- Topography And Glsci - Alaska DGGS
G C 1 m NARY REPOFtTOF TOGIAK LAICE AaGION,Iotsoduct ion:New d i s c o v e r i e s of place gold were r e p o r t e d made SyEskimos, Lapp r e i n d e e r h e r d e r s , and w h i t e p r o s p e c t o r s a t v a r i o u s p a i z t si n cn area hesded by t h e Togiak, Kanektok, and Eek r i v e r s d u r i n g t h egas!; eesson.Uining ms r e p o r t e d i n p r o g r e s s by t h e n a t i v e s , and ad r i l l was i n o p e r a t i o n on t h e le::. d i s s o v e r i g e on Eek River. lWny r e q u e s t s were r e c e i v e d c o n c e r n i n g t h e s e d i s c o v e r i e s . The %ek R i v e rXining Compeny o f f i c l a l s wanted i n f o r m a t i o n i n r e g a r d t o d r i l l i n g , Lnf o m a t i . c n r e g a r d i n g th9 p l a c e r d e p o s i t s on Rainey end Capa roncreeks?:as l a c k i n g . The f o l l o w i n g i n f o r m a t i o n i s compiled from o b s e r v a t i o n e ,i n f o r m a t i o n from p r o s p e c t o r s , and r e p o r t s . Eleven days wers s p e n t i n t h ef i e l d i n t h i s section.Locution, A c c e s s i b i l i t y and Drainage:The Togiak M e r e g i o n i s l o c a t e d i n t h e 3 r i s t o l Bayp r e c i n c t o f t h e T h i r d D i v i i o nand i n l a n d a d i s t a n c e o f 75 m i l e s from t h en o r t h e r n s h o r e of a r i s t o l Bay. Togiab: Lake l i e s between two d i v i d e s ,e x t e n d i n g i n a n o r t h and south d i r e c t i o n . 'Phe d r a i n a g e over t h e d i v i d et o t h e e e s t f l o w s i n t o t h e Wood R i v e r Lakes and t o Nushagak B y , Thed r a i n a g e on t h e west flours dorm t h e KaneM;ok R i v e r t o Yuskokwim Bay.The b e s t means of r e a c h i n g t h i s r e g i o n i s by a i r p l a n e ,which make l a n d i n g s on Togiak, K a g a t i o r Q iinhagab:l & e s w i t h gontoons,o r on A3 J o n e s t l a n d i n g f i e l d near t h e head of Eek River. C t h e r l a n d i n g shave b e e n made on g r a v e l bars n e s r t h e head and a l o n g upper 'Toeial iver.Planes can be c o n t a c t e d a t B e t h e l , P l a t i n u m o r D i l l i n g h m . R a t e s varyfrom 30 t o 50 p e r hour, T h i s r e g i o n c a a l s o be reached w i t h p o l i n gb o a t s up t h e Togiak R i v e r from i t s mouth a t Togiak. T h i s r i v e r i sn a v i g a b l e t o Togiak Lake, w i t h a few r a p i d s which c m be poled d u r i n glow water s t a g e s . T h i s i s t h e s h o r t e s t r o u t e by b o a t . The o t h e r r o u t ei s up t h e Kanektok R i v e r from Quinhsgak on Kuskokwim Bay. T h i s r i v e ri s n a v i g a b l e w i t h r i v e r b o e t s t o H a g a t i o r Quinhagak Lake.Topography-and Glsci at ion:The mountains i n t h i s r e g i o n o c c u r as i n d i v i d u a l n e s t sc l u s t e r e d around t h e i a t r u s i v e s and extending i n e l o n g a t e d d i r e c t i o n si n a n o r t h e a s t - o u t h w e s t d i r e c t i o n . The c e n t r a l i n t r u s i v e c o r e s r i s et o h e i g h t s o f 3,000 t o 7,000 f e e t w h i l e t h e s u r r o u n d i n g peaks r a n g ebetween 2,000 aod 3,000 f e e t , The h i g h e s t mountain i s Mt;. O r a t i a , whichr i s e s t o a h e i g h t o v e r 7,000 f e e t . Other mountains i n t h e r e g i o n areF i s k u k Peak, Atayak Mountain, T i o k p i t Mountain, and s e v e r a l o t h e r unnamed peaks, The h i g h e r mountains show c o n s i d e r a b l e e v i d e n c e of
