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ANTARCTIC EXPLORATION COMPANY

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NEW DISCOVERIES IN THE ANTARCTICA

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The polar expedition under Robert Kohler discovered the soil of an ancient sea at a depth of 2000 meters in Antarctica. By means of a radar, polar researchers from four different countries will be developing an ice chart of one of the last unexplored areas of the continent. This area borders directly on the Weddell Sea (West Antarctica). According to preliminary calculations, a basin is situated there, which is as big as a small country in Europe (an area of about 20 thousand square kilometers). At some points it reaches a depth of about 2 kilometers. The researchers came to the conclusion that in this area there once used to be a sea that extended up to 200 kilometers into the interior of the modern continent. This theory is supported by the rock composition of the subglacial basin surface (these rocks are marine deposits) detected by the radars and by the relief of the pool wall, which was “removed” from the ocean and which was once part of the same maritime coastline as the fjords. If, according to the scientists, the giant ice shelf, which slows down the flow of ice masses, were to dissolve quickly the ice that currently “rests” in the basin, will “slip off” into the sea and melt quickly, thus causing a significant sea-level rise.

Author’s photo of the expedition participant Stefan Kraus. Follow the author’s Instagram account to learn more about the life of polar researchers: www.instagram.com/polarstefan/

https://www.instagram.com/polarstefan

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AQUILIO EXPEDITION TEAM MEMBERS

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ANTARKTISCHE  EXPLORATIONSUNTERNEHMEN

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NEUE ENTDECKUNGEN IN DER ANTARKTIS

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Die Polarexpedition unter der Leitung von Robert Kohler entdeckte in der Antarktis in der Tiefe von 2000 Metern den Boden eines antiken Meeres. Polarforscher aus vier verschiedenen Ländern werden mit Hilfe des Radars eine Eiskarte für eines der letzten unerforschten Gebiete des Kontinents erstellen. Es grenzt direkt an das Weddellmeer (Westantarktis). Nach vorläufigen Berechnungen ist dort ein Becken so groß wie ein kleines Land in Europa (eine Fläche von etwa 20 Tausend Quadratkilometern) versteckt. Es erreicht an einigen Stellen bis etwa 2 Kilometer Tiefe. Die Forscher kamen zu einem Schluss, dass sich in diesem Bereich einst ein Meer befinden musste, das sich bis 200 Kilometer ins Innere des modernen Kontinents erstreckte. Dafür spricht vor allem die per Radar erfasste Gesteinszusammensetzung der Meeresablagerungen des subglazialen Beckens und das Relief der vom Ozean “entfernten” Beckenwand, die einst eine Meeresküste mit Fjorden darstellte. Soll nach Ansicht der Wissenschaftler das riesige Eismassen-bremsende Eisschelf  sich schnell auflösen, wird das Eis, das sich in diesem Becken ruht, ins Meer abrutschen, intensiv abschmelzen und somit einen deutlichen Meeresspiegelanstieg verursachen.

Autorenfoto von Stefan Kraus, des Expeditionsteilnehmers.

Wer mehr über das Leben der Polarforscher erfahren möchte, findet weitere Episoden auf seiner Instagram-Seite: https://www.instagram.com/polarstefan

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 AQUILIO EXPEDITIONTEILNEHMER

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COMPAGNIE D’EXPLORATION ANTARCTIQUE

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L’expédition polaire internationale menée par le scientifique Robert Kohler a découvert d’anciens fonds marins à une profondeur de 2000 mètres sous l’Antarctique. Au moyen d’un radar, les chercheurs polaires de quatre pays différents cartographient les glaces de l’une des dernières zones inexplorées du continent, qui borde directement la mer de Weddell (Antarctique occidental). D’après les premiers calculs, il s’agit d’un bassin de la superficie d’un petit pays européen (environ 20.000 kilomètres carrés). À certains endroits, il atteint environ 2 kilomètres de profondeur. Les chercheurs sont arrivés à la conclusion que cette zone était autrefois occupée par une mer qui s’étendait jusqu’à 200 kilomètres à l’intérieur du continent actuel. Cette théorie est étayée par la composition rocheuse de la surface du bassin sous-glaciaire (constituée de sédiments marins) et par le relief de la paroi qui séparait autrefois cette mer de l’océan. Selon les scientifiques, si la fonte de la calotte glacière, qui ralentit l’écoulement des glaces dans les océans, venait à s’accélérer, la glace sur laquelle elle repose dans le bassin pourrait glisser dans l’océan et fondre très rapidement, provoquant ainsi une élévation significative du niveau de la mer.

Photo prise par Stefan Kraus, membre de l’expédition. Suivez son compte Instagram pour en savoir plus sur la vie des chercheurs polaires : www.instagram.com/polarstefan/

https://www.instagram.com/polarstefan

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MEMBRES DE L’EXPÉDITION AQUILO

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ПОЛЯРНАЯ СТАНЦИЯ “АКВИЛОН”

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Антарктида: новости и открытия

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Полярная экспедиция под руководством Роберта Ланге обнаружила в толще льда грунт, по всей вероятности, являющийся дном древнего моря. Исследователи из четырёх разных стран примут участие в создании ледовой карты одной из последних неизученных областей континента. Участок с обнаруженным морем непосредственно граничит с морем Уэдделла (запад Антарктиды). Согласно предварительным подсчётам, котловина по размеру сравнима с небольшой европейской страной (примерно 20 тысяч квадратных километров). В некоторых местах её глубина достигает двух километров. Исследователи пришли к выводу, что располагавшееся на данной территории море уходило вглубь современной Антарктиды на расстояние до 200 километров. Данную теорию подтверждает строение скальной породы с поверхности котловины подо льдом (представляющую собой морские отложения). При изъятии боковой стенки бассейна, «удалённой» из океана, оказалось, что она некогда представляла собой часть той же береговой линии, что и антарктические фьорды. Если, по словам учёных, этот гигантский шельфовый ледник, замедляющий течение ледовых масс, стремительно растворится, то весь лёд, который в данный момент находится в бассейне, «соскользнёт» в море и быстро растает, тем самым существенно подняв уровень мирового океана. Ведущиеся в настоящее время исследования включают в себя разработки по купированию влияния глобального потепления на льды Южного и Северного полюсов, чтобы эта гипотетическая ситуация не стала угрожающей реальностью для всего побережья Южной Америки.

