Synopsys For Physical Design Of Asic Computer Science Essay

Synopsys For Physical Design Of Asic Computer Science Essay IC Compiler is the software package from Synopsys for Physical Design of ASIC. It provides necessary tools to complete the back end design of the very deep submicron designs. The inputs to the IC Compiler are: a gate-level netlist which can be from DC Compiler or third-party tools, a detailed floorplan which can be from previous Design Planning through IC Compiler or other third-party tools, timing constraints and other constraints, physical and timing libraries provided by manufacturer, and foundry-process data. IC Compiler generates a GDSII-format file as output ready for tape out of the chip. In addition, it is possible to export a Design Exchange Format (DEF) file of placed netlist data ready for a third-party router. IC Compiler uses a binary Synopsys Milkyway database, which can be used by other Synopsys tools based on Milkyway. [16] 4.2 User Interfaces IC Compiler can be used either with Shell interface (icc_shell) or with Graphical user interface (GUI). Shell interface is the command-line interface, which is used for batch mode, scripts, typing commands, and push-button type of operations. Graphical user interface (GUI) is an advanced graphical analysis and physical editing tool. Certain tasks, such as very accurately displaying the design and providing visual analysis tools, can only performed from the GUI. Also tool command language (Tcl), which is used in many applications in the EDA industry, is available to IC Compiler. Using Tcl, you can write reusable procedures and scripts. The IC Compiler design flow is an easy-to-use, single-pass flow that provides convergent timing closure. Figure 4.1 shows the basic IC Compiler design flow, which is centered around three core commands that perform placement and optimization (place_opt), clock tree synthesis and optimization (clock_opt), and routing and postroute optimization (route_opt). [16] icc1 Figure 4.1 IC Compiler Design Flow [21] For most designs, if the place_opt, clock_opt, and route_opt steps are followed, IC Compiler will provide optimal results. You can use IC Compiler to efficiently perform chip-level design planning, placement, clock tree synthesis and routing on designs with moderate timing and congestion challenges. To further improve the quality of results for your design you can use additional commands and switches for placement, clock tree synthesis, and routing steps that IC Compiler provides. IC Compiler design flow involves execution of following steps: 1. Set up and prepare the libraries and the design data. 2. Perform design planning and power planning. -Design planning is to perform necessary steps to create a floorplan, determine the size of the design, create the boundary and core area, create site rows for the placement of standard cells, set up the I/O pads. -Power planning, is to perform necessary steps to create a power plan to meet the power budget and the target leakage current. 3. Perform placement and optimization. IC Compiler placement and optimization uses enhanced placement and synthesis technologies to generate a legalized placement for leaf cells and an optimized design, which addresses and resolves timing closure issues for the provided design. You can supplement this functionality by optimizing for power, recovering area for placement, minimizing congestion, and minimizing timing and design rule violations. To perform placement and optimization, use the place_opt core command (or from GUI choose Placement menu and then Core Placement and Optimization sub-menu). 4. Perform clock tree synthesis and optimization. To perform the clock tree synthesis and optimization phase, use the command clock_opt (or choose Clock > Core Clock Tree Synthesis and Optimization in the GUI). IC Compiler clock tree synthesis and embedded optimization solve complicated clock tree synthesis problems, such as blockage avoidance and the correlation between preroute and postroute data. Clock tree optimization improves both clock skew and clock insertion delay by performing buffer sizing, buffer relocation, gate sizing, gate relocation, level adjustment, reconfiguration, delay insertion, dummy load insertion, and balancing of interclock delays. 5. Perform routing and postroute optimization. To perform routing and postroute optimization, use the route_opt core command (or choose Route > Core Routing and Optimization in the GUI). As part of routing and postroute optimization, IC Compiler performs global routing, track assignment, detail routing, search and repair, topological optimization, and engineering change order (ECO) routing. For most designs, the default routing and postroute optimization setup produces optimal results. If necessary, you can supplement this functionality by optimizing routing patterns and reducing crosstalk or by customizing the routing and postroute optimization functions for special needs. 6. Perform chip finishing and design for manufacturing tasks. IC Compiler provides chip finishing and design for manufacturing and yield capabilities that you can apply throughout the various stages of the design flow to address process design issues encountered during chip manufacturing. 7. Save the design. Save your design in the Milkyway format. This format is the internal database format used by IC Compiler to store all the logical and physical information about a design. [16] 4.3 How to Invoke the IC Compiler 1. Log in to the UNIX environment with the user id and password . 2. Start IC Compiler from the UNIX promt: UNIX$ icc_shell The xterm unix prompt turns into the IC Compiler shell command prompt. 3. Start the GUI. icc_shell> start_gui This window can display schematics and logical browsers, among other things, once a design is loaded. 4.4 Preparing the Design IC Compiler uses a Milkyway design library to store design and its associated library information. This section describes how to set up the libraries, create a Milkyway design library, read your design, and save the design in Milkyway format. These steps are explained in the following sections: à ¢Ã¢â€š ¬Ã‚ ¢ Setting Up the Libraries à ¢Ã¢â€š ¬Ã‚ ¢ Setting Up the Power and Ground Nets à ¢Ã¢â€š ¬Ã‚ ¢ Reading the Design à ¢Ã¢â€š ¬Ã‚ ¢ Annotating the Physical Data à ¢Ã¢â€š ¬Ã‚ ¢ Preparing for Timing Analysis and RC Calculation à ¢Ã¢â€š ¬Ã‚ ¢ Saving the Design 4.4.1 Setting Up the Libraries IC Compiler requires both logic libraries and physical libraries. The following sections describe how to set up and validate these libraries. à ¢Ã¢â€š ¬Ã‚ ¢ Setting Up the Logic Libraries: IC Compiler uses logic libraries to provide timing and functionality information for all standard cells. In addition, logic libraries can provide timing information for hard macros, such as RAMs. IC Compiler uses variables to define the logic library settings. In each session, you must define the values for the following variables (either interactively, in the .synopsys_dc.setup file, or by restoring the values saved in the Milkyway design library) so that IC Compiler can access the libraries: à ¢Ã¢â€š ¬Ã‚ ¢ search_path Lists the paths where IC Compiler can locate the logic libraries. à ¢Ã¢â€š ¬Ã‚ ¢ target_library Lists the logic libraries that IC Compiler can use to perform physical optimization. à ¢Ã¢â€š ¬Ã‚ ¢ link_library Lists the logic libraries that IC Compiler can search to resolve references. à ¢Ã¢â€š ¬Ã‚ ¢ Setting Up the Physical Libraries: IC Compiler uses Milkyway reference libraries and technology (.tf) files to provide physical library information. The Milkyway reference libraries contain physical information about the standard cells and macro cells in your technology library. In addition, these reference libraries define the placement unit tile. The technology files provide information such as the names and characteristics (physical and electrical) for each metal layer, which are technology-specific. The physical library information is stored in the Milkyway design library. For each cell, the Milkyway design library contains several views of the cell, which are used for different physical design tasks. If you have not already created a Milkyway library for your design (by using another tool that uses Milkyway), you need to create one by using the IC Compiler tool. If you already have a Milkyway design library, you must open it before working on your design. This section describes how to perform the following tasks: à ¢Ã¢â€š ¬Ã‚ ¢ Create a Milkyway design library To create a Milkyway design library, use the create_mw_lib command (or choose File > Create Library in the GUI). à ¢Ã¢â€š ¬Ã‚ ¢ Open a Milkyway design library To open an existing Milkyway design library, use the open_mw_lib command (or choose File > Open Library in the GUI). à ¢Ã¢â€š ¬Ã‚ ¢ Report on a Milkyway design library To report on the reference libraries attached to the design library, use the -mw_reference_library option. icc_shell>report_mw_lib-mw_reference_library design_library_name To report on the units used in the design library, use the report_units command. icc_shell> report_units à ¢Ã¢â€š ¬Ã‚ ¢ Change the physical library information To change the technology file, use the set_mw_technology_file command (or choose File > Set Technology File in the GUI) to specify the new technology file name and the name of the design library. à ¢Ã¢â€š ¬Ã‚ ¢ Save the physical library information To save the technology or reference control information in a file for later use, use the write_mw_lib_files command (or choose File > Export > Write Library File in the GUI). In a single invocation of the command, you can output only one type of file. To output both a technology file and a reference control file, you must run the command twice. à ¢Ã¢â€š ¬Ã‚ ¢ Verifying Library Consistency: Consistency between the logic library and the physical library is critical to achieving good results. Before you process your design, ensure that your libraries are consistent by running the check_library command. [16] icc_shell> check_library 4.4.2 Setting Up the Power and Ground Nets IC Compiler uses variables to define names for the power and ground nets. In each session, you must define the values for the following variables (either interactively or in the .synopsys_dc.setup file) so that IC Compiler can identify the power and ground nets: à ¢Ã¢â€š ¬Ã‚ ¢ mw_logic0_net By default, IC Compiler VSS as the ground net name. If you are using a different name, you must specify the name by setting the mw_logic0_net variable. à ¢Ã¢â€š ¬Ã‚ ¢ mw_logic1_net By default, IC Compiler uses VDD as the power net name. If you are using a different name, you must specify the name by setting the mw_logic1_net variable. 