g l a c i a t i o n , which as a r e s u l t h a s l e f t many s t e e p welled v a l l e y s ,p i n n a c l e peaks and mountain lakes. However, no g l a c i e r s e x i s t a t t h ep r e s e n t time. Most of t h e g l a c i a l v a l l z y s lead down and connect upw i t h t h e wide s t r u c t u r a l v a l l e y s between t h e mountain masses. Smallg l a c i e r s no doubt joined w i t h t h e l a r g e r g l a c i e r s t h a t followed t h es t r u c t u r a l v a l l e y s toward t h e sea, These wide v a l l e y s c o n t a i n t h ep r e s e n t d r a i n a g e systems. Bcrvever, many lower mountains, r i d g e s andweas escaped g l a c i a t i o n . These c o n t a i n a d i f f s r e n t , more r o l l i n g andless i r r e g u l a r topography, These a r e a s were no doubt low enough to haveescaped g l a c i a t i o n from above, and missed t h e large g l a c i a l m e s e sv d i c hfollowed o n l y t h e lower topography.I n these l a t t e r areas, witht h e i r s m a l l d.rainage systems, most of t h e p l s c e r p r o s p e c t s were noted.The upper v a l l e y s of t h e Eek, h e k t o k and Togiak r i v e r s a l l occupyl a r g e wide g l a c i a l v a l l e y s . These sre e e s i l y d i s t i n i e b ebyd theirshzpe, presence of e x i s t i n g l a k e s , c h m a c t e r o f t h e g r a v e l s , and t h emarginal morzines along t h e sides of t h e v a l l e y s . Drainage systems oft h e u n g l a c i a t e d areas a r e c o n s i d s r a b l y chanzed 2nd a l t e r e d . The i m f o r t s tfeature i n prospecting within t h i s region i e t o recognize t h e g l a c i a t e dv a l l e y s from t h e u n g l a a i a t e d o r s l i g h t l y g l a c i a t s d v 8 l l e y s and areas,General G e o l x :Only t h e northwest s e c t i o n of t h i s r e g i o a was v i s i t e d byt h e w r i t e r , which extends from t h e northwest s l o p e o f Piskuk Peak northw e s t t o tk3 north lrestslopes of Mt, O r a t i a , f o l l o w i n g t h e 7mtsrshed o ft h e upper iCeneHok and Eek r i r e r z ,.Ganeral geology o f t h i s r e g l o o i s shovm cn a s m a l l - s c a l emap, e x t e n d i n g from h k s C l a r k t o t h e Bring Sea, o f t h e e n t i r e lowerKuskoWm e g i o r , T h i s ;nap 13 contained inU.S . G. S o Bull. 622,"Mineral Resowr as o f Alaska, 1914," by A. H. * aks st a l . The f o m : i b ? ?a s given 02 t h e map range from Paleozoic and o l d e r s c h i s t s , s l a t e s ,c r y s t a l l i n e l i m e s t o n e s , and v o l c a n i c rocks, Mesozoic s a n d s t o n e s , s h a l e s , o g l o x e r a t e sl ,a t e Mesozoic o r a a r l y T e r t i a r y i n t r u s i v e s and s a d h e n t a r ysandstones snd s h a l e s t o r e c e n t unconsolidated g r a v e l s , s i l t s , e t c , Thes e c t i o n e a s t o f Togisk Lake, and exLending southwest, i s a wide band c iMesozcic s a n d s t o n s , s h a l e , e t c , The s s c t i o n west oP t h e Sake and r i v e rc o n s i s t s o f a b e l t of P a l e o z o i c s c h i s t , s l a t e , c r y s t a l l i n e l i m e s t o n e , etc,Ad j o i n i n g this S e l t on t h e west and extending southwest beginning withPiskuk Peak, a s e r i e s of i n t r u s i v e s zr i n c o n t a c t w i t h these n l d e rsed.irnents, Northwest of P i s k u k Peak snd on t h e west c o n t a c t of t h ei n t r u s i v e s , t h e Eesozoic s e d i n e c t s a g a i a cccur, These S e P t s of s9diments, RB they c c m r i n t e r m i t t e n t l y , m e w cbserved. i n t h e r o u t e traveledbetween Piskuk Peak end Xt, O r a t i n .
