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Ocean DrillingDistance Learning Program
Overview
The Ocean Drilling Distance Learning Program (OD-DLP) at Texas A&M University builds on the exciting scientific research achieved by the Ocean Drilling Program to enhance middle school science education. The OD-DLP is made possible through the collaborative efforts of the College of Geosciences and the Ocean Drilling Program, and the eEducation Group in the College of Education at Texas A&M University.
Program Objectives Increasing the technology hardware available in
rural middle school science classrooms, Providing professional development on
technology integration into classroom instruction for middle school science teachers,
Providing earth science instructional materials electronically to rural middle school science classrooms.
These objectives have been met by securing and delivering the essential hardware to participating schools
Participating School Districts
Menard ISD Happy ISD
North Zulch ISD Beeville ISD
San Isidro ISD Charlotte ISD
Motley County ISD Crystal City ISD
Pittsburg ISD Navasota ISD
Marlin ISD Poteet ISD
Carrizo Springs Consolidated ISD
Rocksprings ISD
Jefferson ISD
Resources Provided to Participating DistrictsMajor funded was provided by the
Telecommunications Infrastructure Board (TIFB)
Five WorkstationsTeacher LaptopsDigital CameraPrinterHigh-end Projector
Professional Development Five Day Intensive Opportunities in earth
science and instructional technology
Sessions focus on hands-on training
Sessions spotlight web-based curricula and resources
Each participant learns how to create a web-based science lesson using Trackstar and QuizStar
Web-based Curricula Modules
The Changing Tides Module
Ice Volume Module Sediments – What Can
We Learn from Mud Module?
645+ Texas middle school students are currently field-testing the modules in their classrooms
Web-based Curricula Framework
Lesson Objectives Pre-tests and Post-tests
with answer keys Presentation of Concepts Downloadable Student
Journal Activity Sheets for Experiments and Activities
Teacher Lesson Notes An outline of science and
technology TEKS Standards that are addressed in the lesson
Ship to Shore Conferencing
Seven live conferences were broadcasted weekly from the JOIDES Resolution:
Program Introduction-Leg 194
Shipboard Laboratories Sediments-Types and
Distribution Geological Time Using “Sound” as a Tool Changes in Sea Level The End is Just Beginning
Broadcast, Schedule and Resource Center
Instructional Delivery and Design
The interface includes instructional slides that load in the large window
Streaming video of the teacher on board loads in the lower right window Broadcast Orientation
button directs the user to the Broadcast Agenda, Teachers Notes, Student Journal Activity Page, and Related Resources
ASK A QUESTION button directs the user to the ASK A QUESTION submission page
Instructional Design
A master teacher traveled on the JOIDES Resolution, for fifty-six days and taught weekly lessons to students
Seven twenty-minute lessons were taught
Students conducted problem-solving activities weekly and posed questions
Sample Lesson Slides:How Old is Old? Geologic Time
Broadcast 4:February 7, 2001
Mrs. Joan Linsley
Relative vs. Absolute Time
Relative: the age of a rock layer in relation to other nearby layers. The precise length of geologic time represented by any layer is often unknown.
Absolute: the age of a rock or mineral in numbers of years.
Sample Lesson Slides:
Geolo
gic
Tim
eERA PERIOD EPOCH
AGE (millions of years)
Quarternary Pleistocene PlioceneMiocene
Oligocene
EocenePaleocene
Cretaceous
Jurassic
Triassic
Pa
leo
zoic
Permian
Tertiary
Ce
no
zoic
Me
so
zoic
1.85.0
23
38
54
65
135
192
280
Terms/Tools Determining AgeBiostratigraphical Unit: definition of the
boundaries of a rock layer based on the ages of fossils within it
Lithostratigraphical Unit: definition of the boundaries of a rock layer based on the physical characteristics of the rocks within
Chronostratigraphical Unit: division of a section of rock based on the absolute ages of the rocks within it
Geochronology: development of a time- line of events relating to the deposition or creation of rocks in a given area Sample Lesson Slides:
Use of Fossils Fossils provide a record of the slow, progressive development of life.
Through the use of index fossils, one may identify a particular layer of rock wherever it is exposed.
Scientists use fossils to identify ages of rocks throughout the world.
Sample Lesson Slides:
Guest
Dr. Michael Howell PaleontologistUniversity of South Carolina
These Sample Lesson Slides were used as the guest scientist presented concepts.
Fossils
Bio
/Lit
host
rati
gra
phy
Time for Ask A Question!!
“ASK A QUESTION” Mrs. Linsley, along with
project scientists, answered student questions that were submitted through the Ask a Question system
The teacher on board highlighted students’ questions and scientists’ responses during each broadcast
All ASK A QUESTION responses are posted on the weekly A-A-Q response pages
ASK A QUESTION Example Question: What exactly do you expect to find? Have you found any
clues that there are any life forms that have not been discovered yet?Name: MelissaSchool: Charlotte Middle School, Charlotte TXResponse: We expect to find that there have been rises and falls in the sea level that drowned and exposed the reefs at various times. We will be investigating the times these occurred and the magnitudes of them. One of the scientists has found a foraminifer that appears to be different from those found here previously. There is an indication that there was a shallow lagoon here with sea grass because sea grass fossils were found. This was expected as a part of the reef system. We don't expect to find new life forms, but discovery is always possible. To take a look at some of the life forms we are finding, look at this page on calcareous nannofossils, and this page on foraminifers (mentioned in Broadcast 4 on Geologic Time). Some new life forms were discovered by other scientists as part of a seafloor system called a hydrothermal vent. Scientists didn't know that life could exist in such extreme conditions until they actually went to the vents to study them. To find out more about these newest seafloor forms of life, visit this page on seavents.
Journal Activity ExamplesWhy do you think fossils are
useful in finding ages of sediments?
Fossils are useful for two important reasons:
They are found in many rocks and sediments in many locations around the world. Because they are widespread and have fixed periods of time in which the organisms lived, they are the most commonly used tool for identifying the ages of sediments and sedimentary rocks. Other age-dating tools, such as radiometric dating (absolute ages) cannot be used as often as fossils because of the lack of appropriate minerals to analyze with these methods…