4.4.3 Reading the Design IC Compiler can read designs in either Milkyway or ASCII (Verilog, DEF, and SDC files) format. à ¢Ã¢â€š ¬Ã‚ ¢ Reading a Design in Milkyway Format à ¢Ã¢â€š ¬Ã‚ ¢ Reading a Design in ASCII Format 4.4.4 Annotating the Physical Data IC Compiler provides several methods of annotating physical data on the design: à ¢Ã¢â€š ¬Ã‚ ¢ Reading the physical data from a DEF file To read a DEF file, use the read_def command (or choose File > Import > Read DEF in the GUI). icc_shell> read_def -allow_physical design_name.def à ¢Ã¢â€š ¬Ã‚ ¢ Reading the physical data from a floorplan file A floorplan file is a file that you previously created by using the write_floorplan command (or by choosing Floorplan > Write Floorplan in the GUI). icc_shell> read_floorplan floorplan_file_name à ¢Ã¢â€š ¬Ã‚ ¢ Copying the physical data from another design To copy physical data from the layout (CEL) view of one design in the current Milkyway design library to another, use the copy_floorplan command (or choose Floorplan > Copy Floorplan in the GUI). [16] icc_shell> copy_floorplan -from design1 4.4.5 Preparing for Timing Analysis and RC Calculation IC Compiler provides RC calculation technology and timing analysis capabilities for both preroute and postroute data. Before you perform RC calculation and timing analysis, you must complete the following tasks: à ¢Ã¢â€š ¬Ã‚ ¢ Set up the TLUPlus files You specify these files by using the set_tlu_plus_files command (or by choosing File > Set TLU+ in the GUI). icc_shell> set_tlu_plus_files -tech2itf_map ./path/map_file_name.map -max_tluplus ./path/worst_settings.tlup -min_tluplus ./path/best_settings.tlup à ¢Ã¢â€š ¬Ã‚ ¢ (Optional) Back-annotate delay or parasitic data To back-annotate the design with delay information provided in a Standard Delay Format (SDF) file, use the read_sdf command (or choose File > Import > Read SDF in the GUI). To remove annotated data from design, use the remove_annotations command. à ¢Ã¢â€š ¬Ã‚ ¢ Set the timing constraints At a minimum, the timing constraints must contain a clock definition for each clock signal, as well as input and output arrival times for each I/O port. This requirement ensures that all signal paths are constrained for timing. To read a timing constraints file, use the read_sdc command (or choose File > Import > Read SDC in the GUI). icc_shell> read_sdc -version 1.7 design_name.sdc à ¢Ã¢â€š ¬Ã‚ ¢ Specify the analysis mode Semiconductor device parameters can vary with conditions such as fabrication process, operating temperature, and power supply voltage. The set_operating_conditions command specifies the operating conditions for analysis. à ¢Ã¢â€š ¬Ã‚ ¢ (Optional) Set the derating factors If your timing library does not include minimum and maximum timing data, you can perform simultaneous minimum and maximum timing analysis by specifying derating factors for your timing library. Use the set_timing_derate command to specify the derating factors. à ¢Ã¢â€š ¬Ã‚ ¢ Select the delay calculation algorithm By default, IC Compiler uses Elmore delay calculation for both preroute and postroute delay calculations. For postroute delay calculations, you can choose to use Arnoldi delay calculation either for clock nets only or for all nets. Elmore delay calculation is faster, but its results do not always correlate with the PrimeTime and PrimeTime SI results. The Arnoldi calculation is best used for designs with smaller geometries and high resistive nets, but it requires more runtime and memory. [16] 4.4.6 Saving the Design To save the design in Milkyway format, use the save_mw_cel command (or choose File > Save Design in the GUI). [16] CHAPTER 5: Design Planning 5.1 Introduction Design planning in IC Compiler provides basic floorplanning and prototyping capabilities such as dirty-netlist handling, automatic die size exploration, performing various operations with black box modules and cells, fast placement of macros and standard cells, packing macros into arrays, creating and shaping plan groups, in-place optimization, prototype global routing analysis, hierarchical clock planning, performing pin assignment on soft macros and plan groups, performing timing budgeting, converting the hierarchy, and refining the pin assignment. Power network synthesis and power network analysis functions, applied during the feasibility phase of design planning, provide automatic synthesis of local power structures within voltage areas. Power network analysis validates the power synthesis results by performing voltage-drop and electromigration analysis. [16] Figure 5.1 IC Compiler Design Planning [21] 5.2 Tasks to be performed during Design Planning à ¢Ã¢â€š ¬Ã‚ ¢ Initializing the Floorplan à ¢Ã¢â€š ¬Ã‚ ¢ Automating Die Size Exploration à ¢Ã¢â€š ¬Ã‚ ¢ Handling Black Boxes à ¢Ã¢â€š ¬Ã‚ ¢ Performing an Initial Virtual Flat Placement à ¢Ã¢â€š ¬Ã‚ ¢ Creating and Shaping Plan Groups à ¢Ã¢â€š ¬Ã‚ ¢ Performing Power Planning à ¢Ã¢â€š ¬Ã‚ ¢ Performing Prototype Global Routing à ¢Ã¢â€š ¬Ã‚ ¢ Performing Hierarchical Clock Planning à ¢Ã¢â€š ¬Ã‚ ¢ Performing In-Place Optimization à ¢Ã¢â€š ¬Ã‚ ¢ Performing Routing-Based Pin Assignment à ¢Ã¢â€š ¬Ã‚ ¢ Performing RC Extraction à ¢Ã¢â€š ¬Ã‚ ¢ Performing Timing Analysis à ¢Ã¢â€š ¬Ã‚ ¢ Performing Timing Budgeting à ¢Ã¢â€š ¬Ã‚ ¢ Committing the Physical Hierarchy à ¢Ã¢â€š ¬Ã‚ ¢ Refining the Pin Assignment 5.3 Initializing the Floorplan The steps in initializing the floorplan are described below. à ¢Ã¢â€š ¬Ã‚ ¢ Reading the I/O Constraints: To load the top-level I/O pad and pin constraints, use the read_io_constraints command. à ¢Ã¢â€š ¬Ã‚ ¢ Defining the Core and Placing the I/O Pads: To define the core and place the I/O pads and pins, use the initialize_floorplan command. à ¢Ã¢â€š ¬Ã‚ ¢ Creating Rectilinear-Shaped Blocks: Use the initialize_rectilinear_block command to create a floorplan for rectilinear blocks from a fixed set of L, T, U, or cross-shaped templates. These templates are used to determine the cell boundary and shape of the core. To do this, use initialize_rectilinear_block -shape L|T|U|X. à ¢Ã¢â€š ¬Ã‚ ¢ Writing I/O Constraint Information: To write top-level I/O pad or pin constraints, use the write_io_constraints command. Read the Synopsys Design Constraints (SDC) file (read_sdc command) to ensure that all signal paths are constrained for timing. à ¢Ã¢â€š ¬Ã‚ ¢ Adding Cell Rows: To add cell rows, use the add_row command. à ¢Ã¢â€š ¬Ã‚ ¢ Removing Cell Rows: To remove cell rows, use the cut_row command. à ¢Ã¢â€š ¬Ã‚ ¢ Saving the Floorplan Information: To save the floorplan information, use the write_floorplan command. à ¢Ã¢â€š ¬Ã‚ ¢Writing Floorplan Physical Constraints for Design Compiler Topographical Technology: IC Compiler can now write out the floorplan physical constraints for Design Compiler Topographical Technology (DC-T) in Tcl format. The reason for using floorplan physical constraints in the Design Compiler topographical technology mode is to accurately represent the placement area and to improve timing correlation with the post-place-and-route design. The command syntax is: write_physical_constraints -output output_file_name -port_side [16] Figure 5.2 Floor Plan After Initialization [21] 5.4 Automating Die Size Exploration This section describes how to use MinChip technology in IC Compiler to automate the processes exploring and identifying the valid die areas to determine smallest routable, die size for your design while maintaining the relative placement of hard macros, I/O cells, and a power structure that meets voltage drop requirements. The technology is integrated into the Design Planning tool through the estimate_fp_area command. The input is a physically flat Milkyway CEL view. 5.5 Handling Black Boxes Black boxes can be represented in the physical design as either soft or hard macros. A black box macro has a fixed height and width. A black box soft macro sized by area and utilization can be shaped to best fit the floorplan. To handle the black boxes run the following set of commands. set_fp_base_gate estimate_fp_black_boxes flatten_fp_black_boxes create_fp_placement place_fp_pins create_qtm_model qtm_bb set_qtm_technology -lib library_name create_qtm_port -type clock $port report_qtm_model write_qtm_model -format qtm_bb report_timing qtm_bb 5.6 Performing an Initial Virtual Flat Placement The initial virtual flat placement is very fast and is optimized for wire length, congestion, and timing. The way to perform an initial virtual flat placement is described below. à ¢Ã¢â€š ¬Ã‚ ¢ Evaluating Initial Hard Macro Placement: No straightforward criteria exist for evaluating the initial hard macro placement. Measuring the quality of results (QoR) of the hard macro placement can be very subjective and often depends on practical design experience. à ¢Ã¢â€š ¬Ã‚ ¢ Specifying Hard Macro Placement Constraints: Different methods can be use to control the preplacement of hard macros and improve the QoR of the hard macro placement. Creating a User-Defined Array of Hard Macros Setting