The heeP ters of th9 ICazektok R i v e r c o n s i s t of se srals m l l strsmo flowing i n t o t h e l a r g s v a l l e y which t h i s r i v e r occtlpies.These l a g s v a l l e y s c o n t a i n e a r l y T e r t i a r y s a n d s t o n e s and s h a l e s whichare i n p a r t ccnl-bearing.Narrow searns of l i g n i t e c o a l were observeda l o n e t h e bank2 cf t h e r l v w i n jts upper p o r t i o n , where i t and i t st r i b u t a r i e s a r e i n t r e n c h e d i n t h e s o f t sedimente. Placer gold h a s beenfound by n a t i v e Esklmos a t t h e heads o f t h e s e t r i b u t a r i e s ,D i r e c t l y n o r t h oP Kagati Laks l i e s M t . O r a t i a . This i s al a r g e i n t r u s i v e lirass o f g r a n i t a i d rocks and i n t r u d e s both P a l e o z o i c sndldesoaoic sediments, Quartz antimony veins were f o a d a t t h o head o fAtmugiak Creek, which f l o w s i n t o K a g t iLake. Placer g o l d p r o s p e c t shave been B o n d i n a few o f t h e c r e e k s t h a t head on t h e west s l o p e oft h i s xountnin, Eek River hesds ir a s m a l l l d s e t h a t l i e s on t h e s l o p eo f X t , O r a t i a on t h e north:vest s i d e , 'The r i v e r f l o w s s o u t h f o r a fewm i l e s and e n c o u n t e r s a m g i n a l g l a c i a l moraine, t u r n s west around t h eend of an elongated r i d g e o f w e l l worn h i l l s and e n t e r s s wide g l a c i a lv a l l e y f l o w i n g n o r t h and west. T h i s v a l l e y is o v s a m i l e i n width andc o n t i n u e s northwest u n t i l i t r e a c h e s t h e l e v e l c o a s t a l p l a i n , where I tt e r m i n a t e s , Thence Esk R i v e r t u r n s west and begins i t s meanderingcourse through low h i l l s and over t h e f l a t c o a s t a l p l a i n t o !CuskokwimBay. Gold h a s been found o n t h e s h o r t t r i b u t s r i e s t h a t f l o w from t h eeloxlgated r i d g e which the r i v e r i t s e l f f l o w s aroundo The moat importantof these a r e Rainay snd Capa:mn creeks, :Prospects of gold were found onEek R i v e r and Lha r i s e r i s s t a k e d for s e v e r a l m i l e s below Eek Laks,New placer gold d i s c o v e r i e s were made by n a t i v e Eskimosand Lapps o n T r a i l Creek, a t r i b u t a r y a t t h e head f Togiak Xfvsr, i nt h e f a l l of 1936. hfItfie1#S p a i n ( a Lapp) made t h e d i s c o v e r y an8 t h i sseeson he was r e p o r t e d ground s l u i c i n g on t h e disccvery, Only a fewouncas wera r e p o r t e d obtained. S i x n a t i v e Eekinos w e r e engeged i n mini n g below S p a i n on T r a i l Greek,M r . Oscsr Dahlmade an i n v e a t i g a t i o a o f t h e s e discoveriesd u r i n g July of t h i s year. He r e p o r t e d T r e i l Creek as a t r i b u t a r y ofu s p e r Togiak River ( n o t e s k e t c h ) flowing west and s o u t h f r o n t h e d i v i d ed r a i n e d on t h e n o r t h by Keelor Fork, a t r f b u t e r y of t h e Guithluk 2iver.It flows over most of i t s l e n g t h i n a box canyon w i t h a s t e e p g r a d i e n t .N1mero' s large boulders -tare observed i n t h e bed, and t h e g r a v e l s weret h r e e t o f c n r f e e t i n depth. The v a l l e y showed e v i d e n c e o f g l a c i a t i o n .Most of t h e gold found by M. S p a i n was irnCer o r a l o n g s i d a t h e l s f g eb o i l d e r s , As s r e s u l t of h i s prsspec4;ing h i s o p i n i o n was t h a t t h e c r e e kand d i s c o v e r y a r e not c f imgerfance o t h e r thsn f o r s n i p i 3 g .
