ภาพ space นี้ ควรจะถูกสร้างใหม่เป็นกราฟิกส์เวกเตอร์ ซึ่งมีข้อดีอีกหลายประการ ดูเพิ่มเติมที่คอมมอนส์:สื่อต้องการเก็บกวาดสำหรับสารสนเทศเพิ่มเติม หากภาพนี้มีในรูปแบบกราฟิกส์เวกเตอร์อยู่แล้ว กรุณาอัปโหลดและแทนที่แม่แบบนี้ด้วย {{vector version available|ชื่อภาพใหม่}} แนะนำเป็นอย่างยิ่งให้ตั้งชื่อไฟล์เวกเตอร์ใหม่นั้นในรูปแบบ "Terrestial Planets internal en.svg" แล้วใส่แม่แบบ Vector version available (หรือ Vva) ซึ่งไม่ต้องใช้พารามิเตอร์ ชื่อภาพใหม่
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ความย่อ
คำอธิบายTerrestial Planets internal en.jpg
English: Mercury has an average density of 5430 kilograms per cubic meter, which is second only to Earth among all the planets. It is estimated that the planet Mercury, like Earth, has a ferrous core with a size equivalent to two-thirds to three-fourths that of the planet's overall radius. The core is believed to be composed of an iron-nickel alloy covered by a mantle and surface crust.
It is believed that the composition of the planet Venus is similar to that of Earth. The planet crust extends to around 10-30 kilometers below the surface, under which the mantle reaches to a depth of some 3000 kilometers. The planet core comprises a liquid iron-nickel alloy. Average planet density is 5240 kilograms per cubic meter.
The Earth comprises three separate layers: a crust, a mantle, and a core (in descending order from the surface). The crust thickness averages 30 kilometers for land masses and 5 kilometers for seabeds. The mantle extends from just below the crust to some 2900 kilometers deep. The core below the mantle begins at a depth of around 5100 kilometers, and comprises an outer core (liquid iron-nickel alloy) and inner core (solid iron-nickel alloy). The crust is composed mainly of granite in the case of land masses and basalt in the case of seabeds. The mantle is composed primarily of peridotite and high-pressure minerals. Average planet density is 5520 kilograms per cubic meter.
Mars is roughly one-half the diameter of Earth. Due to its small size, it is believed that the martian center has cooled. Geological structure is mainly rock and metal. The mantle below the crust comprises iron-oxide-rich silicate. The core is made up of an iron-nickel alloy and iron sulfide. Average planet density is 3930 kilograms per cubic meter.
The structure of Pluto is not very well understood at present. Nevertheless, spectroscopic observation from Earth in the 1970s has revealed that the planet surface is covered with methane ice. Surface temperature is -230?C (-382?F), and the frozen methane exhibits a bright coloration. However, with the exception of the polar caps, the frozen methane surface is seen to change to a dark red when eclipsed by its moon Charon. Average planet density is 2060 kilograms per cubic meter. The low average density requires that the planet must be a mix of ice and rock.
ไฟล, terrestial, planets, internal, ไฟล, ประว, ไฟล, หน, าท, ภาพน, การใช, ไฟล, วนกลาง, อม, ลเก, ยวก, บภาพขนาดของต, วอย, างน, กเซล, ความละเอ, ยดอ, กเซล, กเซล, กเซล, กเซล, ภาพท, ความละเอ, ยดส, งกว, 8206, กเซล, ขนาดไฟล, โลไบต, ชน, ดไมม, image, jpeg, ปภาพหร, อไฟล, . ifl prawtiifl hnathimiphaphni karichiflswnklang khxmulekiywkbphaphkhnadkhxngtwxyangni 799 213 phikesl khwamlaexiydxun 320 85 phikesl 640 171 phikesl 1 024 273 phikesl 3 373 900 phikesl duphaphthimikhwamlaexiydsungkwa 8206 3 373 900 phikesl khnadifl 691 kiolibt chnidimm image jpeg rupphaphhruxiflesiyngni tnchbbxyuthi khxmmxns raylaexiyddanlang epnkhxkhwamthiaesdngphlcak ifltnchbbinkhxmmxns khxmmxnsepnewbistinokhrngkarsahrbekbrwbrwmsuxesri thi khunsamarthchwyid phaph space ni khwrcathuksrangihmepnkrafiksewketxr sungmikhxdixikhlayprakar duephimetimthikhxmmxns suxtxngkarekbkwadsahrbsarsnethsephimetim hakphaphnimiinrupaebbkrafiksewketxrxyuaelw krunaxpohldaelaaethnthiaemaebbnidwy vector version available i chuxphaphihm i aenanaepnxyangyingihtngchuxiflewketxrihmnninrupaebb Terrestial Planets internal en svg aelwisaemaebb Vector version available hrux Vva sungimtxngichpharamietxr chuxphaphihmThis space image was uploaded in the JPEG format even though it consists of non photographic data This information could be stored more efficiently or accurately in the PNG or SVG format If possible please upload a PNG or SVG version of this image without compression artifacts derived from a non JPEG source or with existing artifacts removed After doing so please tag the JPEG version with Superseded NewImage ext and remove this tag This tag should not be applied to photographs or scans For more information see BadJPEG khwamyx khaxthibayTerrestial Planets internal en jpg English Mercury has an average density of 5430 kilograms per cubic meter which is second only to Earth among all the planets It is estimated that the planet Mercury like Earth has a ferrous core with a size equivalent to two thirds to three fourths that of the planet s overall radius The core is believed to be composed of an iron nickel alloy covered by a mantle and surface crust It is