Floorplan Placement Constraints On Macro Cells Placing a Macro Cell Relative to an Anchor Object Using a Virtual Flat Placement Strategy Enhancing the Behavior of Virtual Flat Placement With the macros_on_edge Switch Creating Macro Blockages for Hard Macros Padding the Hard Macros à ¢Ã¢â€š ¬Ã‚ ¢ Padding the Hard Macros: To avoid placing standard cells too close to macros, which can cause congestion or DRC violations, one can set a user-defined padding distance or keepout margin around the macros. One can set this padding distance on a selected macros cell instance master.During virtual flat placement no other cells will be placed within the specified distance from the macros edges. [16] To set a padding distance (keepout margin) on a selected macros cell instance master, use the set_keepout_margin command. à ¢Ã¢â€š ¬Ã‚ ¢ Placing Hard Macros and Standard Cells: To place the hard macros and standard cells simultaneously, use the create_fp_placement command. à ¢Ã¢â€š ¬Ã‚ ¢ Performing Floorplan Editing: IC Compiler performs the following floorplan editing operations. Creating objects Deleting objects Undoing and redoing edit changes Moving objects Changing the way objects snap to a grid Aligning movable objects 5.7 Creating and Shaping Plan Groups This section describes how to create plan groups for logic modules that need to be physically implemented. Plan groups restrict the placement of cells to a specific region of the core area. This section also describes how to automatically place and shape objects in a design core, add padding around plan group boundaries, and prevent signal leakage and maintain signal integrity by adding modular block shielding to plan groups and soft macros. The following steps are covered for Creating and Shaping Plan Groups. à ¢Ã¢â€š ¬Ã‚ ¢ Creating Plan Groups: To create a plan group, create_plan_groups command. To remove (delete) plan groups from the current design, use the remove_plan_groups command. à ¢Ã¢â€š ¬Ã‚ ¢ Automatically Placing and Shaping Objects In a Design Core: Plan groups are automatically shaped, sized, and placed inside the core area based on the distribution of cells resulting from the initial virtual flat placement. Blocks (plan groups, voltage areas, and soft macros) marked fix remain fixed; the other blocks, whether or not they are inside the core, are subject to being moved or reshaped. To automatically place and shape objects in the design core, shape_fp_blocks command. à ¢Ã¢â€š ¬Ã‚ ¢ Adding Padding to Plan Groups: To prevent congestion or DRC violations, one can add padding around plan group boundaries. Plan group padding sets placement blockages on the internal and external edges of the plan group boundary. Internal padding is equivalent to boundary spacing in the core area. External padding is equivalent to macro padding. To add padding to plan groups, create_fp_plan_group_padding command. To remove both external and internal padding for the plan groups, use the remove_fp_plan_group_padding command. à ¢Ã¢â€š ¬Ã‚ ¢ Adding Block Shielding to Plan Groups or Soft Macros: When two signals are routed parallel to each other, signal leakage can occur between the signals, leading to an unreliable design. One can protect signal integrity by adding modular block shielding to plan groups and soft macros. The shielding consists of metal rectangles that are created around the outside of the soft macro boundary in the top level of the design, and around the inside boundary of the soft macro. To add block shielding for plan groups or soft macros, use the create_fp_block_shielding command. To remove the signal shielding created by modular block shielding, use the remove_fp_block_shielding command. [16] 5.8 Performing Power Planning After completed the design planning process and have a complete floorplan, one can perform power planning, as explained below. à ¢Ã¢â€š ¬Ã‚ ¢ Creating Logical Power and Ground Connections: To define power and ground connections, use the connect_pg_nets command. à ¢Ã¢â€š ¬Ã‚ ¢ Adding Power and Ground Rings: It is necessary to add power and ground rings after doing floorplanning. To add power and ground rings, use the create_rectangular_rings command. à ¢Ã¢â€š ¬Ã‚ ¢ Adding Power and Ground Straps: To add power and ground straps, use the create_power_straps command. à ¢Ã¢â€š ¬Ã‚ ¢ Prerouting Standard Cells: To preroute standard cells, use the preroute_standard_cells command. à ¢Ã¢â€š ¬Ã‚ ¢ Performing Low-Power Planning for Multithreshold-CMOS Designs: One can perform floorplanning for low-power designs by employing power gating. Power gating has the potential to reduce overall power consumption substantially because it reduces leakage power as well as switching power. à ¢Ã¢â€š ¬Ã‚ ¢ Performing Power Network Synthesis: As the design process moves toward creating 65-nm transistors, issues related to power and signal integrity, such as power grid generation, voltage (IR) drop, and electromigration, have become more significant and complex. In addition, this complex technology lengthens the turnaround time needed to identify and fix power and signal integrity problems. By performing power network synthesis one can preview an early power plan that reduces the chances of encountering electromigration and voltage drop problems later in the detailed power routing. To perform the PNS, one can run the set of following commands. [16] synthesize_fp_rail set_fp_rail_constraints set_fp_rail_constraints -set_ring set_fp_block_ring_constraints set_fp_power_pad_constraints set_fp_rail_region_constraints set_fp_rail_voltage_area_constraints set_fp_rail_strategy à ¢Ã¢â€š ¬Ã‚ ¢ Committing the Power Plan: Once the IR drop map meets the IR drop constraints, one can run the commit_fp_rail command to transform the IR drop map into a power plan. à ¢Ã¢â€š ¬Ã‚ ¢ Handling TLUPlus Models in Power Network Synthesis: Power network synthesis supports TLUPlus models. set_fp_rail_strategy -use_tluplus true à ¢Ã¢â€š ¬Ã‚ ¢ Checking Power Network Synthesis Integrity: Initially, when power network synthesis first proposes a power mesh structure, it assumes that the power pins of the mesh are connected to the hard macros and standard cells in the design. It then displays a voltage drop map that one can view to determine if it meets the voltage (IR) drop constraints. After the power mesh is committed, one might discover problem areas in design as a result of automatic or manual cell placement. These areas are referred to as chimney areas and pin connect areas. To Check the PNS Integrity one can run the following set of commands. set_fp_rail_strategy -pns_commit_check_file set_fp_rail_strategy -pns_check_chimney_file set_fp_rail_strategy -pns_check_chimney_file pns_chimney_report set_fp_rail_strategy -pns_check_hor_chimney_layers set_fp_rail_strategy -pns_check_chimney_min_dist set_fp_rail_strategy -pns_check_pad_connection file_name set_fp_rail_strategy -pns_report_pad_connection_limit set_fp_rail_strategy -pns_report_min_pin_width set_fp_rail_strategy -pns_check_hard_macro_connection file_name set_fp_rail_strategy -pns_check_hard_macro_connection_limit set_fp_rail_strategy -pns_report_min_pin_width à ¢Ã¢â€š ¬Ã‚ ¢ Analyzing the Power Network: One perform power network analysis to predict IR drop at different floorplan stages on both complete and incomplete power nets in the design. To perform power network analysis, use the analyze_fp_rail command. To add virtual pads, use the create_fp_virtual_pad command. To ignore the hard macro blockages, use the set_fp_power_plan_constraints command. à ¢Ã¢â€š ¬Ã‚ ¢ Viewing the Analysis Results: When power and rail analysis are complete, one can check for the voltage drop and electromigration violations in the design by using the voltage drop map and the electromigration map. One can save the results of voltage drop and electromigration current density values to the database by saving the CEL view that has just been analyzed. à ¢Ã¢â€š ¬Ã‚ ¢ Reporting Settings for Power Network Synthesis and Power Network Analysis Strategies: To get a report of the current values of the strategies used by power network synthesis and power network analysis by using the report_fp_rail_strategy command. [16] 5.9 Performing Prototype Global Routing One can perform prototype global routing to get an estimate of the routability and congestion of the design. Global routing is done to detect possible congestion hot spots that might exist in the floorplan due to the placement of the hard macros or inadequate channel spacing. To perform global routing, use the route_fp_proto command. 5.10 Performing Hierarchical Clock Planning This section describes how to reduce timing closure iterations by performing hierarchical clock planning on a top-level design during the early stages of the virtual flat flow, after plan groups are created and before the hierarchy is committed. One can perform clock planning on a specified clock net or on all clock nets in the design. à ¢Ã¢â€š ¬Ã‚ ¢ Setting Clock Planning Options: To set clock planning options, use the set_fp_clock_plan_options command. à ¢Ã¢â€š ¬Ã‚ ¢ Performing Clock Planning Operations: To perform clock planning operations, use the compile_fp_clock_plan command. à ¢Ã¢â€š ¬Ã‚ ¢ Generating Clock Tree Reports: To generate clock tree reports, use the report_clock_tree command. à ¢Ã¢â€š ¬Ã‚ ¢ Using Multivoltage Designs in Clock Planning: Clock planning supports multivoltage designs. Designs in multivoltage domains operate at various voltages. Multivoltage domains are connected through level-shifter cells. A level-shifter cell is a special cell that can carry signals across different voltage areas. à ¢Ã¢â€š ¬Ã‚ ¢ Performing Plan Group-Aware Clock Tree Synthesis in Clock Planning: With this feature, clock tree synthesis can generate a clock tree that honors the plan groups while inserting buffers in the tree and prevent new clock buffers from being placed on top of a plan group unless they drive the entire subtree inside that particular plan group. This results in a minimum of clock feedthroughs, which makes the design easier to manage during partitioning and budgeting. [16] 5.11 Performing In-Place Optimization In-place optimization is an iterative process that is based on virtual routing. Three types of optimizations are performed: timing improvement, area recovery, and fixing DRC violations. T