Ke f x t h e r e p o r t s t h a t Togiak 3 i v e r below Trhil ilr99k hasbeen s t a k e d f o r several m i l e s . He f u r t h e r expressed t h e opinion t h a t t h eval:Ley w i t h i t s wide n a t u r e , g l a c i a l evidence and a p p a r e n t l y deep g r a v e l swas not o f inpcrtance, No work was i n p r o g r e s s on these lower c l e h .Vlit!i t h e above information, t h e w r i t s r was of t h e o p i n i o n thst t h e s e d i s c o v e r i e s d i d not warrant i n v e s t i g a t i o n ,Alfred and Ole h d e r s o n were e p o r t e dgr0ur.d s l u i c i n g on at i b u t a r yo f Fork Greek, and R e m a O m a s was r e p o r t e d mfnjng 9n CanyonCreek. D e t a i l s r e g y r d i n g t h e s e p l a c e r d e p o s i t s and t h e Golden Buttequartz prospect on Callyon Creek, i t geology,his coatsine4 i n a repcrtby F. W. X o l z h s h e r , 1326, Ke d e s c r i b e s t h e f o r n a t i o n a s c o n s i s t i n g o fr h y o l i t e t u f f , chert, 2 z g i l l i t e , c o a g l o z s r a t e , quartz por2byrg and b l a c ks l a t e . These are p o s s i b l y t h e Paleozoic s e r i e s of sediments as showr ont h e map st Tage 26e, Bull, 622." These sediments no doubt extend s o u t hi n t h e v i c i n i t y of T r a i l Creek which Y.%S r e p o r t e d five m i l e s s o u t h ofCanyon Creek,Prcspectg:The most promising p r o a p s c t s found i n t h e Eek R i v e r s e c t i o noccur on Xniney Creek. Gold was discovered h e r e by N e i l C o r r i g d i n 1320,He and a s s o c i a t e s worked t h e creek f o r f o u r seasons and 4500 from twocreek c l a i m s was recovered, L a t e r n a t i v e s mined f o r one season and obtained 600 i n gold. h s t s e a s o n f i f t e e n c l a i m s were staked by F, C. Xiseman,N e i l C o r r i g a l and G i l b e r t McIntyre o f Bethel,runs i n t o ZekRainsy Creek has a l e n g t h o f 6 m i l e sRiver on t h e r i g h t l i m i t , approximately 1 5 m i l e s below Eek Lake. Raineyheads n e a r t h e c e n t e o f an elongated r i d g e o f w e l l worn h i l l s . T h i sr i d g e o f h i l l s extends n e a r l y 20 miles i n l e n g t h , s t a r t i n g on t h e northx e s t s i d e of Xt. 3 r a t i a and e x t e n d i c g southwest b e t m e n M t . Q r a t i a andEek R i v e r v s l l o y . The r i d g e i t s e l f i s an a n t i c l i n a l s t r u c t u r e of f o l d e dsediments o f sandstone, s l a t e , graywacke and some i n t r u d e d p o r p h v y . T h i sa n t i c l i n a l s t r u c t u r e a p p e a r s t o have been caused by an i n t r l s i o nundern e a t h which e l e v a t e d t h e sediments. This i n f r u s i o n caused a h a r d e n i n go f t h e sediments along t h e c o n t a c t s and w i t h t h e wearing down o f t h e surrounding country, t h i s r i d g e r e m i c e d i n i t s p r e s e n t elongated, e l s v a t e dp o s i t i o n . While t h e i n t r u s i v e i t s e l f does not s p p c r e n t l y shmr on t h esurface, i t i s no doubt r r e s e n t underneath, The w e o i n gdown o f t h es e d i a e n t s and t h e r e l c t e d porphyry c o n t a i n i n g t h e m i n e r n l i z a t i c n i sprobably t h e source o f t h e 2 l a c e r g o l d found i n t h e craeks. The a c companying s k e t c h sho:vs t h e l o c z t i o n of t h e d i s c o v e r i e s o c 4ainey Creekand the head o f C a p m n .
