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        "date_updated":"2025-11-03T09:04:36.109000",
        "title_en":"Krossfjorden",
        "title_no":"Krossfjorden",
        "description_en":"<p>When sailing from west to Krossfjorden, course must be held well clear of the shallow area south of Kapp Mitra, with special attention given to the rock awash, Kroneflua, which is located approximately 1.4 NM south of the nearest land between Cape Mitra and Collinsodden.</p>\n<p>A good 1.5 NM west-southwest from this is Kronegrunnen, 9 m, just 2 NM from shore. To go clear south of the shoal area vessels are sailed on&nbsp;<em>the line Blomstrandsalen&nbsp;under the most southerly of Tre Kroner</em>, bearing 116&ordm;-296&ordm; (the saddle is the hollow between the two peaks of Blomstrandhalv&oslash;ya. Vessels are clear of the shoal area on the east side and can sail into Krossfjorden when&nbsp;<em>the southeast point of Kong Haakons peninsula appears over the beach on </em><em>Mitrahalv&oslash;ya</em>, bearing 036&deg; - 216&deg;.</p>\n<p>It is mainly deep close inshore in towards Krossfjorden with&nbsp;steeply sloping seabed.</p>\n<p>Approximately 4 NM inwards from Kapp Guissez on the eastern side lies Fjortende Julibukta, well sheltered from the wind that sets out Krossfjorden. Depth is 10.4 meters in the middle of the entrance. Fjortende Julibreen is a beautiful glacier that calves occasionally, but there is no significant current in the bay, so it is not a major problem.</p>\n<p>On the opposite side of the fjord lies Ebeltofthamna. Approximately in the middle of the entrance, there is a rock awash. The innermost part of the bay is also rocky along the shore and has only 2 m depth in the middle.</p>\n<p>Further inwards, the fjord splits into two fjord arms, divided by the peninsula Kong Haakons Halv&oslash;y and the mountain Kongshammaren (583) at the southern end.</p>",
        "description_no":"<p>Under innseilingen fra W til Krossfjorden, m&aring; man holde&nbsp;godt klar av grunnflaket S av Kapp Mitra, spesielt med tanke&nbsp;p&aring; skvalpeskj&aelig;ret Kroneflua som ligger ca. 1.4 n mil S for n&aelig;rmeste land mellom Kapp Mitra og Collinsodden.</p>\n<p>Vel 1.5 n mil WSW av denne ligger Kronegrunnen, 9 m, knapt 2 n mil av land. For &aring; g&aring; fri S om grunnomr&aring;det kan man seile i medet&nbsp;<em>Blomstrandsalen under S-ligste Tre Kroner</em>,&nbsp;rettvisende 116&deg;-296&deg; (Salen er fordypningen mellom de to toppene&nbsp;p&aring; Blomstrandhalv&oslash;ya.&nbsp;Man er klar grunnomr&aring;det p&aring; E-siden og kan seile inn Krossfjorden n&aring;r&nbsp;<em>SE-odden av Kong Haakons Halv&oslash;y ses over stranden p&aring; Mitrahalv&oslash;ya</em>,&nbsp;rettvisende 036&deg;-216&deg;.</p>\n<p>Stort sett er det dypt kloss i land innover i Krossfjorden med&nbsp;sterkt avfallende bunn.</p>\n<p>Ca. 4 n mil innover fra Kapp Guissez p&aring; &oslash;stsiden ligger Fjortende Julibukta, godt skjermet for vinden som setter ut Krossfjorden. Dybde p&aring; 10.4 m midt i innl&oslash;pet. Fjortende Julibreen er en fin isbre som kalver av og til, men det er ikke noe str&oslash;m av betydning i bukta s&aring; det er ikke noe stort problem.</p>\n<p>P&aring; motsatt side av fjorden igger Ebeltofthamna. Omtrent midt i innl&oslash;pet ligger det et skvalpeskj&aelig;r. Den innerste delen av bukta er ogs&aring; steinet langs&nbsp;land og med kun 2 m dybde midt utp&aring;.</p>\n<p>Videre innover deler fjorden seg, og g&aring;r over i to fjordarmer, delt av Kong Haakons Halv&oslash;y og fjellet Kongshammaren (583 moh) helt s&oslash;r p&aring; halv&oslash;ya.</p>",
        "caution_en":"<h3>Survey data</h3>\n<p>Surveys are incomplete in the area. Soundings within unsurveyed areas and those compiled from incomplete older surveys are unreliable and do not fully exclude undiscovered shoals. Navigation within these waters &nbsp;should be avoided whenever possible. Attention should be paid to the Source Diagram.</p>\n<h3>Shallow areas near shoreline</h3>\n<p>Close to the shore, there can be unsurveyed areas or areas of poor data quality. Due to the chart's scale such areas are not always visible on nautical Charts. Navigation in these waters must be exercised with extreme caution.</p>\n<h3>Front of glaciers</h3>\n<p>Limits of glaciers are subject to frequent change. In front of glaciers going into the sea, there are major &nbsp;variations from year to year, and depths are uncertain. Such areas must be considered as unsurveyed. Such &nbsp;conditions must be taken into account when navigating in these waters and caution exercised.</p>",
        "caution_no":"<p><strong>Sj&oslash;m&aring;lingsdata</strong></p>\n<p>Omr&aring;det er ikke fullstendig oppm&aring;lt. Dybder innenfor ikke sj&oslash;m&aring;lte omr&aring;der og omr&aring;der basert p&aring; eldre, ufullstendige m&aring;linger er up&aring;litelige, og utelukker ikke muligheten for uoppdagede grunner. Navigasjon i disse farvannene b&oslash;r unng&aring;s s&aring; langt det lar seg gj&oslash;re. Det m&aring; vises s&aelig;rlig oppmerksomhet til karets kildediagram (Source Diagram).</p>\n<p><strong>Grunne omr&aring;der n&aelig;r land</strong></p>\n<p>N&aelig;r kystlinjen kan det forekomme ikke sj&oslash;m&aring;lte omr&aring;der eller omr&aring;der med d&aring;rlig datakvalitet. P&aring; grunn av sj&oslash;kartets m&aring;lestokk er slike omr&aring;der ikke alltid synlige. Navigasjon i disse farvannene m&aring; ut&oslash;ves med ekstrem forsiktighet.</p>\n<p><strong>Foran isbreer</strong></p>\n<p>Isbreers utbredelse endres hyppig. Foran breer som munner ut i sj&oslash;en forekommer store variasjoner fra &aring;r til &aring;r, og dybdeforholdene er usikre. Slike omr&aring;der m&aring; betraktes som ikke sj&oslash;m&aring;lte. Disse forholdene m&aring; tas i betraktning ved navigasjon, og forsiktighet m&aring; utvises.</p>"
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