Tora: an emblem of New Woman

Ibsen was a powerful Norwegian playwright who left no stone unturned to explore all the critical problems of the society right from his Pillars of the Society ,Ghosts   to The Enemy of People. Ibsen was really disturbed to find that women were being turned into mere gewgaws of the household ,to decorate the house, to nod at every odd proposal put forth by her husband, i.e, the master of the household, to dance to his tune all the time to keep the peace and harmony of home intact. He was such aggrieved to observe this   unhealthy balance ,that he composed the brilliant play A Doll’s House, considered to be one of the best plays that marks a new epoch in the history of women’s emancipation. Ibsen himself wrote â€Å"The wife in the play ends by having no idea of what is right or wrong; natural feeling on the hand and belief in authority on the other have altogether bewildered her. A woman cannot be herself in the society of the present day ,which is an exclusively masculine society ,with laws framed by men and with a judicial system that judges feminine conduct from a masculine point of view.†[Cf. Ibsen, Henrik:Notes for the Modern Tragedy ] Hence, Ibsen was very much aware of the fact that the housekeeping woman-cum-wife was invariably looked down upon by the male chauvinistic husband. Why not look at Nora Helmer and her position in the household from   close   quarters? In the very first act , when she enters with a load of parcels in her hand and interacts with her husband Torvald , she is addressed at least more than once as â€Å"featherbrain†, â€Å"scatterbrain† so forth. It may be so taken for granted that Torvald driven by the unalloyed passion of love for her wife addresses her in like terms. So far as ‘songbird’ , ‘doll-wife’ go that may have some significance. But, when Torvald unhesitatingly utters, â€Å"You wouldn’t believe how much it costs a man when he’s got a little songbird like you†, his dormant chauvinism suddenly pops up to the open. Does he not mean to belittle the labor his wife is incessantly putting in to run the household smoothly , that too, not in expectation of any material gain for herself in turn? Yes, he does, whether   he intends to mean so or not. In Act One itself, it becomes crystal clear to us that Nora loved her husband so deeply that she never hesitated   to forge a document when it came to the decision of saving her husband’s life. She even confessed of working as a copywriter for sometime working late into the night burning her midnight oil and energy.Why? TO SAVE HER HUSBAND†S PRECIOUS LIFE!!And what did she get in turn? Nora’s interaction with Mr. Krogstad too was not out of the necessities of profession. The letter that he left shoving her to the brink of destruction was rectified later on by another letter of contrition. But , the matters had tuned worse by then. Our query to the playwright is ,if Nora got the taste of earning like a man by copywriting why did she not continue with it and accrue some   sort of self-complacency by seeing herself dependent? Perhaps, the subjugation of women in that era for which Mary Wollstonecraft and others of that period fought was stifling her to death from within! Knowingly, unknowingly, or whatever!! Mr. Krogstad at one point started pestering Nora to influence her husband for retaining him as his subordinate in the bank. Thereafter, this sneaking man went to such a daring extent that Nora could not disown him, knowing full well that this man was more venomous than a viper. Mr. Krogstad started blackmailing Nora with such incriminating statements like, â€Å"Your father died on the twenty-ninth of September. But look at this –your father has dated his signature the second of October. Isn’t that a curious thing, Mrs. Helmer?† [Nora is silent] Can you explain it?†[A Doll’s House,Act One] Nora was caught into the snare and lastly when the act of unintentional forgery stood exposed to Torvald in Act Three and he hit the roof ,accusing his doll-wife   with harsh words ,Nora   had every reason to give vent to her pent-up hurt feelings. She felt humiliated when Torvald pointed rude and naked finger to her dead father’s moral failings and detested her for inheriting so. Was it not the most heinous form of accusation? Torvald could demean her , could call her names even, but was it really ethical of him as a son-in-law to bring down the house at the expense of his dead father-in-law’s moral turpitude? That might be utterly baseless even! Even after such humiliation Nora could utter , â€Å"I’ve loved you more than anything in the world.† Torvald cast aspersions on her by calling her â€Å"liar†, â€Å"hypocrite† even worse, â€Å"a criminal†. She had inherited her father’s shiftless character by proving herself   irreligious, immoral, irresponsible! Nora went on listening all the odorous, obnoxious accusations maintaining her cool. And , even when Torvald thundered, â€Å"And I’m brought so pitifully low all because of a shiftless woman!† she remained surprisingly calm rejoining only, â€Å"Once I’m out of the way, you’ll be free.† Torvald went a step further and snowballed his unguarded comment, You will remain here in my house —that goes without saying—but I shall not allow you to bring up my children†¦.I shouldn’t dare trust you with them†, then could any motherly sentiment remain untouched ? Nora’s heart too bled profusely at such ruthless utterance. That was why, it took hardly a few seconds for her to decide to slam the door on her husband’s face at last! When the letter of repentance or redress reached Torvald, he in the same peremptory tone spoke out, â€Å"Nora, I’m saved.†Nora in a passive tone inquired of her position, â€Å"And I?† With intense passion,Torvald said, â€Å"You too of course.† After such mindless , pointless   humiliation , how could Torvald be so inane to belt out the words, â€Å"I’ve forgiven you..†?† We are surprised to see Nora turning back to look stern at him , thus intimidating him. Nora pulled up all her courage to blurt out on his face, â€Å"You’ve never loved me, you’ve only found it   pleasant to be in love with me.†Therafter , Nora went on expatiating her restrained attitude in both her father’s house and later at her husband’s . She admitted of dancing to both her father’s and husband’s tunes , as the cases might have been. Later on with much conviction the revelation dawned upon her, â€Å"You and Papa have committed a grievous sin against me: it’s your fault that I’ve made nothing of my life.† She never had the courage to express her own opinion. Now she mustered her guts to speak out and think independently with her own grey cells!! Now she was not hesitant to say that she was never happy at Torvald’s , but only â€Å"gay†. Nora felt the need of educating herself, she was keen on standing on her own feet ,if she was to know herself and the world outside. Her tongue did not falter to utter, â€Å"That’s why I can’t stay here with you any longer.†This daring statement could only suffice to bring   a New Woman   out of conventional Nora ,a   doll-wife ,in the era when voicing   a protest against a husband   was simply next to impossible!! Nora lastly hit the bull’s eye by saying that life could hardly be a real marriage for a couple who pretended all he time to be HAPPY!! It was the greatest miracle of all when Nora left the house slamming the door behind. The house appeared EMPTY to Torvald. We were being prepared throughout the play for this final action from Nora. Her unrequited love for her husband , for her family shoved her to the edge of utter denial . The children for whom she spent her last farthing to buy the costliest Christmas gift , too, could not be trusted with her!! Such utterance drove her desperate, insane and her decision seemed appropriate.However inane it might appear at the outset, it brought to the fore a revolutionary   and protesting self   of a woman who hated demeaning her womanhood. As economic freedom happened to be a significant criterion of a free woman , will it be very wrong to say that Nora of Ibsen foreshadowed Lily Briscoe of Virginia Woolf or her thought of an earning woman as a New Woman as appeared in her A Room of one’s Own?As in later days we find Michele Foucault arguing   about self-refusal rather than self-discovery,by which he meant to say that ‘to become what she was not at the beginning.† Thus, the concept of New Woman which was taking shape with Mother Courage of Brecht or Wife of Bath of Chaucer even much earlier found a veritable shape in Nora Helmer. Nora was truly justified to rise up in arms against the abominable subjugation inflicted on her and Ibsen was assiduously preparing the audience right from Act One for such a finale. Of course, Nora had every right to chime in with a contemporary woman-poet, Anna Laetitia Barbauld, â€Å"Yes,injured Woman!rise, assert thy right! Woman!too long degraded , scorned, oppressed; O born to rule in partial Law’s despite, Resume thy native empire o’er the breast.†[The Rights of Woman] Works Cited 1.Ibsen , Henrik[Tr. Peter Watts]:A Doll’s House and Other Plays, Penguin, England, 1965. 2.Cole, Toby ed: Playwrights on Playwriting,Colonial Press, USA, 1960. 3.Pritchard, R.E.ed:Poetry by English Women ,Elizabethan to Victorian, Continuum, New York, 1990. 4.Meyer, Michael:Ibsen, Penguin, England, 1967. 5, Gatting, Gary ed:The Cambridge Comapanion to Foucault, CUP, New York, 1994.            

