea level rise for San Diego Bay, 10 km north of Tijuana Estuary. Yearly mean sea level is referred to the 1960-78 datum for mean lower low water (MLLW). T
RMRFW9FP–. The Canadian record of science. Natural history; Science. ABSTRACT FOR THE MONTH OF AUGUST, 1896. Meteorological ObservatiooB, McGill College Observatory, Montreal, Canada. Height above sea level, 187 feet. C H. McLEOD. Superintendent.. [Meai relative bumid 63-8 78.9 73.0 S.W. s.w. S.W. N.W. N.W. S.W. s. S.W. S.W. Mean velocity in miles perhouT Ss is .Sunday ... Sums AMALXSIS OF WIND RECORD. Direction N. N.E. E. S.E. •353 S.W. W. N.W. Calm. Miles 8 4023 1583 621 Duration in hrs . 82 ^ 2 •3 III 3-3 147 67 7 Mean velocity— 9-ot 5.50 15-54 12.19 12.85 10.79 9,27 lireatesi luilea SB lU 0. e hour
RMRMGMJF–. Annals of the South African Museum = Annale van die Suid-Afrikaanse Museum. Natural history. 0 m(x 10 ) . 20 . , . 15 . , , 10 , 8 6 5 4 3 2 1 ' M1OCENE PLIOCENE PLEISTO. TM 1.3,1.4,2.1 TM 22,2.3 I TM31 TM 3.2,33 TP1 7 TP3 01 B / UT Surface / 1 7ppm"^« deposits 9-I-GM-. Jqsm i » 1 1 BQF 1 / ^ / * / /elandsfontyn / FM. Bedrock 90 60 30 0 30 75 50 25 Years B.P xlO^. ^^IM/^ ' • ' I • • 'i' I • ' • ' I ' • 3-2,8 2 .-,6 1 PLIOCENE QUATERNARY I ' ' ' ' my Fig. 2. A. Gross Tertiary sea-level trends after Siesser & Dingle (1981). B. Langebaanweg deposits (south-western Cape) rel
RMRH08E4–. Bulletin. Agriculture -- New Hampshire. METEOROLOGICAL TABLES 181 RECORD Long. 70° otiMV. Baijometkii ij-j Fkkt Auox k Sea Level 1 2 3 â i ti 7 S 9 10 11 12 13 14 15 16 17 18 19 â¢20 21 22 23 24 25 2(j 27 28 29 m 31 rRECIPITATION.. r- X 9 a. in. 2.1 10. 8 a. 111. Night. 1. fi. 0 ]). 111. 8 p. 111. t) a. 111. Night. 12 111. 7 a. Ill 9 1 N. N. S.W. S.W., w. N. i W. ; W. N.W. N.W. N.W. N.W. N.W.i N.E. W. S.E. W. N.W. W. S.W. S.W. W. W. N.W. N.W. N.W. N.W. S. w. w. N.E. I'artly Clear. Clear. Partly Cloudy Cloudy Clear. Clear. Cloudy Clear. Clear. Clear. I'artly Cloudy Partly I'artly Tartly ]*ar
RMRCD2NR–. Discovery reports. Discovery (Ship); Scientific expeditions; Ocean; Antarctica; Falkland Islands. 212 DISCOVERY REPORTS level. The second period of increase is apparently the greatest, although in the sub-Antarctic this may be due to a single very large volume of 10-5 cc. for the 50-0 m. sample at St. 2219. Table 4. The monthly variation in the mean total volume of plankton {i.e. the sum of all measure- ments from 1000 to o m.). Numbers of observations are given in brackets Zone January February March April May June Sub-Antarctic Antarctic 7-03 (6) 6-86 (30) 10-15 (J7) 9-18(14) 9-44 (8) 10-3
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