The g r a v e l s on Rainey Creek extend a c r o s s a width o f 200t o 300 f e e t and v a r y from 5 t o 1 2 f e e t i n dept;h, They c o n t a i n n m e r o u sw e l l worn b o u l d e r s of smell s i z e , w a t e r worn, and which range i n s i z e from4 t o 18 i n c h e s i n diameter. They a r e flat and o b l o r g i n shape, and consist o f grsywacke arkose, sandstone, with an o c c a s i o n a l l a v a boulder. Thebedrock c o n s i s t s of graywacka, s l a t e and shale. S m a l l q u a r t z a t r i o g e r eoccur i n t h e gray.vacke and s l a t e and c o n t a i n a sparse m i n e r a l i z a t i o n ,A pan t a k e n from t h e g r a v e l s near bedrock c l n gt 5 e b m k of the m e e k ont h e upper d i s c c e r i e sehc :. d 1 2 m e d l l m t o l e r g e c o l o r s , some o f whichwsre rounded and w e l l worn and o t h e r s r a t h e r rough. Black sands, p y r i t e ,a r s e n o p y r i t e , r e a l g a r and orpirnent !Irere t h e a s s o c i s t e d h s a cj o n c e n t r s t e .The workings c o n s i s t o f sever81 c u t s of s m a l l s i z e and twobedrock d r a i n s . Frcm t h e c t z?::crked Xeil C o r r i g a l r e p o r t e d t h e groundrum.isg 25 c s c t s c Ledrock f o o t .Located 300 f e e t above t h e upper d i s c o v e r i e s on Rainey( n o t e sketch) s e v e r e l s m a l l gash veins and i r r e g u l z x s s e s o f ? e a r l yl2ure r e a l g a r a c oi r p h e n t occur on t h e bank of t h e s s l tribut-.Smll a r vt ezi r s a m a e q c c i s t c d , 9 t3h e q u s r t z i s m i n e r a l i z e d w i t hp y r i t e and arsenopyyrite, T3e formetion i s interbanded graywacke, s a n d s t o r e ,and a s l a t y s h a l e ,A sample t a k e n from a 6-inch v e i n assayed 10.8 p e r c e n ta r s e n i c and no mercury,Gold was found i n small amount8 i n t h e g r a v e l s a t t h e headof 3apatuun Creek. Some micing h a s been done 5 m i l e s down on C a p a m from i t shead, T h i s c r e e k h a s a l e n g t h of 1 0 nilesflows northwest, emptyingi n t o Eek R i v e r approximately 12 m i l e s bslow t h e mouth o f Rainey. Thehesd of Ceyavmn has a s t e e p grndient. Ths bedrock c o n s i s t z of s l a t e s ,s h a l e s , and grnywackes. The lower s e c t i o n , a s s e e n from t h e sir, flowsout i n t o a g l a c i a l valley,The Zek Xiver Mining Company, formed by Al. Jones and a s s o c i a t e s ,h a s s e v e r a l m i l e s of p l a c e r h o l d i n g s on Eok River e x t e n d i n g from above t h emouth o f Rainsy Creek t o bslow Eek Lake, The f o l l o w i n g s k e t c h shovrs t h el o c u t i o n o f t h e d i s c o v e r i e s and d r i l l holes. D r i l l i n g w i t h a n a i r p l a n ed r i l l was i n p r o g r e s s p r i o r t o t h e m i t e r ' s visit t o t h i s s e c t i o n . Threeh o l e s w e r e v d r i l l e d batween d e p t h s o f 40 and 60 f e e t on t h e r i g h t l i m i t ofEek R i v e r f i v e m i l e s above t h e mouth of Rainey. Bedrock was encounteredi n t h e f i r s t h o l e near t h e bench, but not i n t h e o t h e r tvn holes, Snallcopper nuggets vfere found snd an o c c s s i o n a l speck of g o l d , Uuewash g l a c i a lg r a v e l s were encountered w i t h some b l u e clay. T h i s r e g i o n no dcnbt was aworn topography p r i o r t o g l a c i a l t i r e sa3 t h e g l a c i a l g r a v e l s c o n t a i nnumerous worn and rounded b o u l d e r s s c a t t e r e d w i t h t h e g l e o i a l d e S r i s .