Main Theoretical Perspectives Within Sociology - 1330 Words

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2. Natural Knowledge of God in Insight Lonergan’s argument, I will offer my assessment of whether or not the constitution permits his philosophical means. Lonergan moves from treating God as an object of thought to treating God as an object of affirmation by way of an argument: â€Å"If the real is completely intelligible, God exists. But the real is com ¬pletely intelligible. Therefore, God exists.† I will refrain from elaborating on the argument itself; works doing this are available. What is important, given the interests of this study, is the following statement by Lonergan in the Epilogue: [O]ur first eighteen chapters were written solely in the light of human intelligence and reasonableness and without any presupposition of God’s†¦show more content†¦The question arises, however, as to what Lonergan’s assessment would be of arguments that proceed more—or at least more explicitly—on the side of the object. One wonders, for instance, how Lonergan would see his argument in relation to Aquinas’s five ways. As it happens, Lonergan makes two illuminating statements about the five ways in chapter nineteen of Insight. First, he writes, â€Å"[T]he five ways in which Aquinas proves the existence of God are so many particular cases of the general statement that the proportionate universe is incompletely intelligible and that complete intelligibili ¬ty is demanded.† Second, he writes, â€Å"[B]esides Aquinas’s five ways, there are as many other proofs of the existence of God as there are aspects of incomplete intelligibility in the universe of proportionate being.† These two statements illuminate what is central to Lonergan’s argument: the incapacity of proportionate being as such to satiate the mind’s demand for complete intelligibility. Alicia Jaramillo contends that Lonergan’s focus on this demand—something on the side of the subject—does not mark an abandonment of classical cosmological arguments. I now return to the question of whether

Coca Cola Supply Chain Management - 1425 Words

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Hudson River a Detailed and Comprehensive Geological History Free Essays

string(88) " than a centimeter in the last couple thousand years and shows no signs of speeding up\." Contents Introduction†¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦.. 2 Hudson River Formation†¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦. We will write a custom essay sample on Hudson River: a Detailed and Comprehensive Geological History or any similar topic only for you Order Now . 5 Hudson Canyon†¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦12 Glacial History†¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦.. 14 Conclusion†¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢ € ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦17 Bibliography†¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦18 Maps Diagrams†¦.. †¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦. 19 Hudson Canyon†¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã ¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦.. 19 Geological Processes†¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦Ã¢â‚¬ ¦. 2 1|Page Introduction In 1872, a naturalist and surveyor by the name of Verplanck Colvin found the source of the Hudson River. It is a small pond on the south western slope of Mt. Marcy, the highest peak in the Adirondacks, called Lake Tear of the Clouds. So little is Lake Tear of the Clouds that if no water was to feed it for seven days it would be reduced to just an empty basin. Nevertheless, the Hudson starts right in its waters. One could say the Hudson River is divided into two distinct sections differentiated by geology and appearance. The first section winds its way through the Adirondack Mountains spanning 166 miles from Lake Tear of the Clouds to the Federal Dam in Troy. This section is un-navigable by boat and in some places somewhat rapid. The second section, which is quite different from the first, starts at the Federal Dam and runs for 149 miles through the â€Å"rolling hills† all the way to the Narrows between Brooklyn and Staten Island. Back up north at Lake Tear of the Clouds is fed by natural springs and runoff from the sheer steepness of Mt. Marcy and other streams winding down from the high peaks of the Adirondacks. Throughout the whole Adirondack mountain range, the watershed drains and dumps runoff from 3,400 foot peaks into the lowlands less than 410 feet above sea level. From Lake Tear of the Clouds [in the space of a mile] the river drops 1,000 feet down a deep trench to join the Opalescent River1. A bit more southward, the Mohawk River drains much of the runoff from central New York into the Hudson. In fact, over half of the Hudson Rivers water volume comes from the Mohawk, and without it, the Hudson would be practically non-existent. Further south of Albany tributaries flow westward to the Hudson from the Taconic Mountains and eastward from the Catskills. Still further south the tributaries for the Hudson begin to appear rectangular, almost following the trend of the faults and 1 The Opalescent River is not a separate river from the Hudson but merely a section named by old Native American tribes. 2|Page ridges that run northeast to southwest of the river while other tributaries join at right angles to the faults along the joint planes. At this point in its path, the river begins to occupy its original bedrock gorge formed millions of years ago, flowing over rock ledge rapids and the coarse cobble point bars2 that are very common from Mt. Marcy to Glens Falls, until it is partially blocked by mountains. It is here that the river makes a sharp turn to the east and flows through the Luzerne Mountain gorge in western New York and then emerges quickly onto glacial lake sediments deposited in the Pliocene Glaciation and forms a very broad, almost meandering path on the lowlands (supported by shale) for the nearly 130 miles to Newburgh. South of Newburgh the river cuts laterally through the hard crystalline rocks of the Hudson Highlands, shifting back and forth in its valley (almost like a cradle) until it emerges from the highlands and starts to exhibit fjord like characteristics within the towering rock walls around it. The river’s course then slightly curves in front of the Palisades escarpment3, which towers more than 328 feet above the water’s surface. At the Narrows the Hudson breaches its final barrier, the terminal moraine4 of the last glaciation (more on this in the Glacial History section) before it reaches the Atlantic Ocean. At the Atlantic (although tidal) the Hudson behaves as any other river would and deposits its bed load (sediments carried by the river) and some of the fine-grained suspended load (basically fine grained sand and dirt floating in the water) into the form of sandbars. Over millions of years, these have contributed to building up many islands including Staten Island, Hoffman Island, Swinburne Island and many others. The very low slope of the Hudson plays a great role in the amount of discharge and island buildup, too, as it only rises about 0. 4 inches per mile for the last 150 miles of the rivers path. To give some perspective, the Mississippi river rises approximately 6 inches per mile during its course, and discharges about 700 million tons of sediment per year into the Gulf of Mexico 2 Coarse cobble point bars are essentially pointed cobble that has been piled into bar like formations. These formations are generally formed when sediments carrying cobble leave it behind. 3 Ground fo rmed into a steep slope as part of fortification. â€Å"Moraine† is a word used to describe the earth, stones and debris a glacier deposits. â€Å"Terminal† describes that these items were deposited where the glaciers maximum extent was, in this case Long Island. 3|Page and its mouth is approximately a ? -mile wide. The Hudson River discharges about 175 million tons of sediment per year and its mouth is about the same width at a ? mile. With a 2 inch increase in slope geologists predict the discharge rate of the Hudson would spike up to about 450 million tons per year and the mouth of it would close up to about 250’ wide. This would place Manhattan underwater and greatly limit boat traffic as well as make Long Island more of a true island separated from land by at least 3 miles or so of water5. And so, the geography of the Hudson River today ends here in Manhattan, but the geology of what lies underneath is much more important. Continue reading if you must, and dwell into a mystery of time and a lot of pushing and pulling. 5 Do not worry about this happening now though because the rivers overall slope has not changed more than a centimeter in the last couple thousand years and shows no signs of speeding up. You read "Hudson River: a Detailed and Comprehensive Geological History" in category "Papers" 4|Page Hudson River Formation The Geology of the Hudson River is complex. Billions of years of folding, pushing, pulling, separating, and moving have formed, deformed and reformed the Hudson River valley into what it is today, a â€Å"giant palimpsest6, a great parchment on which the hand of nature has written and rewritten her bold signature for more than a billion years†7. In the next section, I am going to attempt to condense over a billion years worth of Geologic History into less than ten pages. Despite complex knowledge and strange words it is a simple story of time and rocks, moving and changing: the formation of the Hudson River and its valley. The Hudson’s geological â€Å"personality† very much reflects its structure and the changes made on it, underneath it and all around it from the Pleistocene glaciations8 . The bedrock foundation of the Hudson was established in the space of three oregany’s (mountain building periods) beginning over a billion years ago. These mountain-building episodes re-triggered long intervals of underground erosion and periodic submersion by the epicontinental seas (or oceans) to help start forming the Hudson River Valley. At a point much later in this story, glacial erosion reshaped the landscape of the HRV into what it appears as today. The first major mountain building episode, the Grenville Orogeny began about 1. 