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  • Hofstra University Misp Plate Tectonics Worksheet 2 2011

Get Hofstra University Misp Plate Tectonics Worksheet 2 2011-2025

Tp://pubs.usgs.gov/publications/text/Hawaiian.html) The Hawaiian Islands represent the last and youngest part of a long chain of volcanoes extending some 6000 km across the Pacific Ocean and ending in the Aleutian Trench off the coast of Alaska. This volcanic chain consists of the small section Hawaiian archipelago (Windward Isles, and the U.S. State of Hawaii), the much longer Northwestern Hawaiian Islands (Leeward Isles), and finally the long Emperor Seamounts. The Leeward Isles consist mostly.

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How to fill out the Hofstra University MiSP Plate Tectonics Worksheet 2 online

This guide provides clear, step-by-step instructions to help users successfully fill out the Hofstra University MiSP Plate Tectonics Worksheet 2 online. Whether you are a student or an educator, this comprehensive resource will make the process straightforward and user-friendly.

Follow the steps to complete the worksheet effectively.

  1. Click the ‘Get Form’ button to obtain the worksheet and open it for filling out.
  2. Begin by entering your name in the designated space at the top of the form.
  3. Fill in the date next to the 'Date' label to indicate when you are completing the worksheet.
  4. In Procedure 1, utilize Table 1 to plot a graph comparing the age of the Hawaiian Islands with their longitude. Make sure to label each plotted point with the corresponding island or reef name and connect the points with a smooth line.
  5. Answer the questions in the Discussion section regarding the deviation of islands from the best-fit line and approximate ages based on your graph.
  6. Proceed to Procedure 2, where you will transfer the age data from Table 1 to the Hawaii Map associated with each volcano and record it in Table 2.
  7. Measure the distance from each island's volcanic peak to the Kilauea Volcano, documenting this measurement in Column B of Table 2.
  8. Calculate the actual distance and document it in Columns C and D, followed by the ages in Column E and converting them to years in Column F.
  9. Finally, calculate the average rate of movement for each island, filling in the results in Column G of Table 2.
  10. Once you have completed all sections, ensure to save your changes, and utilize the options to download, print, or share the completed worksheet as needed.

Fill out the Hofstra University MiSP Plate Tectonics Worksheet 2 online today for an enriching educational experience!

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List of modern island arcs Island arcCountryOverriding PlateJapanese ArchipelagoJapanNorth American Plate, Eurasian PlateRyukyu IslandsJapanEurasian PlatePhilippine IslandsPhilippinesEurasian PlateSunda ArcIndonesiaEurasian Plate12 more rows

The Hawaiian Islands and the chain of seamounts that continue their trend for about 6,000 kilometers (3,750 miles) into the northwest Pacific Ocean are an example of a hotspot track. The Island of Hawaii is the youngest, and most active, volcano in the chain.

The Hawaiian Islands were formed by such a hot spot occurring in the middle of the Pacific Plate. While the hot spot itself is fixed, the plate is moving. So, as the plate moved over the hot spot, the string of islands that make up the Hawaiian Island chain were formed.

The molten magma rises up and breaks through the crust to form a volcano. While the hot spot stays in one place, rooted to its deep source of heat, the tectonic plate is slowly moving above it. As the plate moves, so does the volcano, and another one forms in its place. The volcano that moved is no longer active.

The Pacific Plate is being moved north west due to sea floor spreading from the East Pacific Rise (divergent margin) in the Gulf of California. The North American Plate is being pushed west and north west due to sea floor spreading from the Mid Atlantic Ridge (divergent margin).

The Formation of the Hawaiian Islands Ages of some of the Hawaiian Islands and outer seamountsVolcano Number (see note at table bottom)Volcano NameDistance from Kilauea along trend of chain (km)69Yuryaku3,52072Kimmei3,66874Koko (southern)3,75841 more rows • May 13, 2018

The active hot spot lies near the center of the Pacific plate, under the southeastern end of the Island chain. The rising magma plumes and subsequent eruptions have created the Island chain. As noted in the previous section, the Pacific plate is moving toward the northwest in the Hawaiian Islands region.

In the case of the Hawaiian Islands, the Pacific Plate is continually moving to the northwest over the Hawaiian hot spot. This movement caused the Hawaiian chain of islands to form.

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© Copyright 1997-2025
airSlate Legal Forms, Inc.
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Form Packages
Adoption
Bankruptcy
Contractors
Divorce
Home Sales
Employment
Identity Theft
Incorporation
Landlord Tenant
Living Trust
Name Change
Personal Planning
Small Business
Wills & Estates
Packages A-Z
Form Categories
Affidavits
Bankruptcy
Bill of Sale
Corporate - LLC
Divorce
Employment
Identity Theft
Internet Technology
Landlord Tenant
Living Wills
Name Change
Power of Attorney
Real Estate
Small Estates
Wills
All Forms
Forms A-Z
Form Library
Customer Service
Terms of Service
Privacy Notice
Legal Hub
Content Takedown Policy
Bug Bounty Program
About Us
Blog
Affiliates
Contact Us
Delete My Account
Site Map
Industries
Forms in Spanish
Localized Forms
State-specific Forms
Forms Kit
Legal Guides
Real Estate Handbook
All Guides
Prepared for You
Notarize
Incorporation services
Our Customers
For Consumers
For Small Business
For Attorneys
Our Sites
US Legal Forms
USLegal
FormsPass
pdfFiller
signNow
airSlate WorkFlow
DocHub
Instapage
Social Media
Call us now toll free:
+1 833 426 79 33
As seen in:
  • USA Today logo picture
  • CBC News logo picture
  • LA Times logo picture
  • The Washington Post logo picture
  • AP logo picture
  • Forbes logo picture
© Copyright 1997-2025
airSlate Legal Forms, Inc.
3720 Flowood Dr, Flowood, Mississippi 39232