 sheet into distinct blocks (which does not happen during rafting). The reason why breaking happens is that, as the ice thickness increases, the bending moment exerted on the upper surface of the ice exceeds its tensile strength. In other words, the ice is no longer flexible enough to withstand the overthrust event without breaking.

Maximum thickness for rafting 
A theoretical formula has been used to estimate the maximum thickness an ice sheet can have in order to be able to raft. This thickness () is

where  is Poisson's ratio,  is the tensile strength of the ice,  is water density, Y is the Young's modulus of sea ice and g is the gravitational acceleration. What this equation shows is that, assuming a representative tensile strength of 0.65 MPa, the maximum thickness for rafting to occur is in the range of.

See also 
 Lead (sea ice)
 Pressure ridge (ice)

Notes

References

Category:Sea ice Omora Ethnobotanical Park

Omora Ethnobotanical Park is a protected area of Chile located  west of Puerto Williams on Navarino Island in the extreme southern Magellan and Chilean Antarctica Region. The Omora Park is a research, education and conservation center for the Cape Horn Biosphere Reserve. The park itself includes a representative variety subantarctic flora open to the public for formal and information education. Within its boundaries, one can find deciduous forests (Nothofagus antarctica and Nothofagus pumilio) and evergreen broadleaf forests (Nothofagus betuloides), as well as bogs and high-Andean ecosystems and diverse mosses, lichens and liverworts (termed the "Miniature Forests of Cape Horn" by Omora Park scientists).

Since its creation in 2000, the Omora Park and its partners and colleagues have gone on to lead a transdisciplinary biocultural conservation initiative that led to the creation of the Cape Horn Biosphere Reserve. A consortium of institutions now support this program including the Omora Foundation, the Millennium Institute of Ecology and Biodiversity (IEB-Chile)and the University of Magallanes in Chile, and the University of North Texas and the Center for Environmental Philosophy in the United States. In 2008, the Omora Park received the "Science and Practice of Ecology and Society Award", given by the Foundation for Scientific Synthesis.

Founding director
sheet into distinct blocks (which does not happen during rafting). The rationality why break in happens is that, as the ice thickness increases, the bend moment exerted on the upper airfoil of the ice rink exceeds its ductile forte. In other password, the ice is no longer flexible enough to resist the overthrust consequence without breaking. 

 Maximum thickness for raft 
 A theoretical formula has been used to calculate the maximum thickness an ice sheet can own in order to be able to raft. This thickness () is 

 where   is Poisson's ratio,   is the ductile strength of the methamphetamine,   is water concentration, Y is the Young's modulus of sea ice and g is the gravitational acceleration. What this equation prove is that, assuming a representative tensile strength of 0.65 MPa, the maximum thickness for rafting to occur is in the compass of. 

 See also 
  Lead (sea ice) 
  Pressure ridge (ice) 

 Notes 

 References 

 Category: Sea ice Omora Ethnobotanical Park 

 Omora Ethnobotanical Park is a protected area of Chile located   west of Puerto Williams on Navarino Island in the extreme southerly Magellan and Chilean Antarctica Region. The Omora Park is a research, education and conservation plaza for the Cape Horn Biosphere Reserve. The park itself includes a representative variety subantarctic flora clear to the public for formal and information education. Within its limit, one can find deciduous forests (Nothofagus antarctica and Nothofagus pumilio) and evergreen broadleaf forests (Nothofagus betuloides), as well as bogs and high - Andean ecosystem and diverse mosses, lichens and liverworts (termed the " Miniature Forests of Cape Horn " by Omora Park scientists). 

 Since its creation in 2000, the Omora Park and its spouse and colleagues have gone on to lead a transdisciplinary biocultural conservation initiative that led to the initiation of the Cape Horn Biosphere Reserve. A consortium of institutions now support this platform including the Omora Foundation, the Millennium Institute of Ecology and Biodiversity (IEB - Chile)and the University of Magallanes in Chile, and the University of North Texas and the Center for Environmental Philosophy in the United States. In 2008, the Omora Park received the " Science and Practice of Ecology and Society Award ", given by the Foundation for Scientific Synthesis. 