2 billion years ago. It was one of the biggest Oregany’s and affected a broad region along the coast of what was Ancient North America, from the northeast waters of Canada to northwestern Mexico. The mountains created by the Grenville Orogeny were most likely as tall as or taller than the Himalayas and were driven to these heights by a collision of Laurentia (Ancient N. America) and Gondwana (Africa) in which Gondwana overrode Laurentia. The deep burial of Laurentia resulted in the first 7 Written upon, or engraved on more than once. The Hudson: A History, Chapter 1: The River and the Land, pg. 10 8 A period of ice buildup to form glaciers, or the act of glaciation. 5|Page metamorphism, partial melting of rock and the separation of the light and dark minerals found in the Adirondack gneisses9. Many hundred thousand of years later in the Proterozoic period as the continents periodically moved, basal tic volcanic rocks merged into the mountains cutting the anorthosites10 and gneisses laterally across. These gneisses are around one billion years old, while the Highland gneisses may be a bit older. The Fordham gneisses are the youngest and can be dated to just under a billion years old. Over the millions of years, long episodes of erosion on the Grenville Mountains and constant lifting of the crust have brought it to the surface. Later in the Proterozoic period, erosion of this crust formed and provided a thick source of sedimentary deposits that partially submerged the upland area of coastal Laurentia (presently this is the area south of and parallel to the Appalachian Mountains). These deposits are now found mostly in the Appalachians, with almost all of them have been removed from the Hudson valley, leaving hard rock and clay for the Hudson River to rest on. In the early Paleozoic, the sand and gravel that was eroded from the mountains during the Proterozoic period became basal sandstone and conglomerate11, which is more commonly known as the Potsdam Sandstone in northern NY and the Lower Quartzite that is prized throughout the Hudson Highlands. As the Epicontinental sea inundated this (once) mountainous region the sandstone and Lower Quartzite were buried under a thick cover of marine limestone and shale, which was laid down in an elongated trough that formed on the continental shelf where mountains had once been. The limestone was mostly deposited on the shallow edges of the trough while the shale solidified from the mud carried into the deeper seaward part of the trough. The solidified shale then created the bedrock between Glens Falls and the Highlands. 9 Coarse, grained metamorphic rock composed of quartz, feldspar and mica. An igneous rock made up largely of soda-lime feldspar. 11 Rock composed of rounded fragments of various rocks cemented together in a mass of hardened clay and sand, like a composite. 10 6|Page In the Late Cambrian period,12 Laurentia once again collided, but this time with the ancestral core of Europe, Baltica and a large fragment of what is thought to be the continental crust known as Avalonia. This started the mountain building period known as the Taconic Orogeny, which lasted throughout the Ordovician Period. The Taconic Orogeny also resulted in the new supercontinent Laurasia. While much of the activity involving this collision took place well to the east it also affected the HRV. Island arc volcanic structures such as the Cortlandt Complex have been found in the Hudson Highlands. To the North and West in the mid-Hudson Valley, the sedimentary rocks that were deposited in the early Paleozoic Period were folded (with the trend of the folds and faults already in place) parallel to the southwest to northeast facing the Appalachians. These folds and faults eventually became some of the paths of the HRV tributaries. Closer to the coast than these faults, thin sheets of rock were pushed several dozen miles west. This event is known as the Taconic Thrust and took place in the area where today exists the Taconic parkway. Because of this event, the fine-grained shale that was there was crumpled (as if we crumple paper) and pushed into the narrow channel of water west of the mountains near present day Croton. Over many years thereafter blocks of limestone into the channel and were merged into a jumble of shale clumps. Today millions of years later the river flows past the western edge of the channel and then cuts into the disorganized deposits of shale as it continues south. As we travel through time, sandstone, limestone, shale and Proterozoic bedrock from the Hudson Highlands became buried as Laurentia’s coastal margin was subducted13 close to where it and Europe’s plates met. The rocks that met each other from each plate partially melted and transformed into more gneiss, marble and schist14, which was then folded and moved once more to be in alignment 12 00 million years ago Subduction can be described as the action or process in plate tectonics of the edge of one crustal plate descending below the edge of another, almost like a controlled earthquake. 14 Schist is a metamorphic crystalline rock that has a closely foliated structure and can be split along approximately parallel planes. 13 7|Page with the Appalachians. This set the stage for the modern day continental shelf to form, although it would take millions of more years for it to happen. After the two plates of Europe and Laurentia collided, there was a sort of lull in activity around this area. This allowed streams in the lowlands to follow the valleys formed along the fault lines, or on the softer marble layers around Manhattan. The oceanic crust borders and the rocks around NYC and to the east more or less contained the streams around Manhattan, while the streams in the lowlands and around our area were free to roam and spread out. After the Taconic Orogeny ended, a long interval of erosion began stripping away the excess crust as the â€Å"new† continent (modern North America, or Laurasia) was very slowly lifted by the compression of the plates. As the upland area was eroded away the epicontinental sea gradually filled the Hudson Valley region from the low lying land of the coastal margin all the way west nearly three-quarters of the way to Pittsburgh. Later during the Silurian and into the early Devonian period shallow seas covered the area and left behind calcium carbonate sediments making the soil very rich. At around the same time rivers formed and flowed from the uplands carrying major amounts of sediment west to the sea to form marine sandstone. While the marine sandstone was being formed, at the shoreline a large delta15 formed over the junk that the marine sandstone left behind. By the midDevonian period, an alluvial plain16 had reached across much the western Catskill region and the shoreline had shifted slightly west about 15 miles or so. At this time, thousands and thousands of feet of sediment from mid-Paleozoic times were piled up over the Hudson Valley and continental red sandstone (one reason why there is so much sandstone around here) from farther east inland were incorporated with the gray marine sandstone from the west closer to the coast. The force of all this happening at once overturned the folds that were in place to the northwest (near present day Schunemunk Mountain along the NYS thruway near Highland Mills) exposing the limestone that 15 A Delta is a triangular alluvial plain, usually where a rivers mouth is. A level or gently sloping flat or a slightly undulating land surface resulting from extensive deposition of alluvial materials by running water 16 8|Page was buried slightly underneath the sediment that had accumulated over the years. This marked the end of the Devonian Period, and the start of the Acadian Orogeny. The Acadian Orogeny began as the North American plates started to compress again and lift up the eastern mountain ranges around New England and western Pennsylvania. This Orogeny was also partially caused and linked to the collision that happened between Laurentia and Gondwana that created Laurasia, and most likely, if this Orogeny had not happened the Hudson River would be a completely different river, and possibly would be connected to the Mississippi River. As the plates began to compress each other again they created volcanic arcs and granite intrusions somewhat east of the Hudson Valley near the coast. Around this time in our little history story the seas started to retreat from the east to west and started to expose the incredibly thick layer of sediment and rocks from the Acadian Mountains all the way to the Catskills. The final compressions dating back to the Paleozoic era continents and the Alleghenian Orogeny now ended and the earth came together to form Pangaea. Because of all this land being pushed up, the Epicontinental Sea retreated from the Catskills to the Poconos in Pennsylvania leaving much of New York and New England dry once again. Now above sea level the strata from the Devonian period became subject to erosion for 250 million years. At some point during this time, the drainage patterns shifted and aligned the ancient Hudson River along a NorthSouth line much like it is today. This was the biggest directional change the Hudson ever underwent. As the strata and sediment were worn away from this new path of drainage, it revealed the granite, marble and schist underneath which became the building materials for our modern world. With the Taconic Mountains now more to the east and the Catskill Mountains to the west the Hudson worked its way down deep into the sediment it was on top of leaving behind a hard bedrock base nearly 5,000 feet deep in places17. This created a solid foundation and left the Hudson with a relatively stable path 17 Over the last several million years, and an Ice age this has all been filled in and now the Hudson has an average depth of 32’. 