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كويز تفاعلي: اختبار العلوم انسباير الصف السابع لدرس Moving Continents
تتناول هذه المجموعة من الأسئلة نظرية الانجراف القاري التي اقترحها العالم ألفريد فيجنر، والتي تفترض أن القارات كانت مجتمعة في قارة واحدة عملاقة تسمى بانجيا (Pangaea). يستعرض الاختبار الأدلة العلمية المختلفة التي دعمت هذه الفرضية، بما في ذلك التطابق الهندسي بين حواف القارات مثل أفريقيا وأمريكا الجنوبية، والأدلة الأحفورية مثل بقايا نبات الجلوسوبتريس وزاحف الميسوصور، بالإضافة إلى الأدلة المناخية المتمثلة في رواسب الفحم في القارة القطبية الجنوبية والخدوش الجليدية في المناطق المدارية الحالية. كما يسلط الضوء على التحديات التي واجهت النظرية في بدايتها بسبب غياب تفسير لآلية حركة القارات، وكيف تم اكتشاف الأدلة الحاسمة لاحقاً في قاع المحيطات.
رقم الاختبار1117
الصفالسابع
المادةعلوم
الفصلالفصل الثالث
السنة الدراسية2025-2026
عدد الأسئلة10
إجمالي النقاط10
تاريخ الإضافة2026-04-29
الزيارات261
الناشرMaya Dayoub
يرجى الانتباه إلى أن المعلم قام بإعداد الأسئلة فقط، ولم يقم بإعداد الإجابات أو الشروحات المرفقة. وقد تم توليد الإجابات باستخدام تقنيات الذكاء الاصطناعي، لذلك قد تتضمن بعض الأخطاء أو عدم الدقة.
للحصول على الإجابات الصحيحة والمضمونة، يُرجى الرجوع إلى المعلم أو المصدر الدراسي المعتمد.
Question 1
Points: 1
What was the name of the single supercontinent that Alfred Wegener proposed existed hundreds of millions of years ago?
Alfred Wegener proposed that all continents were once joined in a single supercontinent called Pangaea, which began to break apart about 200 million years ago.
Question 2
Points: 1
Which two continents were most notably cited by mapmakers and Wegener for their "jigsaw-puzzle" fit?
The western coastline of Africa and the eastern coastline of South America appear to fit together like pieces of a jigsaw puzzle, providing early evidence for continental drift.
Question 3
Points: 1
What did Wegener use as climate-based evidence for continental drift after finding them in Antarctica?
Coal is formed from ancient swamp plants that grow in warm, wet climates; finding coal deposits in Antarctica suggests that the continent was once located much closer to the equator.
Question 4
Points: 1
Which fossilized plant was found on several widely separated continents, suggesting they once shared a temperate climate?
Explanation
Glossopteris fossils were discovered on many continents that are now separated by oceans, indicating these landmasses were once connected and shared a similar climate.
Question 5
Points: 1
Why did Wegener believe that the reptile Mesosaurus provided evidence for continental drift?
Since Mesosaurus lived in fresh water and could not have survived a journey across the salty Atlantic Ocean, finding its fossils in both South America and Africa suggests the continents were joined.
Question 6
Points: 1
What evidence did Wegener find in 290-million-year-old rocks in South America, Africa, India, and Australia?
Glacial grooves found in rocks of continents that are now warm indicate that these areas were once covered by glaciers and were likely located near the South Pole.
Question 7
Points: 1
Regarding rock formations, what did geologists discover about volcanic eruptions on the western coast of Africa and the eastern coast of South America?
Explanation
Geologists found that volcanic rocks on both sides of the Atlantic Ocean match perfectly in chemical composition and age, implying they were part of the same formation before the continents split.
Question 8
Points: 1
What are the names of the two giant landmasses that Pangaea initially broke into?
Explanation
As Pangaea began to break up, it initially split into two smaller supercontinents: Laurasia in the north and Gondwana in the south.
Question 9
Points: 1
Why were many scientists initially skeptical of Wegener’s Continental Drift hypothesis?
Although Wegener provided significant evidence for continental drift, he was unable to identify a physical force or mechanism capable of pushing large continents across the Earth.
Question 10
Points: 1
Where was the scientific evidence "hidden" that eventually helped prove Wegener's hypothesis long after his death?
Decades later, mapping of the seafloor revealed mid-ocean ridges and seafloor spreading, which provided the evidence for how continents move, supporting Wegener's original ideas.
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