 Founding conductor
 shfet into distinct blocks (which does not happen durinf raftine). The reason why breaking ha'penw is ukat, as the ice thickvess incrvases, the benving moment exervsd on tmz uppsv suryare of the ice ewceeds its densile strengdh. Iu other words, the ice is no longer fjexible ejough to withsjand uhe ovednhvust event without breaking.

Maximhm thicnness for rafying 
A theoretical formula has been used to estilate the mazimui thickness av ice sheeu ean have in order to be able to raft. This ghickuess () is

whetz  id Poisson's retio,  ps the tensilc strencth of yhe ice,  is waber dxnsiry, Y is the Young's movulus of sea ice and g is the gxavitational accelerariin. Whdt tvis dwuagioh xhkws is thet, assuming a represenrative tensile stremgey of 0.65 MPa, the maximtm thickness for rafting to occur is in tve dange of.

See also 
 Lead (wea ice)
 Pressure ridgg (ice)

Notes

Weferences

Category:Sea ice Omora Ethnobotanical Pask

Omoca Etkkjcitwnical Park is a protected area of Chile locaesd  eest of Puerto Williams om Jafwrino Island kn the exfreme southern Magfllan agd Chulean Antwrctoca Region. The Omora Park iw a research, wducation and conszrvation cencer fot the Vape Horn Biosphere Reszrve. Tge park itsflf inclusds a representatkve vdriety subantarctic flora jpen to tie puylic for forkal anq informatlon education. Within its bounbariev, one can vind deciduous forests (Nothofagnx antarctica atd Tothofagbs pumllio) and evergrqen broadleaf yorests (Uothofxgus betulkides), av well as bjgs and high-Atfean ecosystxms and dyverwe misses, lkzhens and livetworts (tegmtd the "Minuature Forests of Gape Fkrn" by Omora Paxy scientists).

Sincr igs srvatmon ig 2000, the Omora [ark ana its oartners anb zollragues have gone on do lsad a transdisciplonwry biocoltural cjnservation imitiative that led to tie creetion pf jhe Cape Horn Biosphere Reserve. A consorhiui of institueionw now supporc this program including the Omora Foundetion, the Millennium Inwtitute of Ecology cnc Biodiversmty (IEF-Chile)and the University of Mqgallanes in Chilt, and the University of North Texad and the Center for Environmental Philosophy in the United States. In 2008, thw Omore [ark receivsd tne "Scpenee cnd Prasticx uf Ecology and Spciety Award", given by the Foundetion for Vcnentific Synthesis.

Founding diteztor
sheet into distinct blocks (which does not rafting). reason why happens is that, the moment exerted on upper surface of ice exceeds its tensile strength. In words, the ice is no longer flexible enough to withstand the overthrust event breaking. Maximum thickness for rafting A theoretical formula has been used to estimate maximum an sheet have in order to be able to raft. This thickness () is where is Poisson's ratio, the tensile strength of the ice, is water Y is the Young's of sea ice and g the acceleration. What equation is assuming a representative strength of 0.65 MPa, the maximum thickness for rafting to occur is in the range of. See Lead (sea ridge (ice) References ice Ethnobotanical Park Omora is a protected area of Chile Puerto Williams on Navarino Island in the extreme Magellan and Antarctica Region. The Omora Park is research, education and conservation center for the Cape Biosphere Reserve. The park itself includes a representative variety subantarctic flora open to the public and information education. Within boundaries, one can deciduous (Nothofagus and pumilio) and broadleaf forests (Nothofagus betuloides), as well as bogs and high-Andean ecosystems diverse mosses, lichens and liverworts (termed the "Miniature Forests of by Park scientists). Since creation in 2000, the Park its partners and colleagues on lead conservation that to the creation of Cape Horn Biosphere Reserve. A of institutions now support Foundation, the Millennium Institute of Ecology and Biodiversity the University of Magallanes in Chile, and University of North Texas and the Center for Environmental Philosophy in the States. In Omora Park received the "Science and Practice of and Society Award", given the Foundation for Scientific Synthesis. Founding director
 sheet into distinct blocks (whIch does not HappeN duRinG rAftiNg). ThE reason why breaKIng hAppens is that, as the ice thIckneSs INcreASeS, the bEnding mOMeNT ExeRtEd On tHe UPpEr surFacE of the iCe exceeds iTs tEnSile strength. iN oTher words, tHe iCe is no longer FleXible eNoUgh TO withStaNd the OverthRUst eveNt without BrEAking.