Снимок сделан участником экспедиции Штефаном Ленцем. Чтобы узнать больше о жизни полярных исследователей, подписывайтесь на автора в Instagram: @polarpenguinstefan

 

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ЭКСПЕДИЦИОННАЯ КОМАНДА СТАНЦИИ «АКВИЛОН»

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border_color=”#ffffff” border_style=”solid”]США, Великобритания[/et_pb_team_member][/et_pb_column][et_pb_column type=”1_4″ _builder_version=”3.25″ custom_padding=”|||” custom_css_main_element=”position: relative;||” custom_padding__hover=”|||”][et_pb_team_member name=”Штефан Ленц” position=”Повар” image_url=”https://pole-explorer.org/wp-content/uploads/2018/10/kraus-2.jpg” admin_label=”Person” _builder_version=”4.7.6″ header_font=”|on|||” background_size=”initial” background_position=”top_left” background_repeat=”repeat” custom_padding=”20px|20px|20px|20px” custom_css_member_image=”border-radius: 200px;||overflow: hidden;||margin-top: 10px;||box-shadow: 0 0 20px rgba(0,0,0,.1);||border: 2px solid #fff;||max-height: 200px;||max-width: 200px;||” use_border_color=”off” border_color=”#ffffff” border_style=”solid”]США, Германия[/et_pb_team_member][/et_pb_column][et_pb_column type=”1_4″ _builder_version=”3.25″ custom_padding=”|||” custom_css_main_element=”position: relative;||” custom_padding__hover=”|||”][et_pb_team_member name=”Мария Масиас Прадо” position=”Медицинский работник” image_url=”https://pole-explorer.org/wp-content/uploads/2018/10/maria.jpg” admin_label=”Person” _builder_version=”4.7.6″ header_font=”|on|||” background_size=”initial” background_position=”top_left” background_repeat=”repeat” custom_padding=”20px|20px|20px|20px” custom_css_member_image=”border-radius: 200px;||overflow: hidden;||margin-top: 10px;||box-shadow: 0 0 20px rgba(0,0,0,.1);||border: 2px solid #fff;||max-height: 200px;||max-width: 200px;||” use_border_color=”off” border_color=”#ffffff” border_style=”solid”]Чили[/et_pb_team_member][/et_pb_column][et_pb_column type=”1_4″ _builder_version=”3.25″ custom_padding=”|||” custom_css_main_element=”position: relative;||” custom_padding__hover=”|||”][et_pb_team_member name=”Рауль Охедо Толедо” position=”Механик” image_url=”https://pole-explorer.org/wp-content/uploads/2018/10/raul-2.jpg” admin_label=”Person” _builder_version=”4.7.6″ header_font=”|on|||” background_size=”initial” background_position=”top_left” background_repeat=”repeat” custom_padding=”20px|20px|20px|20px” custom_css_member_image=”border-radius: 200px;||overflow: hidden;||margin-top: 10px;||box-shadow: 0 0 20px rgba(0,0,0,.1);||border: 2px solid #fff;||max-height: 200px;||max-width: 200px;||” use_border_color=”off” border_color=”#ffffff” border_style=”solid”]Чили[/et_pb_team_member][/et_pb_column][/et_pb_row][et_pb_row column_structure=”1_4,1_4,1_4,1_4″ make_equal=”on” admin_label=”Row” _builder_version=”3.25″ background_size=”initial” background_position=”top_left” background_repeat=”repeat” make_fullwidth=”off” use_custom_width=”off” width_unit=”on”][et_pb_column type=”1_4″ _builder_version=”3.25″ custom_padding=”|||” custom_css_main_element=”position: relative;” custom_padding__hover=”|||”][et_pb_team_member name=”Томас Грубер” position=”Биолог” image_url=”https://pole-explorer.org/wp-content/uploads/2018/10/thomas-schneider-2.jpg” 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custom_css_member_image=”border-radius: 200px;||overflow: hidden;||margin-top: 10px;||box-shadow: 0 0 20px rgba(0,0,0,.1);||border: 2px solid #fff;||max-height: 200px;||max-width: 200px;||” use_border_color=”off” border_color=”#ffffff” border_style=”solid”]Австралия[/et_pb_team_member][/et_pb_column][et_pb_column type=”1_4″ _builder_version=”3.25″ custom_padding=”|||” custom_css_main_element=”position: relative;” custom_padding__hover=”|||”][et_pb_team_member name=”Лео Нойман” position=”Гляциолог” image_url=”https://pole-explorer.org/wp-content/uploads/2018/10/klaus-neumann-2.jpg” admin_label=”Person” _builder_version=”4.7.6″ header_font=”|on|||” background_size=”initial” background_position=”top_left” background_repeat=”repeat” custom_padding=”20px|20px|20px|20px” hover_enabled=”0″ custom_css_member_image=”border-radius: 200px;||overflow: hidden;||margin-top: 10px;||box-shadow: 0 0 20px rgba(0,0,0,.1);||border: 2px solid #fff;||max-height: 200px;||max-width: 200px;||” 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