9|Page that has not changed tremendously since. The breakup of Pangaea followed soon thereafter and the coastline of North America began to resemble what it is now. At the same time, the Hudson was filling its banks; basaltic magmas were merged along the fault lines and into the bedrock forming the Palisades Sill18. After that, compression and buildup of sediment and rock slowly built the Palisades up. Today the part of the Palisades that stands is almost like a canyon above the Newark Basin. The â€Å"tabular†19 Palisades still slope to the west, and the eastern edge forms the escarpment, or â€Å"palisade†20 21 of rock joined vertically that we recognize today from miles around New York and from the air as we fly to new places and heights. But to learn how, we must travel to another time in this story, the Mesozoic Period. Some time in the late Mesozoic period, igneous rock deposits were moved yet again and placed along a line going Northwest to southwest from Canada to New England lifting the mountains in its path by several hundred feet and in some cases over 1,000 feet. Because, as you might infer, rock takes up space, and as it lifted up the mountains and separated them, it started to separate North America’s continental plate away from the mid-ocean ridge22 and over a very hot area above the earth’s layer of magma near where the present day Appalachians exist. This caused what geologists think was a shot of magma that melted through that particular part of the plate (which was quite thinner than today) and uplifted the Northern part of the Appalachians. This, in turn reactivated erosion and brought the domed like anorthosites to the surface which is most likely the reason that the Appalachian Mountains are not scraggly and sharp like the Alps, but more rolling with large boulders and open expanses of rock. The Catskills and Adirondacks also experienced lifting, but in a much smaller amount. Almost at the same time as all this uplifting was happening, a 18 19 Think of this as the palisades foundation. L. Sirkin H. Bokuniewics – The Hudson River Valley: Geological History, Landforms, and Resources pg. 17. 20 L. Sirkin H. Bokuniewics – The Hudson River Valley: Geological History, Landforms, and Resources page 17 21 Palisade literally means â€Å"a fence of stakes for defense† The Palisades are called the Palisades by Native American Tribes because they helped as defense for them from other tribes. 22 The mid-ocean ridge is a undersea mountain ridge that is where the North American and European plate meet. While this ridge has hardly ever changed, the plates do move. In this case it is the biggest moves it has ever made. 10 | P a g e hole began to form from sinkholes on the western slope of Mt. Marcy and soon filled with water. This was Lake Tear of the Clouds. After Lake Tear of the Clouds formed and filled with water, the Newark basin reached its fullest capacity of water and the Hudson began to â€Å"drive† into its flood plain and carve out its gorge in the gneisses of the Highlands of southern New York. This area is now mostly between West Point and Hastings on Hudson, but it continues as a much smaller â€Å"weaker† gorge almost down to Fort Lee. The Hudson was now a true river, but would still undergo massive changes over the next several million years. At this time in the Hudson River’s history, Long Island did not exist as what it does today. It was a tiny, almost alcove piece of land that was in no way an island. In addition to that, there was no opening to the Atlantic for the Hudson. At the place where the Hudson empties into the Atlantic at the Narrows was a big solid mass of land. The Hudson by definition was a lake. So, as the Hudson filled up and he water put immense pressure on the piece of landmass blocking it from the Atlantic it began to carve out and widen an outlet. It took only a few hundred years23 for the Hudson to make it to the Atlantic, bringing with it thousands upon thousands of tons of sediment that had piled up in the Newark Basin. This created the new continental shelf to form the coastal â€Å"plain† we see today that stretches for about a hundred miles out to sea from New York, only in that time and age it stretched for nearly 425 miles, nearly halfway to Bermuda. The Hudson now had an outlet, and the waters started moving south digging, and bringing sediment to the mouth building up Long Island a little bit24, as well as separating it from the mainland with what is now the East River. The sea levels around North America also dropped a few centimeters as the waters made their way up the Hudson forming the Hudson River estuary. This raised the Hudson’s waters by a few centimeters and created its almost permanent banks that have 23 This is an extremely short time in geologic history and greatly shows how much the pressure was on the landmass blocking the Hudson from the Atlantic. 24 Although Long Island did get built up at this time, the majority of it was built up during the last ice age nearly 20,000 years ago. 11 | P a g e not changed very much since. Because the sea levels were much lower in that time period the Hudson also began its excavation of the Hudson Canyon with the help of the naturally occurring currents (more on this in the Hudson Canyon section) and more than doubled its length to nearly 895 miles (about 1,440km) long. After nearly 500 million years the Hudson rivers formation had ended and all that was left to change it was its own water wearing away at its bottom and a glaciation that would come in a few million years. Hudson Canyon The Hudson Canyon is possibly the biggest mystery of the Hudson River. How did it form? When exactly did it form? Why did it form? These are all questions geologists and hydrologists ask when looking at it. Most people in fact have never heard of it. To them the Hudson is a river that starts in the Adirondacks and ends at the narrows. To the few that know of the Hudson Canyon, the Hudson River starts in the Adirondacks and ends nearly 925 miles south halfway to Bermuda right after falling over a half mile down a [now] underwater canyon and then fanning out and spreading to the Atlantic Ocean. There, even though underwater it still carries small amounts of the Hudson’s freshwater (out to sea), and most geologists still consider it a part of the Hudson. This makes the true length of the river from Lake Tear of the Clouds to the end of the Hudson Canyon 922 miles, more than double of what we consider the â€Å"Hudson†. As explained in the last section (Hudson River Formation) in the late Mesozoic Period the Hudson River broke the land barrier that held it from emptying into the Atlantic. When it broke the barrier it began to carve a new path out to sea towards Bermuda. At some point, it reached the Continental Shelf and dug into it creating a canyon that eventually connected the shelf to the ocean basin, which is about 1. 5-2. 5 miles deep. Technically the canyon begins as a natural channel many miles wide at the mouth of the Hudson in a depression about 12 feet deep in the rivers bed. It 12 | P a g e ontinues then through the Hudson channel and under the Ambrose light25. Soon after the Ambrose light, it reaches the shelf and goes through the real canyon part of it that is called the Hudson Canyon proper. The Hudson Canyon proper is located about 100 miles east of Battery Park City and has walls almost ? mile in height, which can be compared to the Grand Canyon whose cliffs are about 1-1/8 mile dee p. The Hudson Canyon is the largest â€Å"submarine† canyon in the United States, partially due to the currents that pass over, and carrying away sediment and rock, thus carving it deeper and deeper. Over the past 30 years since it was discovered, tracking equipment has logged a nearly 12-inch change in its depth and width making the Hudson Canyon also the fastest growing canyon in the Atlantic Ocean. At the same time it is growing wider and deeper, it is also getting closer to the magma underneath and behind the continental shelf. In simple terms, one day in the next couple hundred or thousand years it will break through and magma will come out creating a new island, possibly connecting the East Coast of the United States with a land bridge that extends more than halfway to Bermuda. Many tributaries around the canyon would be raised by the magma, creating a new network of rivers and streams on the land bridge that could host many kinds of wildlife as well as marsh like environments. In addition to this, the Hudson Canyon has large stores of methane hydrates which according to scientists is a very promising clean burning natural energy source, and could help reduce oil consumption. It is a Canyon of great importance to the Hudson River, and also a big clue into the Glacial history surrounding the HRV. 25 The Ambrose light is the site of a Light House that ships going into the New York Harbor and other harbors in the area use for navigation purposes. 13 | P a g e Glacial History The Glacial History of the Hudson River is probably the one of the most important geological event that happened in the Hudson Valley in the last 50,000 years. Evidence points mostly to the Pleistocene Glaciation, which was the last and only Glaciation to reach this far south into the United States for the change that happened on the Hudson River since it was originally formed. The topography of the Hudson Valley enabled the ice from the Pleistocene Glaciation to form a Lobate Ice margin26 about 50 miles north what is now Manhattan long island. Around 22,000 years ago the Ice over the Catskills and Taconic uplands thinned, while it thickened in the Hudson Valley and expanded southward closer to the mouth of the Hudson. Scientists today doing Pollen analysis and radiocarbon dating have found that the climate back then right before, and as the last Ice age started was much warmer than today. As one can expect, warmer conditions meant more plants, and the sea level was much higher than today27. When the climate cooled and the Glaciers expanded south all these trees, plants and debris were ground down and immense pressure pushed them into the ground, almost dissolving them into dirt. This not 26 Lobate means resembling of a lobe. In this context it is used to describe the shape of the edge of the Glacier, or its maximum extent which was a short of lobe shape. 27 Evidence shows that the waters might have been as far north Albany. 14 | P a g e only made the area much more barren, but also flattened the Adirondacks, and Hudson Highlands down many thousands of feet. The glacier continued to expand 26,000 years ago and merged with smaller glaciers up north to form one big glacier known as the â€Å"Laurentide Glacier†28. This Glacier covered all of Ontario, the St. Lawrence River, Manitoba, Nunavut, and parts of Quebec, as well as the Great lakes down to Chicago where it almost ran parallel to the US/Canada border before dipping slightly down towards present day Manhattan and following the coast of the US up north. At the height of this glaciers advance the ice most likely was more than 1,000 feet thick over the tops of the Appalachians (if you do the math this means that it was over 1. miles deep) meaning immense pressure was being placed on everything flattening the landscape. This also meant that because there was so much pressure, and the water of the Hudson never froze 100%29 the Hudson’s waters literally pushed the earth and carved the floor of the Hudson to a depth similar that of what it was before it broke its barrier at th e Narrows. 