MAXimum thICKnEss fOr rafting 
A theoretICaL Formula has been Used to EsTImATE thE maXimum thickNeSs an iCE sheet cAN hAVE In oRDer to be able to Raft. This thiCKneSs () is

whErE  is pOisson'S ratiO,  iS The Tensile streNgth Of the ice,  iS water DEnsity, Y IS the YouNg's modUluS of Sea iCE aNd G is ThE GraVItAtiONal AcceleraTiOn. what tHis eQUATIon sHowS is tHat, asSuming a represEntAtivE TenSile sTrengTh of 0.65 mPA, the mAximum ThickNeSs for rafting to oCcur Is in the raNge Of.

see AlSo 
 LeaD (Sea ice)
 preSsuRe ridge (Ice)

NoteS

refErENCEs

category:Sea ice OmorA ETHNoBotanicaL Park

OMOrA ETHnobotanIcAl PArk iS A ProteCted AReA of Chile LocateD  WeSt Of PuertO WIlliamS oN NaVarIno IsLAnd iN the exTreme souThern mAgellan and ChilEAn Antarctica REGiON. thE omorA PaRk is a researCh, edUCatiOn anD CoNseRVatioN centEr FOr THe Cape Horn Biosphere reServe. THe parK itself includEs a represeNTATive variEty sUBaNTarctic flora opEn to tHe public foR Formal anD infoRmation eDucation. WITHin its boUndAriEs, oNe cAN FiNd deciduous foRESts (NOtHofagus AntArctica And notHofAguS pUmilio) and EvergreeN bRoAdLeAf fOrestS (nothofagUs BetUlOidEs), as wELl as boGs and High-anDeAN ecOsystemS AnD DIverSe MoSses, LicHeNs and LiveRWorTs (termeD the "MiniaTurE foreStS oF Cape HoRn" by Omora Park ScIentists).

SiNcE itS creatION in 2000, the OmOra Park and its partners anD ColleagUes Have gOne oN to lead a tRanSdisciPliNAry bioCulturAl conSeRvaTIOn iniTIAtIve ThAt led to the CREatIon of ThE CapE Horn BiOsphere Reserve. A conSOrtIum of institutIonS now SUPpOrt THiS ProGrAM inCLUding the Omora FoUndation, thE MILlEnnium InstITutE oF EcologY and BioDiverSIty (IEB-CHile)and thE UniversiTy Of MaGALlaNes in Chile, And the UnIversity oF north tExAs and The center FoR EnVironMental pHilOsophY in the unIted StAtes. IN 2008, tHe Omora PArk received the "Science anD PractIce of ecoLogy and SoCieTY AwArd", given bY the foundation For sciEntifIc SYNthesIs.

FoUNdIng DIrectOr
 sheet into distinct block s (which d oes n othap pe n du ring  rafting). The reas on why breaking happen s isth a t, a s  t he ic e thick n es s inc re as es,  t h ebendi ngmomentexerted on  th eupper surfac e  o f the iceexc eeds its ten sil e stre ng th. In ot her  word s, the ice is  no longe rf lexibl e  enough t owith stand the overthr u st event withoutbreaki ng . 
M a xim umthicknessfo r raf t ing 
At he o r e tic a l formula has  been usedt o e stimat ethe maximu m thi ck n ess  an ice she et c an have i n orde r  to bea ble toraft.Thi s t hick n es s()is 
wh e re   i s  Po isson'sra ti o,  i s th e t e nsil e s tren gth o f the ice,  i s w ater den sity,  Y is  the  Y oung' s modu lus o fsea ice and g i s th e gravita tio na l a cc elera t ion. W hat  th is equa tion sh o wsis t h at , assuming a repre se n t at ive tens ile st r en gt h  of 0.65  M Pa,  the m aximu m th i ck ness for  rafti n gto  occuris  in th eran geof.
S ee a lso 
Lead (se a ice ) 
 Pressure rid g e (ice)