believed that the composition of the planet Venus is similar to that of Earth The planet crust extends to around 10 30 kilometers below the surface under which the mantle reaches to a depth of some 3000 kilometers The planet core comprises a liquid iron nickel alloy Average planet density is 5240 kilograms per cubic meter The Earth comprises three separate layers a crust a mantle and a core in descending order from the surface The crust thickness averages 30 kilometers for land masses and 5 kilometers for seabeds The mantle extends from just below the crust to some 2900 kilometers deep The core below the mantle begins at a depth of around 5100 kilometers and comprises an outer core liquid iron nickel alloy and inner core solid iron nickel alloy The crust is composed mainly of granite in the case of land masses and basalt in the case of seabeds The mantle is composed primarily of peridotite and high pressure minerals Average planet density is 5520 kilograms per cubic meter Mars is roughly one half the diameter of Earth Due to its small size it is believed that the martian center has cooled Geological structure is mainly rock and metal The mantle below the crust comprises iron oxide rich silicate The core is made up of an iron nickel alloy and iron sulfide Average planet density is 3930 kilograms per cubic meter The structure of Pluto is not very well understood at present Nevertheless spectroscopic observation from Earth in the 1970s has revealed that the planet surface is covered with methane ice Surface temperature is 230 C 382 F and the frozen methane exhibits a bright coloration However with the exception of the polar caps the frozen methane surface is seen to change to a dark red when eclipsed by its moon Charon Average planet density is 2060 kilograms per cubic meter The low average density requires that the planet must be a mix of ice and rock wnthi 13 singhakhm ph s 2556 15 57 44aehlngthima http solarsystem nasa gov multimedia display cfm IM ID 168phusrangsrrkh NASA karxnuyatichsiththi Public domain Public domain false falsephaphniepnsatharnsmbti enuxngcakepnphaphthisrangkhunodyxngkhkarbriharkarbinaelaxwkasaehngchati NASA sungtamnoybaydanlikhsiththikhxngnasarabuiwwa phaphaelasuxtang khxngnasaimidrbkarkhumkhrxngodylikhsiththiykewncarabuiwwamilikhsiththi duephimthi hnanoybaydanlikhsiththikhxngnasa hrux noybaykarichphaphkhxng JPLkhaetuxn karich olokkhxngnasa ekhruxnghmayaelaekhruxngpradbkhxngnasa thukcakddwykdhmayshrthxemrikainlksna 14 khxngkhxbngkhbthangrachkarshrthxemrika swnthi 1221 ewbistkhxngnasaekbrwbrwmphaphthimacakxngkhkarxwkasosewiyt xngkhkarxwkasaehngchatirsesiy aelaxngkhkarxwkasthimiichxngkhkarxwkaskhxngshrthxemrika epncanwnmak phaphehlaniimcaepntxngepnsatharnsmbtiesmxip phaphhruxsuxthimacak klxngothrthrrsnxwkashbebil xacmilikhsiththi hakphaphhruxsuxnnimidrabuchdecnwamacak sthabnwithyasastrklxngothrthrrsnxwkas 1 phaphhruxsuxthnghmdthimacakekhruxngmuxkhxng okhrngkarsuksadwngxathityaelalmsuriya milikhsiththi karnaphaphhruxsuxcakokhrngkaripichnxkehnuxcakkarichephuxkarkhahruxephuxkarsuksa txngidrbxnuyatkxn 2 phaphthithukkhdeluxkihepn phaphdarasastrpracawn APOD bnewbistkhxng APOD xacmilikhsiththi 3 Derivative works iflxunthiichiflni Terrestial Planets internal ru jpgkhabrryayodyyxithyephimkhabrryaythrrthdediywephuxkhyaykhwamwaiflnimixairixethmthiaesdngxyuiniflniprakxbdwywnthisrang wnkxtng13 singhakhm 2013 prawtiifl khlikwnthi ewlaephuxduiflthipraktinkhnann wnthi ewlarupyxkhnadphuichkhwamehn pccubn06 01 15 mithunayn 25483 373 900 691 kiolibt Dbenbennoriginal 3373x900 version from http sse jpl nasa gov multimedia gallery terrest int jpg 05 15 15 mithunayn 25482 361 630 364 kiolibt Sig11The internal structure of the inner planets Source http sse jpl nasa gov multimedia display cfm IM ID 168 PD USGov NASA Category Solar system hnathimiphaphni hnatxipni oyngmathiphaphni aekndaw karichiflswnklang wikixuntxipniichiflni karichbn ar wikipedia org نواة كوكب karichbn bn wikipedia org অগ ন য ৎপ ত karichbn br wikipedia org Derc henn planedenn karichbn ca wikipedia org Nucli planetari Evolucio mineral karichbn cs wikipedia org Planetarni jadro Planetarni plast karichbn cv wikipedia org Planeta tĕshĕ karichbn el wikipedia org Planhtikos pyrhnas karichbn en wikipedia org Volcanism Planetary core User Dudekahedron sandbox User Lesturn sandbox Volcanism Mineral evolution User PriscillaAguiar sandbox karichbn es wikipedia org Planeta interior Nucleo geologia Vulcanismo Evolucion mineral karichbn eu wikipedia org Nukleo geologia karichbn fa wikipedia org هسته سیاره karichbn gl wikipedia org Planeta interior Terraformacion Nucleo xeoloxia karichbn hi wikipedia org ग रह य क र ड karichbn hr wikipedia org Planetna jezgra karichbn hu wikipedia org Bolygomag karichbn hy wikipedia org Վուլկանիզմ Մասնակից Liana Yeghyan Ավազարկղ2 Մոլորակային միջուկ karichbn 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https th wikipedia org wiki ifl Terrestial Planets internal en jpg, wikipedia, วิกิ หนังสือ, หนังสือ, ห้องสมุด,