30 The dirt being compressed turned back into soft metamorphic rock, and created marble where none existed near Warrensburg. A few miles south at Glens Falls the Ice naturally deepened because of the drop in elevation and gained momentum31 carving out the fjord previously made even bigger, which created Storm King, Beacon and Bear Mountain. All this rock carved out of the Fjord eventually made its way south where it was dumped over Manhattan and Long Island, somewhat accounting for all the Limestone and shale and schist around that area. At this time, the Hudson Canyon was also carved out by the glacial ice melt flowing through it with rocks and debris and became much deeper and wider. When the Laurentide glacier made it to the Narrows its front stopped moving forward, but its back kept on moving forward compressing everything together (Like an accordion) and melting a lot of the ice. Why this happened is not really known by Scientists because glaciers can float. This area became the Glaciers â€Å"dumpster† and the Terminal Moraine was officially formed. Long Island was 28 29 Yes, it was named after Laurentia, ancient North America. Meaning the whole time there was a glacier over this area, the Hudson was still flowing but now mostly with ice melt from the glacier itself. 0 Of course this all filled back in as the glacier melted. 31 A glacier is always moving, whether it is 1 foot a year or 1 inch a year. 15 | P a g e built up and out to its current state and the Moraine extended west into New Jersey and Pennsylvania, carrying with it glacial melt creating many of the glacial lakes in that area such as Lake Hackensack, Glacial Lake Hudson and many others. C lay also being carried was dumped all over the region (mostly on the current Rockland County side) and created a nice thick, slippery layer on which the glacier to slide on. This process of dumping and melting continued for many thousand years and started the recession of Laurentide. In a 2,000 year period from 26,000 years ago to 24,000 years ago Laurentide melted and receded so that all of Long Island, Staten Island, New Jersey, Pennsylvania and pretty much everything south of present day Hartford Connecticut was ice free. The Ice continued to melt over the next 4,000 years until everything south of Glens Falls was free of ice. The ground, sort of like a sponge when you fill it with water, rose a few meters and went nearly back to its state before the glacier. At Glens falls The glacier stopped for a thousand or so years and slowly melted providing the Hudson valley with a constant stream of fresh glacial water. Around 19,000 years ago the glacier started to recede from Glens Falls and the melt water created Glacial Lake Albany which continued to grow throughout the next several thousand years as Laurentide receded. At 15,500 years the Climate suddenly got cold and the glacier advanced back south to near Poughkeepsie and created the Wallkill, Poughkeepsie, Red hook, Hyde Park ad Pine Plains moraine. As suddenly as the Climate got cold, it got warm again and by 13,000 years the glacier was receded north of present day Quebec City. When the climate got warmer again the sea levels rose, this time to near Albany, and caused Glacial Lake Albany to drain. For the next couple thousand years as the climate cooled, the Hudson was tidal up to Poughkeepsie and as the Sea retreated. This brought the tides down with it to near Peekskill where it stayed for many thousands of years until around 6,000 years ago it began to go north to nearly 20 miles past Troy32 by 2,000 years ago the sea was at its present place, and the Hudson was in its present 2 The exception to this is the Troy Dam; if it wasn’t built the Hudson would still be tidal nearly 20 miles north of it. 16 | P a g e state. Long Island was as it is now, and the coast was pretty much the same besides what natural erosion as taken away since then. This was the final Glaciation, and the final change to the Hudson River. After ne arly 1. 2 billion years, several different Oregany’s, Hundreds of changes, 4 different climate changes and a whole lot of pushing and pulling and moving the Hudson River was finished being formed and all it needed was for Henry Hudson to come sailing to name it†¦. Conclusion If you have gotten this far along into this history story then you will know that the Hudson River didn’t just appear, it doesn’t formally end at the Narrows between Brooklyn and Staten island and it isn’t just a river. It is the culmination of 1. 2 billion years (and counting) of the earth doing its shtick33 on the world we live on. It took 7 different continents to pull this off, and it worked out beautifully creating a river of outmost importance to our lives, lives before us, and lives to come. I like most of you out there reading this paper did not know a thing about the Geology of the Hudson River when I started this project. It probably took me a proportionate amount of time to learn this as it did to create the whole Hudson. Now, after early 3 months of reading words I don’t know, looking at diagrams I can’t even understand and writing technical terms that I can’t pronounce I have learned what it took, and takes to create the Hudson. Like they say, it takes a village to raise a child; it took a whole world and 1. 2 billion years to create this river, a river of small nature compared to others around us such as the Nile, or Amazon which are nearly 5 times the length of the Hudson and took a very disproportionate amount of time to create. 3 â€Å"Piece†, or â€Å"thing† in Yiddish 17 | P a g e So, as I leave you with this 20 page Essay, think about the next time you go to the Hudson and pick up a handful of sand, and know, just know that that handful of sand has been moved around for 1. 2 billion years to end up at your feet. Bibliography L. Sirkin H. Bokuniewics (2006) – The Hudson River Valley: Geological History, Landforms and Resources Wikipedia (http://en. wikipedia. org/w/index. php? title=Hudson_Canyonoldid=453958227) – Hudson Canyon Data SIO, NOAA, U. S. Navy NGA, GEBCO (2010) – Google Earthâ„ ¢ United States Geological Survey (USGS) (2004) – Sea Floor Topography Backscatter Intensity of the Hudson Canyon Region Offshore of New York New Jersey (http://pubs. usgs. gov/of/2004/1441/html/interp. html) Phil Stoffer Paula Messina (2008) – Introduction to the Geologic History of the New York Bight (http://www. geo. hunter. cuny. edu/bight/Geology. html) Phil Stoffer Paula Messina (2008) – The Highlands Region (http://www. geo. hunter. cuny. edu/bight/highland. html) R. G. Wilkins Booth (1970) – The Ontario Water resources commission Geology of the upper part of the Severn River basin and the Severn River basin lying within the Hudson River Lowlands. Steven H. Sehimmrich – Geology of the Hudson Highlands Region (www. environmentalconsortium. org) Access Genealogy – Geology of the Hudson (http://www. accessgenealogy. com/newyork/hudson/geology_hudson. html) Charles Merguerian (2010) – Geology 133 Field Trip 18 | P a g e Dick Goodman (2013) – Geologist in California, gave much information and advice on this project United States Navy Geological Services (2013) – Maps, Graphs Bradford B. Van Diver (1985) – Roadside Geology of New York John F. Shupe (1996) – National Geographic Atlas of the World Revised sixth edition Kevin Hile (2009) – The Big Book of Answers Tom Lewis (2005) – The Hudson: A History Maps 19 | P a g e The maps presented here on the next couple of pages are all ones used in this essay as reference. They are from many different sources and show many of the things I talked about, visually. Hudson Canyon 20 | P a g e 21 | P a g e 22 | P a g e Geographical Diagrams 23 | P a g e 24 | P a g e 25 | P a g e How to cite Hudson River: a Detailed and Comprehensive Geological History, Papers

An Effective Parenting Style Essay Example For Students

An Effective Parenting Style Essay Parents have a major role in their children lives because of how they decided to raise their children. Parents tell their children what is right and what is wrong. According to the Wikipedia, â€Å"Parenting style is a psychological construct representing standard strategies that parents use in their child rearing.† As parents use the technique to raise their children, they also shaped their value and personality. â€Å"Parenting style considers the balance between two aspects of parenting, namely, control, and warmth† (Ginsburg, Durbin, Garcias-Espana, Kalicka, and Winston, p. 1041). The most commonly heard parenting styles are authoritative, authoritarian, permissive, and uninvolved. Authoritative parenting is the one with most control and provide the least amount of support whereas authoritarian parenting also has most control, but with more support. Permissive parenting parents give their children all the supports that are needed and not much of the control. Uninvolved parents are basically similar to carless parents; they give nearly no support and no control to their children. Which style of parenting did your parent(s) use on you? In 2009, the American Academy Pediatrics published a journal along with a research case, Associations Between Parenting Styles and Teen Driving, Safety-Related Behaviors and Attitude. The study was claiming to be how parenting related to the behavior of driving. By the end of the study, it was suggested by professionals that parents should set limits for their children freedom (Ginsburg, Durbin, Garcias-Espana, Kalicka, and Winston, p. 1042-1043). The case study had proven that young adults who were raised by high controlling and least supportive parent(s) had a significant number of differences. ., et al. Parenting and Obsessive Compulsive Symptoms: Implications of Authoritarian Parenting. Journal of Cognitive Psychotherapy 24.3 (2010): 151-164. Academic Search Premier. EBSCO. Web. 28 Aug. 2011. Li, Yan, Philip R. Costanzo, and Martha Putallaz. Maternal Socialization Goals, Parenting Styles, and Social-Emotional Adjustment Among Chinese and European American Young Adults: Testing a Mediation Model. Journal of Genetic Psychology171. 4 (2010): 330-362. Academic Search Premier. EBSCO. Web. 28 Aug. 2011. Partridge, Brian C. Adolescent Psychological Development, Parenting Styles, and Pediatric Decision Making. Journal of Medicine Philosophy 35.5 (2010): 518-525.Academic Search Premier. EBSCO. Web. 9 Sept. 2011. Wikipedia contributors. Parenting styles. Wikipedia, The Free Encyclopedia. Wikipedia, The Free Encyclopedia, 10 Aug. 2011. Web. 14 Sep. 2011.