The i c e a c t i o n was t h e predominating f a c t o r i n c o n t r o l l i n g a ad l t e r i n gt h e p r e s e n t d r a i n a g a systems, T h i s i s v e r y much i n e v i d e n s e on llpuer EekR i v e r and i n t h e s e c t i o n where t h e d r i l l i n g was done. Above t h e l o c a t i o no f t h e d r i l l i n g , Eek R i v e r i s i n t r e n c h e d , c u t t i n g a c r o s s t h e s t r i k e of t h esediments, T h i s intranchmezt has been s i n c a g l a c i a l t b . 3 and was causedby t h e damming a c t i o n of t h e m a r g i n a l n o r a i n e i n t h e wide v a l l e y t c t h esouth, S h a l l o . : g r a v e l s a r e d i s t r i b u t e d i n t h e v a l l e y a c r o s s t h e width o ft h e i n t r e n c h m e n t , a d i s t m c e of 200 t o 300 f e e t . P l u c s r gold p r o s p e c t s wered i s c o v e r e d i n t h e s e g r a v e l s . Panning t h e dumps of t h e p i t s r e v e a l e d o n l ya few f i n e c o l o r s .A s m a l l crsek named Cloudy Creek f l o w s from t h e west s l o p eo f M t . C r a t i a n o r t h w e s t , and e n t e r s Eek R i v e r a b o et h e l a t t e r ' s entrenchment.t h e head a few c o l o r s were found i n t h e g r a v e l s , The lower 3 milee ofCloudy f l o w s s l o n z s i d e t h e m s r g i n a l moraine n di t s bed i s compose3 ofnumerous g l a c i a t e d b o u l d e r s . S e v a r a l c l a i m s hsve been s t a k e 6 on t h i s c r e e k ,f i o n g a s m a l l c r e e k l o c a l l y known a s I r o n Creek, a t r i b u t a r ya t s h e head of t h e K m e k t o k iliver, l o c e t e d 1 5 m i l a s s o u t h e a s t o f K a g a t iM e and 3 m i l e s west of 14enevok11k Lake, a p l a c a r gold d i s c o v e r y was madeb: two n e t i v e s , Guy Tegyl.re m d Vh. E i s e y u l i a , T ' l i sc r e s k he5 a lengt,hof 1 0 m i l e r and j o i n s t h e Kane'k-tok R i v e r 5 m i l s s abovg K a g a t i Lake.'Twenty c l a i m s a r e s t a k e d i n 8 group, l i n i n g :ms i n p r q r e s s wi5h twoa u t o m a t i c dams, T h i s c r e e k i s i n t r e n c h e d i n t o s h a l e a n 3 sandstone s e d i n e n t sw i t h a v a l l e y t h a t s v a r s g e s 300 f e e t i n widfb. Tke d i s c o v e r i e q w e m a rt h e head i n s h u l l o j rg r s v e l s and n e E . t h e mouth of' slnall gulclles t h a t e n t s rfrom t h e e s s k The a c c o m p n y t n g s k e t c h s)lovre t h e up
rum.isg 25 cscts c Ledrock foot. Located 300 feet above the upper discoveries on Rainey (note sketch) severel small gash veins and irregulz xsses of ?early 2ure realgar a ci orphent occur on the bank of the s sll tribut-. Smll artz veirs am aeqccistcd, 93 and A and the of of and
Alaska Airlines Inflight Magazine. Economics 300: Economy of Alaska, Notes-Introduction to Alaska Geography, page 9 Alaska Census Areas For purposes of collecting and reporting economic and social Alaska data, Alaska is divided into 27 “census areas.” These census areas are shown in the map below.
