Warning: foreach() argument must be of type array|object, bool given in /var/www/html/web/app/themes/studypress-core-theme/template-parts/header/mobile-offcanvas.php on line 20

Choose the best answer to each of the following. Explain your reasoning with one or more complete sentences. Earth's oceans formed (a) during the late stages of accretion as water ice collected on the surface; (b) from water vapor outgassed by volcanoes; (c) when Earth underwent differentiation.

Short Answer

Expert verified
The best answer is (b), as oceans mainly formed from volcanic outgassing.

Step by step solution

01

Understanding the Question

The question asks us to determine when the Earth's oceans were formed, and provides three different choices, each referring to a possible process or stage of Earth's formation and development.
02

Analyzing Option A

Option (a) suggests that oceans formed during the late stages of accretion as water ice collected on the surface. During accretion, Earth was still forming from debris and particles, and water ice could indeed have collected on the surface after the planet cooled down enough.
03

Analyzing Option B

Option (b) claims that Earth's oceans formed from water vapor outgassed by volcanoes. This means water vapor released by volcanic activity condensed to form liquid water as the Earth cooled, which is a significant and widely accepted theory explaining ocean formation.
04

Analyzing Option C

Option (c) states that oceans formed when Earth underwent differentiation. Differentiation is the process by which Earth separated into layers based on density but does not specifically refer to ocean formation, making it less likely to be correct.
05

Selecting the Best Answer

Comparing the explanations, option (b) aligns well with the scientific consensus that volcanic outgassing significantly contributed to ocean formation, making it the most appropriate choice.

Unlock Step-by-Step Solutions & Ace Your Exams!

  • Full Textbook Solutions

    Get detailed explanations and key concepts

  • Unlimited Al creation

    Al flashcards, explanations, exams and more...

  • Ads-free access

    To over 500 millions flashcards

  • Money-back guarantee

    We refund you if you fail your exam.

Over 30 million students worldwide already upgrade their learning with Vaia!

Key Concepts

These are the key concepts you need to understand to accurately answer the question.

Accretion Phase
The accretion phase was one of the earliest stages in Earth's formation. During this phase, small particles collided and stuck together, gradually forming larger planetary bodies. This process took place over millions of years. The Earth at this time was a hot, molten mass undergoing intense bombardment from space debris. As the collisions decreased and the Earth started to cool, water ice could have been delivered to Earth by icy bodies such as comets and asteroids. These impacts would have provided the raw ingredients necessary for water to eventually accumulate on the Earth's surface.
This phase is crucial because it set the stage for Earth's initial water supply, though the water might not have directly formed oceans yet. Instead, the materials collected during the accretion phase provided a foundation that later processes would build upon.
- The accretion phase involved the gathering of particles to form planets. - It ended with the Earth as a molten body that slowly cooled, allowing for water solidification. - Icy bodies from space contributed to Earth's water inventory during this phase.
Volcanic Outgassing
Volcanic outgassing is a key process that significantly contributed to the formation of Earth's oceans. This process involves the release of gases, including water vapor, from the Earth's interior through volcanic eruptions. As the young Earth continued to cool, the water vapor released into the atmosphere began to condense into liquid water. Over time, this accumulated into what became the Earth's oceans.

Volcanoes were much more active in the Earth's early history than they are now, continuously expelling immense quantities of gases and water vapor. This volcanic activity led to a thick atmosphere rich in water vapor. The cooling of the Earth then allowed this water to condense and fall as rain, eventually collecting in low-lying areas and further forming the oceans.
  • Volcanic outgassing was essential in providing water vapor that eventually formed oceans.
  • Early volcanic activity was extensive, contributing to a dense, water-rich atmosphere.
  • As Earth cooled, the atmosphere's water vapor condensed, creating early oceans.
Planetary Differentiation
Planetary differentiation is an important process in the young Earth's development, though not directly responsible for ocean formation. During differentiation, Earth separated into layers based on material density. The densest materials, such as iron and nickel, sank to form the core, while lighter materials formed the crust and mantle.

This process is crucial for understanding the internal structure of the Earth. Differentiation helped create the conditions for volcanic activity by generating heat within the Earth's interior. This internal heat led to melting and movement within the mantle, driving the volcanic outgassing that contributed to ocean formation. However, differentiation itself did not produce the water necessary for oceans; rather, it facilitated processes, like volcanic activity, that did.
  • Differentiation refers to the layering of Earth by density.
  • It established inner heat sources crucial for volcanic activity.
  • While not directly forming oceans, it supported volcanic outgassing, aiding in ocean creation.

One App. One Place for Learning.

All the tools & learning materials you need for study success - in one app.

Get started for free

Most popular questions from this chapter

Be sure to show all calculations clearly and state your final answers in complete sentences. You are analyzing Moon rocks that contain small amounts of uranium-238, which decays into lead with a half-life of about 4.5 billion years. a. In one rock from the lunar highlands, you determine that \(55 \%\) of the original uranium- 238 remains; the other \(45 \%\) decayed into lead. How old is the rock? b. In a rock from the lunar maria, you find that \(63 \%\) of the original uranium-238 remains; the other 37\% decayed into lead. Is this rock older or younger than the highlands rock? By how much?

To simulate the cooling of planetary bodies of different sizes, use a freezer and two small plastic containers of similar shape but different size. Fill each container with cold water and put both into the freezer at the same time. Checking every hour or so, record the time and your estimate of the thickness of the "lithosphere" (the frozen layer) in the two containers. How long does it take the water in each container to freeze completely? Describe in a few sentences the relevance of your experiment to planetary geology. Extra credit: Plot your results on a graph with time on the \(x\) -axis and lithospheric thickness on the \(y\) -axis. What is the ratio of the two freezing times?

Decide whether each statement makes sense (or is clearly true) or does not make sense (or is clearly false). Explain your reasoning clearly; because not all of these have definitive answers, your explanation is more important than your chosen answer. The most common rock type in the strata of the Grand Canyon is sedimentary rock.

Decide whether each statement makes sense (or is clearly true) or does not make sense (or is clearly false). Explain your reasoning clearly; because not all of these have definitive answers, your explanation is more important than your chosen answer. We can expect that if there are paleontologists a few million years from now, they will find the fossil remains of almost every human who ever lived.

Briefly summarize the key ways in which geology is important to Earth's long- term habitability.

See all solutions

Recommended explanations on Biology Textbooks

View all explanations

What do you think about this solution?

We value your feedback to improve our textbook solutions.

Study anywhere. Anytime. Across all devices.

Sign-up for free