Scan1

  • April 2020
  • PDF

This document was uploaded by user and they confirmed that they have the permission to share it. If you are author or own the copyright of this book, please report to us by using this DMCA report form. Report DMCA


Overview

Download & View Scan1 as PDF for free.

More details

  • Words: 305
  • Pages: 1
7. The diagram below represents a cross section of a pOliion of the Earth's crust.

Ocean

Oceanic crust (basalt)

II

9. The diagram below represents a geologic cross section of a portion of Earth's crust.

Continental crust (granite)

I

\~

( Not drawn to scaie )

Folding and erosion occurred after the fOlmation of the (1) Gayle shale (2) Freeport sandstone (3) Erie coal, but before formation of Freeport sa.lldstone (4) Dunbar limestone, but before formation or Erie coal

¥lmch statement about the Earth's crust is best supported by the diagram? (1) The oceanic crust is thicker than the mantle. (2) The continental crust is thicker than the oceanic crust. (3) The continental crust is composed primarily of sedimentary rock. (4) The crust is composed of denser rock than the mantle is.

10. Which geologic event occurred most recently in New York State? (1) A continental glacier covered most of the State. (2) The entire State was uplifted fi.om below sea leveL (3) The Palisades Sill intruded. (4) The Taconic Mountains formed.

8. The diagram below represents cross sections of three rock outcrops approximately 100 kilometers apart. \\That would be the best method or correlating the rock layers of each outcrop?

c

'1 1 ',l

'

~

c,v",n8111'lO "o"k -,---, ..•..i .•.tJ. ;:,.;;. "'...~tynes .....t-' ...

/"" comparmg .. mmera 1 composItIOn ' .

\L)

) comparing index fossils (4'1 ro,rnpc""l'nn l'h;~'i,.",,,,s'" ,,+ ',) ."" l./.. .•. {..w. l....I.b 11..>.\..A'L.d..\.. ••.' C'..l...

1..'.. 1J...

The characteristic of the radioactive isotope uraruum-238 that ma.kes this isotope useful for accurately dating the age of a rock is the isotope's (1) (2) (3) (4)

organic origin constant half-life common OCCUITencein sediments resistance to \veat1J,cring a.nd erosion

temperature of 73° Fahrenheit is appr()Xirllatel~veq'ual to a temperature of (I

17° Celsi"us

26° Celsius

23° eelsiv.s

1620 C=elsius

April Reyiew 2009

Related Documents

Scan1
April 2020 3
Scan1
October 2019 14
Scan1.pdf
December 2019 5
Scan1.pdf
December 2019 8
Scan1.pdf
December 2019 11
Scan1.pdf
July 2020 3