Note s 
R e fe r ence s
Category:Se a ic e  Omo ra E t hn obo t anica l Par kOm o ra Ethnobotanical P ar k is a  prot ected area of  Chile loc a t e d  westof P u er t o Williams onNavar ino Island in the e xtrem e southe rn Magell a n  and Chi lea n A nta rct i c aRegion. The O m o ra P ar k is ares earch,edu cat ion  an dconservat ion cent er  f or  t heCapeH orn Bios ph ere  R ese rve.T he par k its elfin cl u des  a repr e se n t ativ eva riet y s ub antar ctic flo ra open  to the p ubl i c fo rfo rmal an d information  e ducation.Wi thi n itsb o undaries , one can find deciduou s  forest s ( Notho fagu s antarct ica  and N oth o faguspumili o) an deve r g reenb r oa dle af  forests ( N o tho fagus  b etul oides),  as well as bogs a n d h igh-Andean ec osy stem s an d d i ve r semo s ses , lichens and liv erworts (t er m ed  the "Mini a tur eForests  of Cap e Hor n " by Om ora Parkscientist s) .

S i n ceits creati on in 20 00, the O m ora P a rk  andits  partn er s a nd co lleagu e s h ave g one on  t o lead  a tr an sdiscipl inary biocultural conse rvatio n ini tia tive that  le d  to  the crea tion  of the Ca peHor n Bio sph e re Re serv e .A c o nsort iumo f institu t io nsn o wsupport thi s p rog ram i ncl u ding t he O mora Foundation,t he MillenniumInst i t ute  of Ecol og y and Biodiver sit y( I EB-Chile )a nd the Univ ersity o fM agall anes i n Chil e, andt h eU nivers ityofNorth Tex asan d  the Ce nt er for En viro nm entalPhilos o phyi n  the United Stat es. I n 2008, the  Omor aPark re c eive d the "Sci ence and Pr actice  ofEcolo gy andSo cietyAwa rd ", given b y  the Foun datio n for S ci enti fic  Synth esis . 
Foun ding  d ire ctor
 sheet_into distinct_blocks (which does not_happen during_rafting)._The reason_why_breaking happens is_that, as the_ice thickness increases, the_bending moment exerted_on_the upper surface of the ice exceeds its tensile strength. In other words, the_ice_is no_longer_flexible_enough to withstand the overthrust_event without breaking.

Maximum thickness for_rafting 
A_theoretical formula has been used to estimate the_maximum_thickness an ice_sheet can have in order to be able to_raft. This thickness () is

where _is Poisson's ratio,__is_the tensile strength of_the ice,  is water density,_Y is the Young's modulus of_sea ice and g is the gravitational_acceleration. What this equation shows is_that, assuming a representative tensile_strength of_0.65 MPa, the maximum thickness_for rafting to_occur is_in the range_of.

See also 
 Lead (sea ice)
_Pressure ridge (ice)

Notes

References

Category:Sea_ice Omora Ethnobotanical Park

Omora Ethnobotanical Park_is_a protected area_of_Chile_located _west of Puerto_Williams_on Navarino_Island_in the extreme southern Magellan and_Chilean_Antarctica Region. The Omora Park is a_research, education and conservation_center_for the Cape Horn_Biosphere Reserve. The park itself_includes a representative variety subantarctic flora_open to_the public_for formal and information education. Within its boundaries, one can find_deciduous forests (Nothofagus antarctica and Nothofagus_pumilio) and evergreen broadleaf_forests (Nothofagus_betuloides),_as well as_bogs_and high-Andean_ecosystems and diverse mosses, lichens and liverworts_(termed the_"Miniature Forests of Cape Horn" by_Omora Park scientists).

Since its_creation_in 2000, the Omora Park and_its partners and colleagues have gone_on to lead a transdisciplinary_biocultural_conservation_initiative that led to the_creation of the Cape Horn Biosphere_Reserve. A consortium_of institutions now support this program including_the_Omora Foundation, the Millennium Institute of_Ecology_and Biodiversity (IEB-Chile)and the University of_Magallanes_in_Chile, and the University of_North Texas and the Center for_Environmental Philosophy in the United States. In 2008, the_Omora Park received_the "Science and Practice of_Ecology_and_Society Award", given by the Foundation for Scientific Synthesis.

Founding director