Judge Larry Zervos Alaska Superior Court, Sitka Rural Access Subcommittee Judge Dale Curda, co-chair Alaska Superior Court, Bethel Judge Roy Madsen (retired), co-chair Alaska Superior Court, Kodiak Louise Brady Sitka Tribe of Alaska, Sitka James Jackson Alaska Court Magistrate, Galena Judge Michael Jeffery Alaska Superior Court, Barrow
Division of Geological and Geophysical Surveys reports and maps on Alaska released during 1975 indexed by quadrangle: U.S. Geological Survey 0 pen-File Report 76- 332,95 p. Cobb, E. H., 1977, Selected Geological Survey and US, Bureau of Mines and Alaska
SIMPLIFIED lEDROCK GEOLOGIC MAP OF THE WALKER LAKE AREA, SURVEY PASS AND HUGHES QUADRANGLES, ARCTIC ALASKA, 1971 Figure 5 . 0 - 2 4 MILES SCOlO GEOCHEMICAL SAMPLING IN THE WALKER LAKE AREA, SURVEY PASS AND HUGHES QUADRANGLES, ARCTIC ALASKA, 1971 Figure 6 . 50 miles to the Kogoluktuk River in the eastern Ambler River quadrangle. .
Wholesale Trade, and Construction. Source: Alaska Department of Labor, . employment pie. 2 ALASKA ECONOMIC TRENDS AUGUST, 1998 Alaska Economic Trends is a monthly . the Employment Security Division and published by the Alaska Department of Labor, P.O. Box 21149, Juneau, Alaska 99802-
In addition to DEC, the slate agencies named as Defendants are: Alaska Department of Natural Resources, Alaska Oil and Gas Conservation Commission, Alaska Energy Authority, and Regulatory Commission of Alaska. 2 Kanuk v. State, 335 P.3d 1088, 1090 (Alaska 2014). 3 4 Id. at 1103. Id. at 1097. 1
Alaska Native Language Materials . in the . Alaska State Library . Historical Collections . Compiled by . James Simard . Alaska State Library - Historical Collections . Alaska Department of Education & Early Development Division of Libraries, Archives & Museums . P.O. Box 110571 Juneau Alaska 99811-0571 (907) 465-2925 Fax: (907) 465-2990
ANATOMI & FISIOLOGI SISTEM LIMFATIK DAN KONSEP IMUN Atika Dalili Akhmad, M. Sc., Apt . PENDAHULUAN 20 L cairan plasma difiltrasi keluar menuju bagian interstisial, 17 L direabsorpsi oleh pembuluh darah, BAGAIMANA 3 L SISANYA ? Sistem Limfatik sistem yang terdiri dari pembuluh, sel, dan organ yang membawa kelebihan cairan insterstisial ke dalam aliran darah dan filter patogen dari darah. FUNGSI .
