Rocks, Fossils & Evolution Quiz

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Explore fossils, rocks, and evolution.

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Josie

Estados Unidos

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Rocks, Fossils & Evolution Quiz


Rocks, Fossils & Evolution QuizVersión en línea Explore fossils, rocks, and evolution. por Josie 1 Erosion and Weathering never create gaps in the geologic record. Yes No 2 Index fossils lived for relatively short times but were widespread geographically. Yes No 3 The Law of Superposition says newer layers are below older ones. Yes No 4 Artificial selection occurs without human involvement. Yes No 5 How Fossils Help Scientists: they provide a physical record of how species have changed over millions of years. Yes No 6 Fossilization methods include burial in sediment, amber, freezing in ice, or preservation in tar pits. Yes No 7 Intrusions: magma that melts through existing rock and then cools into igneous rock. Yes No 8 Law of Superposition: in an undisturbed sequence of sedimentary rocks, each layer is older than the one above it. Yes No 9 Mutations have no effect on survival or evolution. Yes No 10 Fossils can form only in amber and tar pits. Yes No 11 Fossilization methods include burial in sediment and mineralization. Yes No 12 The Process of Evolution happens only through natural selection; mutations have no role. Yes No 13 Intrusions are rocks that form at the Earth’s surface and do not move through existing rock layers. Yes No 14 Fossilization only occurs in amber and tar pits. Yes No 15 Fossils help scientists by providing a physical record of how species have changed over millions of years. Yes No 16 Index fossils are fossils of organisms that lived for a relatively short period but were widespread geographically. Yes No 17 Intrusions and faults always move upward toward the surface. Yes No 18 A cross-cutting principle means a rock feature that cuts through another must be older than the rock it cuts through. Yes No 19 Mutations can be helpful, neutral, or harmful in evolution. Yes No 20 The Law of Superposition states that in an undisturbed sequence of sedimentary rocks, older layers lie below younger ones. Yes No

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Rocks, Fossils & Evolution Quiz

Sí o No

Sobre esta actividad

Creada por

Descarga la versión para jugar en papel

Top juegos

Sí o No

OPEN UP 5 UNIT 3: THERE IS/ARE, THERE WAS, THERE WERE

Sí o No

Grammys a mejor canción/grabación

Sí o No

¿Es verdad?

Sí o No

¿Está creado con Inteligencia Artificial?

Sí o No

Preguntas sobre futbol para niños

Rocks, Fossils & Evolution QuizVersión en línea

por Josie

Erosion and Weathering never create gaps in the geologic record.

Index fossils lived for relatively short times but were widespread geographically.

The Law of Superposition says newer layers are below older ones.

Artificial selection occurs without human involvement.

How Fossils Help Scientists: they provide a physical record of how species have changed over millions of years.

Fossilization methods include burial in sediment, amber, freezing in ice, or preservation in tar pits.

Intrusions: magma that melts through existing rock and then cools into igneous rock.

Law of Superposition: in an undisturbed sequence of sedimentary rocks, each layer is older than the one above it.

Mutations have no effect on survival or evolution.

Fossils can form only in amber and tar pits.

Fossilization methods include burial in sediment and mineralization.

The Process of Evolution happens only through natural selection; mutations have no role.

Intrusions are rocks that form at the Earth’s surface and do not move through existing rock layers.

Fossilization only occurs in amber and tar pits.

Fossils help scientists by providing a physical record of how species have changed over millions of years.

Index fossils are fossils of organisms that lived for a relatively short period but were widespread geographically.

Intrusions and faults always move upward toward the surface.

A cross-cutting principle means a rock feature that cuts through another must be older than the rock it cuts through.

Mutations can be helpful, neutral, or harmful in evolution.

The Law of Superposition states that in an undisturbed sequence of sedimentary rocks, older layers lie below younger ones.